Science topics: ChemistryCarbon
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Carbon - Science topic

A nonmetallic element with atomic symbol C, atomic number 6, and atomic weight 12.011. It may occur as several different allotropes including DIAMOND; CHARCOAL; and GRAPHITE; and as SOOT from incompletely burned fuel.
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Is fracking a way to obtain oil and natural gas and fracking reduced carbon emissions and what liquid is used in fracking?
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Yes, natural gas can be obtained without fracking. It can be extracted from conventional gas reservoirs, where the gas is trapped in permeable and porous rocks, allowing it to flow easily to the surface through a drilled well. Hydraulic fracturing, or fracking, is a drilling method used to extract petroleum (oil) or natural gas from deep in the planet. In the fracking process, cracks in and below Earth's surface are opened and widened by injecting water, chemicals, and sand at high pressure. Hydraulic fracturing produces fractures in the rock formation that stimulate the flow of natural gas or oil, increasing the volumes that can be recovered. Wells may be drilled vertically hundreds to thousands of feet below the land surface and may include horizontal or directional sections extending thousands of feet. It reduces the current rate of carbon emissions. The burning of methane is “cleaner” than burning coal or gasoline, but as others have pointed out when a well is fracked, significant amounts of methane can be released into the air during the production stage – through leaks, venting, and flaring. Fracking has been blamed for leaking millions of tons of methane, a greenhouse gas more potent than carbon dioxide. Fracking is also associated with other airborne hydrocarbons that can cause health and respiratory issues. Fracking uses large amounts of water, which can become contaminated and affect local groundwater. Fracking fluid is 99.5% water and sand. 0.5% is made up of safe chemical additives, most of which are found in common household products, like toothpaste and makeup remover, or in the foods you eat. Fracking is a slang term for hydraulic fracturing, which is the process of creating fractures in rocks and rock formations by injecting specialized fluid into cracks to force them to open further. Fracking increases the rate at which water, petroleum, or natural gas can be recovered from subterranean wells. Fracking reduced CO2 emissions by producing lots of natural gas (methane). The increase in supply brought the price down to where it was cheaper than coal. Power plants were converted from coal to natural gas. Methane emits a lot less CO2 than coal to produce the same amount of energy.
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Why is economic growth not compatible with environmental sustainability and relationship between carbon emissions and income?
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If economic growth depended on technological innovation, the relationship would not be strained. China is trying this way, which may provide an effective strategy for developing countries.
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Is a low carbon development market a green market model?
If yes;
Is low carbon development a win-win sustainable development model?
If yes;
Is low carbon development a green growth based market model?
If yes;
Is low carbon development a win-win economy-environment partnership model?
If yes.
Then, sustainable development a la low carbon is a green markets/green growth based model.
Therefore, if they believe this why not to say openly that to ensure environmental sustainability as per goal 7 of the Millenium Development Goals(MDGs) we have to implement sustainable development strategies(e.g. low carbon) through green market based green growth?...
If they believe that, then why to use low carbon development sometimes, sustainable development sometimes, green growth sometimes, and green markets sometimes in any document coming from the UN institutions related to this file or agreements like the 2015 Paris Agreement giving the impression that they are not closely related concepts, but the same?. Why not to minimize confusion?
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RK, thank you for taking the time to comment.
Did you read the context on which this question is based before commenting? The existence of confusion that allows people, busnesses, institutions like UN, FAO, governments and non-profit organizations to use concepts/models as if they were other concepts/models or to describe even inverse opposite models as the same model or to attach characteristics to models which they do not have if you look closely to the structure of that model is what prompted this question. I see all that concept confusion in your comment.
However, I am not hear to convert anybody and I respect your view if that is the way you think.
You may find some good food for thoughts in the following articles aimed at minimizing development concept/model confusion by looking backwards to how critical sustainability problems were created 1776-1987 and to how critical sustainability problems were addressed by the WCED 1987 as critical sustainable development problems, which sparks the beginning of the confusion:
Sustainability thoughts 192: What are the sustainability consequences of assuming that flawed paradigms are golden paradigms? The case of the perfect traditional market.
Sustainability thoughts 194: How can we show that the sustainable development solutions to the socio-environmental sustainability problem created by traditional market thinking by 1987 are both partial and without clear priority solutions?
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What effect does economic growth have on carbon emissions and balance between the environment equity and economy?
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Economic growth has a consistent, positive and significant relationship with both territorial and consumption-based carbon dioxide emissions. Second, we find some evidence that economic growth has a stronger effect on consumption-based emissions than territorial emissions. With steady improvements in the energy intensity of economic growth (meaning that less energy is required to produce an additional unit of global GDP) and, more recently, a dramatic rise in clean energy deployment, there has been a growing divergence between GDP growth and CO2 emissions. All households will lose income, and low-income households will suffer the most. Low-income households could see income losses of 12 per cent in a low emissions scenario and 19 percent in a high emissions scenario by the end of the century markedly higher losses than the median income group. Higher levels of economic activity tend to go hand-in-hand with additional energy use and consumption of natural resources. As fossil fuels still account for 80 percent of the global energy mix, energy consumption remains closely related to greenhouse gas emissions and hence to climate forcing. Sustainability is the balance between the environment, equity, and economy. Sustainability is used to indicate programs, initiatives and actions aimed at the preservation of a particular resource. However, it actually refers to four distinct areas: human, social, economic and environmental. Instead of using non-renewable natural resources, use of renewable natural resources should be preferred. Waste water generated by industries should be recycled. We should use natural resources cautiously so that economic growth and ecological conservation go hand in hand. The balance between the environment, equity and the economy. Sustainability is a term used in the most diverse contexts, from fashion to economic investment, through culture or food. This concept is often confused to environmental sustainability. Sustainable development emphasizes the responsible use and preservation of natural resources. Implementing resource-efficient practices, such as recycling, waste reduction, and sustainable agriculture, helps protect ecosystems, reduce pollution, and enhance economic productivity.
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What does the recycling process involve and role of microorganisms in recycling of carbon and nitrogen through air and soil?
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Recycling is the process of collecting and processing materials that would otherwise be thrown away as trash and turning them into new products. Recycling can benefit your community, the economy, and the environment. Products should only be recycled if they cannot be reduced or reused. Recycling is the process of collection and conversion of waste into useful and new products. Recycling is done to minimize the pollution and the waste generated. It helps in the converse the environment. Microorganisms and fungi break down wood and return carbon to the biogeochemical cycles. If these organisms become absent, carbon would accumulate in the wood, where it could not be recycled into the environment. The fixation of nitrogen is dependent on microorganisms mostly through biological nitrogen fixation. Microbes and fungi decompose dead animals, plants and matter. When they do so, they release carbon dioxide into the air due to respiration and contribute to the carbon cycle. In the soil and ocean there are certain microbes that have the ability to convert ammonia into nitrites. This contributes to the nitrogen cycle. Microbes are critical in the process of breaking down and transforming dead organic material into forms that can be reused by other organisms. This is why the microbial enzyme systems involved are viewed as key 'engines' that drives the Earth's biogeochemical cycles. Plants absorb carbon from the environment in photosynthesis and return it in respiration. Animals obtain their carbon by eating plants; they release carbon in respiration. Micrororganisms return carbon to the environment when they decompose dead plants and animals. Bacteria play a central role: Nitrogen-fixing bacteria, which convert atmospheric nitrogen to nitrates. Bacteria of decay, which convert decaying nitrogen waste to ammonia. Nitrifying bacteria, which convert ammonia to nitrates/nitrites. Microorganisms play a dominant role in the biogeochemical cycling of nutrients.
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What is the role of microorganisms in the decomposition of organic matter and the recycling of carbon and role of microorganisms in the breakdown of organic matter?
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Dr Ania Isandra thank you for your contribution to the discussion
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Is there significant difference between these other element present which highlighted as black? This is from Scanning Electron Microscope-EDS
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You should ask someone familiar with that particular EDS system. It may be as Jürgen Weippert suggested. Maybe that system flags the currently highlighted element in green. Our Oxford Aztec will normally overlay an elemental profile. I don't know about other systems.
The spectrum is similar to that of orthoclase (KAlSi3O8) or its weathering products. The C is probably that which is virtually ever-present in the SEM. It may be from SEM pump oil or contamination during preparation. Great care is necessary to completely eliminate it. It is only a footnote to the main story.
See if you can get more counts (less noise) next time. Also expand the energy axis to highlight the interesting area. There is nothing going on beyond 5 keV.
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The biocatalysts can be more available than traditional catalysts? The quation is related to the sustainablity by conversion of carbon using biocatalysts.
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Biocatalysts, which are typically enzymes derived from living organisms, have gained significant attention for their potential in catalyzing various chemical reactions. One area of interest is their ability to convert carbon sources into valuable products, such as biofuels, pharmaceuticals, and fine chemicals.
Compared to traditional chemical catalysts, biocatalysts offer several advantages:
1. Specificity: Enzymes often exhibit high specificity for their substrates, leading to fewer side reactions and higher product purity compared to chemical catalysts. This specificity can also lead to higher yields of the desired product.
2. Mild Reaction Conditions: Enzymes usually operate under mild conditions (e.g., ambient temperature and pressure, neutral pH), which can reduce energy consumption and minimize the need for costly equipment.
3. Renewable and Sustainable: Biocatalysts are derived from living organisms and can be produced from renewable resources, making them more environmentally friendly compared to chemical catalysts, which may rely on non-renewable resources and generate hazardous waste.
4. Compatibility with Aqueous Systems: Many biocatalysts are water-soluble and function well in aqueous environments, which simplifies reaction conditions and downstream processing.
5. Biodegradability: Enzymes are generally biodegradable, which can simplify purification and reduce environmental impact.
However, biocatalysts also have some limitations compared to traditional chemical catalysts:
1. Stability: Enzymes can be sensitive to temperature, pH, and other environmental factors, which may limit their stability and reusability in industrial processes.
2. Cost: Production and purification of enzymes can be expensive, especially for complex or low-yield reactions, which can impact the overall cost-effectiveness of biocatalytic processes.
3. Substrate Limitations: Enzymes may have specific substrate requirements, limiting their applicability to certain reactions or substrates.
4. Reaction Rate: While enzymes can exhibit high specificity, they may also have slower reaction rates compared to chemical catalysts, especially for large-scale industrial processes.
Overall, the efficiency of biocatalysts in converting carbon sources into valuable products depends on various factors, including the specific reaction, substrate, enzyme properties, and process conditions. In many cases, biocatalysis offers significant advantages in terms of selectivity, sustainability, and compatibility with aqueous systems, making it an attractive option for certain applications despite its limitations.
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What are the microorganisms that recycle nutrients by breaking down dead and what organism plays a role in constantly recycling carbon?
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Dr Joseane Maria Hammes thank you for your contribution to the discussion
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carbon nitride is a organic polymer and used as photocatalyst. It exhibits sheet like morphology.
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Determining the binary layer structure of Urea derived Carbon Nitride (UCN) involves a few steps:
1. **Synthesis**: UCN can be synthesized through the pyrolysis of urea under ambient pressure without additive assistance¹.
2. **Characterization**: After synthesis, the structure of UCN can be characterized using various techniques. These may include X-ray diffraction (XRD), Fourier-transform infrared spectroscopy (FTIR), and X-ray photoelectron spectroscopy (XPS)².
3. **Microscopy**: Techniques such as transmission electron microscopy (TEM) and scanning electron microscopy (SEM) can be used to visualize the binary layer structure³.
4. **Analysis**: The data obtained from these techniques can be analyzed to determine the binary layer structure of UCN³.
Remember, the specifics of your experimental design might need to be adjusted based on the characteristics of the UCN and the specific objectives of your research. It's always a good idea to consult with a materials scientist or chemist to ensure your experimental design is robust and appropriate for your study.
(1) Simple pyrolysis of urea into graphitic carbon nitride with recyclable .... https://pubs.rsc.org/en/content/articlelanding/2011/jm/c1jm12620b.
(2) Carbon nitrides: synthesis and characterization of a new class of .... https://pubs.rsc.org/en/content/articlehtml/2017/cp/c7cp02711g.
(3) Layered graphitic carbon nitride: nano-heterostructures, photo/electro .... https://link.springer.com/article/10.1007/s40097-021-00442-5.
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glassy carbon electrode 0.071 cm2
Carbon Cloth, Nickel foam= 1X1 cm2
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Measure the Double Layer Capacitance of the Electrode: The double layer capacitance (Cdl) of the electrode can be measured using electrochemical impedance spectroscopy or cyclic voltammetry1.
  1. Measure the Double Layer Capacitance of a Flat Surface: The double layer capacitance of a flat surface (CdlRef) is also measured1.
  2. Calculate the Roughness Factor: The roughness factor is then estimated by normalizing the double layer capacitance of the electrode with the double layer capacitance of a flat surface1. This can be represented by the formula:\text{Roughness Factor} = \frac{C_{dl}}{C_{dlRef}}Roughness Factor=CdlRef​Cdl​​
  3. Calculate the Density of Electrochemically Active Sites: Using the roughness factor, the density of electrochemically active sites can be obtained by calculating the density of active sites on a flat surface multiplied by the roughness factor1.
Remember, the specifics of your experimental design might need to be adjusted based on the characteristics of the electrode and the specific objectives of your research. It’s always a good idea to consult with a materials scientist or electrochemist to ensure your experimental design is robust and appropriate for your study.
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(1) Best Practices for Reporting Electrocatalytic Performance of Nanomaterials. https://pubs.acs.org/doi/pdf/10.1021/acsnano.8b07700.
(2) Reporting activities for the oxygen evolution reaction - Nature. https://www.nature.com/articles/s42004-023-01024-y.pdf.
(3) New insights into evaluating catalyst activity and stability for oxygen .... https://pubs.rsc.org/en/content/articlehtml/2018/se/c7se00337d.
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I am heating melamine at 550°C for 4 hrs but around 470°C I could observe white fumes from the muffle furnace which deposits as white powder on the outside of the furnace. I do not know why the product graphitic carbon nitride is also not formed.
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Addition: I just found a (German) safety data sheet on which it says that the ignition temperature for a dust layer (Mindestzündtemperatur der Staubschicht) is 450°: https://www.gischem.de/download/01_0-000108-78-1-000000_1_1_400.PDF
So I would say you're lucky there was no severer incident.
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We are currently developing a BFT system. It is necessary to measure the C:N ratio level in BFT. Imhoff cone techniques are used only to observe floc density.
However we prefer to measure the C:N ratio in the BFT rather than using elemental analysis. Can anyone suggest if there is a device or kit available?
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There are C/N analysers that function well
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I'm looking for public databases for green finance indicators, which provide information on sustainable investments, carbon emissions, sustainable development initiatives, and other indicators related to green finance. These are used by green banks, businesses, and governments to assess and track progress in the field of sustainable finance.
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Here are a few examples:
1. Bloomberg NEF (BNEF): BNEF provides data and analysis on various aspects of sustainable energy and finance, including green bonds, renewable energy investments, and clean energy funds. They offer a range of subscription plans and have a comprehensive database on renewable energy projects and financial transactions.
2. Climate Bonds Initiative: The Climate Bonds Initiative maintains a database that tracks global green bond issuance. They provide information on the types of projects funded by green bonds, such as renewable energy, energy efficiency, and sustainable transportation. Their database is freely accessible on their website.
3. CDP (formerly Carbon Disclosure Project): CDP is a global platform that collects and discloses environmental data from companies, cities, states, and regions. They manage a comprehensive database of climate-related information, including financial metrics and performance indicators related to climate change mitigation and adaptation.
4. United Nations Environment Programme Finance Initiative (UNEP FI): UNEP FI is a partnership between the United Nations and the financial sector. They provide a range of resources and initiatives aimed at promoting sustainable finance. While they may not have a specific public database for green finance indicators, they publish reports and guidelines related to sustainable finance practices.
5. Global Sustainable Investment Alliance (GSIA): GSIA is an international network of organizations that promote sustainable investment practices. While they don't maintain a public database, they publish an annual report that provides insights into the size and growth of the global sustainable investment market.
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Most current projections of carbon emissions are based on structural data such as the economy, population, and technology. However, unstructured data will also have a certain impact on carbon emission prediction, such as public attitude and government policy intensity. Now how do you measure most unstructured data? What is the basis for the change in the unstructured data if the scenario analysis is followed?
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Carbon emission projections can be incorporated into unstructured data through various methods such as natural language processing (NLP) to analyze textual reports, sentiment analysis on news articles, or topic modeling on social media discussions.
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I have to calculate the carbon content present in the catalyst from the TGA plot. Does anybody have an idea?
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From 900 Celsius to more
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I milled two activated carbons, with different main sources (shell nutt and bituminous coal). The shell nut AC did not increase in surface area but had some degree of amorphization after milling. Still, the bituminous coal AC remains the same in graphitization, but the surface area is duplicated. Can changes in surface structure alter the surface area measured by BET method? Does the amorphization remove micropores and then reduce surface area? And the main source could influence this result and how?
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Surface area and amorphization degree in high-energy ball-milled activated carbon can indeed be related, and the main source can influence this relationship. When milling activated carbons from different sources, such as shell nut and bituminous coal, variations in surface area and amorphization can occur due to differences in their intrinsic properties.
Regarding your Antonio Ilderlânio de Sousa Leite observation, it's intriguing that while the shell nut activated carbon didn't increase in surface area, it exhibited some degree of amorphization post-milling. Conversely, the bituminous coal activated carbon maintained its graphitic structure but showed a doubling in surface area.
Firstly, changes in surface structure can indeed impact the surface area measured by the BET method. Amorphization, characterized by the disruption of the ordered carbon structure, can lead to the creation of new surface sites and defects, potentially increasing the measured surface area despite a reduction in crystallinity.
Secondly, it's plausible that amorphization could remove micropores, especially if the milling process is severe. Micropores are inherently part of the porous structure of activated carbon and contribute significantly to its surface area. Therefore, their removal could result in a decrease in measured surface area.
The influence of the main carbon source on these results is multifaceted. Differences in precursor materials can lead to variations in the initial structure and composition of the activated carbon. This variance can affect how the carbon responds to the milling process, impacting factors such as the extent of amorphization and the preservation of micropores. For instance, bituminous coal may have a more robust crystalline structure that resists amorphization, while shell nut-derived activated carbon may be more prone to structural changes.
In conclusion, the relationship between surface area and amorphization in high-energy ball-milled activated carbon is complex and influenced by factors such as the carbon source and the milling conditions. Understanding these relationships is crucial for tailoring activated carbon properties for specific applications.
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How many tons of carbon emissions does it take to raise the temperature of the Earth by one degree and impact of CO2 on climate change and the planet's temperature?
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Every time the CO2 concentrations rise by 10 ppm, the mean global temperature increases by 0.1 °C. A temperature rise of just one degree Celsius would also intensify extreme heat waves, which would become more frequent and last longer. This would in turn increase the risk of heat-related illnesses, which especially affect members of the most vulnerable populations. Global carbon dioxide emissions from fossil fuels and industry totaled 37.15 billion metric tons (GtCO₂) in 2022. Without carbon dioxide, Earth's natural greenhouse effect would be too weak to keep the average global surface temperature above freezing. By adding more carbon dioxide to the atmosphere, people are supercharging the natural greenhouse effect, causing global temperature to rise. It has been estimated that 2,400 gigatons of CO₂ have been emitted by human activity since 1850, with some absorbed by oceans and land, and about 950 gigatons remaining in the atmosphere. The relationship between carbon emissions and the increase in Earth's temperature is complex and not directly quantifiable in terms of tons of carbon emissions per degree of temperature rise. The impact of carbon emissions on global warming depends on various factors, including the concentration of greenhouse gases in the atmosphere, feedback loops, and the Earth's climate system.
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Does microbial decomposition remove carbon from the atmosphere and role played by microorganisms in the cycling of carbon in the atmosphere?
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decomposition? No
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The synthesis of CQD has the process of neutralizing by NaOH to PH7, what's the aim of this process?
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Greetings to all,
As part of my research, I am synthesising carbon quantum dots. Using ethanol as the solvent, I performed a solvothermal method. As I have tried different temperatures and times (up to 70 hours of treatment, the color remains yellowish), as well as catalysts (Con. Sulfuric acid, Con. Nitric acid, and Con. Hydrochloric acid - Nitric acid does not give fluorescence). In spite of this, I was only able to obtain yellowish green fluorescent. It shows a very very light blue color without a catalyst (nearly imperceptible). If you could please assist me in figuring this out and tell me any important points I need to keep in mind while synthesizing carbon quantum dots. The precursor used in this process is resorcinol.
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I am confused on how the sand content is calculated in aggregate size fractions separated by wet sieving, especially when the fractions are to be used for further analysis. If they are to be dispersed later on and analyzed for carbon content, is the correct approach to subtract whatever was determined to be carbon in the fraction from the total weight of the fraction and that will give you the sand content of that fraction?
Sometimes the literature is vague and just states that the sand contents were determined for each fraction and that the final aggregate weights were corrected, and then provides a formula (in some cases) but do not exactly state how the sand weight was determined. Was it determined by texture analysis? Was it calculated post carbon analysis? Was it done by dispersion of a sub-sample?
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Dear friend Valeria Izeppi
Determining the sand content in soil aggregate fractions after wet sieving involves a meticulous approach to ensure accurate results, especially when these fractions are intended for further analysis.
To calculate the sand content of a fraction, subtracting the determined carbon content from the total weight of the fraction is not typically the correct approach. Instead, sand content is usually determined directly through methods specific to soil analysis.
One common method involves texture analysis, where the soil sample is dispersed and separated into different particle size fractions using sieves. The sand fraction, typically consisting of particles with diameters between 0.05 mm and 2 mm, is collected and weighed separately.
In some cases, determining sand content may involve post-carbon analysis adjustments, but this depends on the specific protocol followed. However, it's essential to ensure that the method used is well-documented and follows established procedures to maintain accuracy and consistency.
Literature on soil analysis may sometimes lack specific details on how sand content was determined for each fraction. In such cases, it's beneficial to refer to established methodologies or consult with experts in the field for clarification.
In summary, determining sand content in soil aggregate fractions after wet sieving involves a combination of sieving, weighing, and possibly additional analyses, with the specific method chosen based on the requirements of the study and established protocols in soil science.
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What are the sources of carbon footprint in agriculture and difference between carbon footprint and carbon emissions?
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Dr Ilan Kelman thank you for your contribution to the discussion
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Can biochar retain carbon in stable form in soil and biochar actually sequester carbon?
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Dr Chandan De thank you for your contribution to the discussion
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contextualise climate change, think of batteries, solar, wind...
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The stored energy is released during periods of low energy generation with grid integration, ensuring continuous power supply and enhancing grid stability.
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So, I am doing electrodeposition of Zn onto carbon fabric, which is my working electrode. As reference electrode, I used Ag7AgCl in 3M KCl, and as counter electrode, I used a Zn plate. After varying the current density, I see that the cathodic potential increases. Is it something to do with Gibbs energy? or the ease of overcoming the barrier to form Zn onto the cathode?
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Your calculation of the combined electrode potential (E = E⁰_Zn -E⁰_Ag/AgCl) is correct
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How is the biosphere involved in the carbon cycle and compare and contrast the ways carbon and water cycle through the biosphere.?
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Dr Murtadha Shukur thank you for your contribution to the discussion
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How the water and carbon cycles are linked to the interactions within the biosphere and how does carbon move from the biosphere to the hydrosphere?
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The water cycle and the carbon cycle are intimately linked through their interactions within the biosphere, Earth's zone of life. Here's how:
The Big Picture:
  • Sun's Energy Drives It All: Solar energy powers both cycles. It evaporates water, starting the water cycle, and fuels photosynthesis in plants, a key player in the carbon cycle.
  • Plants Bridge the Gap: Through photosynthesis, plants absorb carbon dioxide (CO2) from the atmosphere and use it to build organic matter. This pulls carbon from the atmosphere and stores it in living things (biosphere).
  • Water is Essential: Plants release water vapor (transpiration) during photosynthesis, adding moisture to the atmosphere, influencing the water cycle.
Carbon from Biosphere to Hydrosphere:
  • The Highway of Water: When it rains, water washes over land, carrying organic materials (dead plants, waste) from the biosphere into rivers and ultimately the oceans (hydrosphere).
  • Dissolution: Some of this organic matter dissolves in water, introducing carbon into the hydrosphere.
  • Sinking Carbon: Dead organisms that fall into water bodies also sink, carrying their carbon to the ocean depths. These can become buried in sediments, storing carbon for long periods.
Here's the takeaway:
  • The biosphere acts as a giant carbon reservoir, taking CO2 from the atmosphere through plant activity.
  • Water movement physically transports organic carbon (from dead plants, waste) from land to the hydrosphere (oceans, lakes).
  • Some of this carbon dissolves in water or gets buried in sediments, becoming part of the long-term carbon cycle.
This intricate dance between the water cycle, carbon cycle, and the biosphere is vital for life on Earth. It regulates climate, supports healthy ecosystems, and influences the long-term storage of carbon.
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How do the hydrosphere and biosphere interact to move water through the water cycle and carbon and water cycles connected to plants & algae?
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The interaction between the hydrosphere and biosphere plays a crucial role in moving water through the water cycle and connecting it with the carbon cycle. Here's how they interact, particularly concerning plants and algae:
  1. Water Cycle in the Hydrosphere and Biosphere Interaction:Transpiration: Plants and algae play a significant role in the water cycle through transpiration, the process by which water vapor is released from their leaves into the atmosphere. During photosynthesis, plants and algae take up water from the soil or aquatic environment through their roots. This water is then transported through the plant or algal cells to the leaves or fronds, where it evaporates into the atmosphere as water vapor. Transpiration accounts for a substantial portion of water movement from the biosphere into the atmosphere. Evapotranspiration: Evapotranspiration combines the processes of evaporation from water bodies and transpiration from plants and algae. It represents the total loss of water to the atmosphere from both sources. Evapotranspiration plays a crucial role in the redistribution of water vapor in the atmosphere and influences regional climates and precipitation patterns.
  2. Connection to Carbon and Water Cycles:Photosynthesis: Plants and algae play a pivotal role in both the water and carbon cycles through photosynthesis. During photosynthesis, plants and algae absorb carbon dioxide (CO2) from the atmosphere or water and utilize water and sunlight to produce glucose and oxygen. This process fixes carbon from CO2 into organic molecules, forming carbohydrates, lipids, and other organic compounds. Water molecules are split during photosynthesis, providing electrons and protons for the conversion of CO2 into organic matter. Carbon Sequestration: Through photosynthesis, plants and algae sequester carbon dioxide from the atmosphere or water, incorporating it into their tissues. This process helps mitigate the accumulation of CO2 in the atmosphere, acting as a carbon sink. Carbon stored in plants and algae can be further transferred to other organisms through the food web or deposited as organic matter in soils or sediments, contributing to long-term carbon storage. Respiration: Conversely, plants and algae also participate in cellular respiration, where they metabolize organic carbon compounds to release energy, CO2, and water. During respiration, stored carbohydrates and other organic molecules are oxidized to generate ATP, the energy currency of cells, and CO2 is released back into the atmosphere or water. This respiration process completes the cycling of carbon between plants, algae, and the environment.
Overall, the interaction between the hydrosphere and biosphere, particularly through the activities of plants and algae, plays a critical role in moving water through the water cycle and connecting it with the carbon cycle. Through processes such as transpiration, photosynthesis, and respiration, plants and algae influence the distribution, movement, and transformation of water and carbon within terrestrial and aquatic ecosystems, shaping ecosystem dynamics and global biogeochemical cycles.
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How does cellular respiration relate to the cycling of carbon through the environment and hydrosphere connected to the carbon cycle?
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Cellular respiration is intimately connected to the cycling of carbon through the environment, including the hydrosphere, and plays a crucial role in the global carbon cycle. Here's how cellular respiration relates to the cycling of carbon and its connection to the hydrosphere:
  1. Carbon Fixation and Release:During photosynthesis, carbon dioxide (CO2) from the atmosphere is taken up by autotrophic organisms such as plants, algae, and cyanobacteria. These organisms use the CO2 along with water and sunlight to produce glucose and oxygen through the process of carbon fixation. This glucose serves as an energy source for the organism and is also used for growth and reproduction. The oxygen is released into the atmosphere as a byproduct.In contrast, during cellular respiration, glucose is broken down in the presence of oxygen to produce energy, CO2, and water. This process occurs in both autotrophic and heterotrophic organisms. The CO2 produced during cellular respiration is released back into the atmosphere, completing the cycle. In aquatic ecosystems, this CO2 can also dissolve in water, contributing to the carbon content of the hydrosphere.
  2. Role in the Carbon Cycle:Cellular respiration is a significant component of the carbon cycle, which involves the movement of carbon between the atmosphere, biosphere, hydrosphere, and lithosphere. Carbon exists in various forms, including atmospheric CO2, dissolved carbon in water bodies, organic carbon in living organisms and detritus, and inorganic carbon in rocks and minerals.During cellular respiration, carbon is transferred from organic molecules (such as glucose) to CO2, which is released into the atmosphere or dissolved in water. This CO2 can then be taken up by photosynthetic organisms in aquatic ecosystems, such as phytoplankton and aquatic plants, or terrestrial ecosystems, such as trees and other vegetation. Through photosynthesis, these organisms convert CO2 back into organic carbon compounds, completing the carbon cycle loop.
  3. Hydrosphere Connection:The hydrosphere plays a critical role in the global carbon cycle, as it contains large reservoirs of dissolved inorganic carbon (DIC) and organic carbon. CO2 from the atmosphere can dissolve in water bodies, forming carbonic acid and contributing to the acidity of aquatic environments. Aquatic organisms, including phytoplankton, algae, and aquatic plants, utilize this dissolved CO2 during photosynthesis to produce organic carbon compounds.Conversely, during cellular respiration, aquatic organisms release CO2 into the water as a byproduct of metabolism. This contributes to the dissolved CO2 pool in aquatic environments. The cycling of carbon through cellular respiration and photosynthesis in the hydrosphere is essential for maintaining carbon balance in aquatic ecosystems and influencing global carbon dynamics.
In summary, cellular respiration is a key process in the carbon cycle, contributing to the exchange of carbon between the atmosphere, biosphere, and hydrosphere. It involves the conversion of organic carbon compounds into CO2, which can then be utilized by photosynthetic organisms to produce organic carbon again. This cycling of carbon through cellular respiration and photosynthesis helps regulate the global carbon balance and influences Earth's climate and ecosystems.
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I am currently working on carbon biomass carbon stock estimation by the pace of climate change I'm keen interest on carbon neutrality strategies, particularly in forest ecosystem. I would appreciate insights, case studies, or best practices regarding how small we can achieve carbon neutrality. Are there specific challenges or success stories that you've come across? Any recommended resources or recent studies on this topic would be valuable.
Thank you in advance for your valuable insights
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Greetings of the Day sir,
I presented one seminar on carbon-neutral farming and came across some insightful case studies. I am hereby recommending three case studies, Pls see. Hope, it will help you.
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Are biofuels environmentally friendly, and will its use reduce carbon emissions and significance of plant-based biofuels in reducing carbon emissions?
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Dr Himanshu Tiwari thank you for your contribution to the discussion
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How can CO2 emissions be lowered to net zero without biofuels and role do renewable energy sources play in reducing carbon emissions?
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Dr Himanshu Tiwari thank you for your contribution to the discussion
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Is biofuel currently a sustainable energy solution and production of biofuels affect carbon emissions?
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Biofuels can be a sustainable energy solution, particularly if produced from waste materials or dedicated energy crops grown sustainably. However, certain biofuel production methods can have varying impacts on carbon emissions:
  1. Sustainable Biofuel Production: Biofuels sourced from waste materials, algae, or sustainably grown crops can offer carbon-neutral or even carbon-negative emissions profiles, contributing to overall emissions reduction.
  2. Land Use Change and Emissions: However, if biofuel feedstocks require significant land use change, such as deforestation or conversion of agricultural land, it can lead to increased carbon emissions, undermining the sustainability of biofuel production.
  3. Lifecycle Analysis: Assessing the lifecycle emissions of biofuels is crucial, considering factors like cultivation, processing, transportation, and combustion. Sustainable practices throughout the production chain are essential to minimize emissions and maximize environmental benefits.
In short, biofuels can be a sustainable energy solution depending on their production methods and feedstock sources, but careful consideration of their environmental impacts, particularly on carbon emissions, is necessary.
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Can algae replace fossil fuels as an energy source and bio fuels be claimed to be carbon neutral?
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Biomass and biofuels derived from microalgae can be used in power production. Microalgae biofuels has high potential to replace fossil fuel for internal combustion engine. Electricity can be generated using microalgae in coal co-firing to mitigate greenhouse emission and reduce coal consumption. Algae-derived renewable diesels and jet fuels are drop-in fuels that directly replace petroleum fuels without modification of engines. They meet all the specifications for the petroleum fuel they replace. Algae cultivation on non-arable land allows it to produce biofuel while not competing with them for resources. Algae biofuel has many advantages over fossil fuels, including reduced greenhouse gas (GHG) emissions and carbon emissions. Because algae use carbon dioxide through photosynthesis, algae biofuel is carbon neutral. The CO2 produced by burning the fuel is the same amount of CO2 that the algae took to grow and produce the fuel. This means that the net CO2 emission is zero, the same as if the algae had never been grown. Biofuels are said to be carbon-neutral because the carbon dioxide that is absorbed by the plants is equal to the carbon dioxide that is released when the fuel is burned. This means it doesn't release any extra carbon dioxide into the atmosphere. Within the biospheric carbon cycle, bioenergy can be carbon neutral because the carbon that is released during combustion has previously been sequestered from the atmosphere and will be sequestered again as the plants regrow. Microalgae were found to be the largest renewable, clean energy resource with the potential to replace fossil fuels. Cultured microalgae in a photobioreactor could meet the biomass requirements for continuous biofuel generation in addition to repairing CO2 emissions and treating wastewater. It's estimated that under the right conditions, algae could produce up to 60 times more oil per acre than land-based plants. Since algae needs carbon dioxide to grow, it takes greenhouse gases out of the atmosphere, making it nearly carbon-neutral.
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What is the carbon footprint of algae fuel and algae plants that produce energy almost carbon neutral?
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Respected Sir, Rk Naresh
  • Algae-based fuels and energy production have often been touted as having a potentially low carbon footprint compared to traditional fossil fuels. However, the actual carbon footprint can vary depending on various factors such as the specific production method, the energy sources used in cultivation and processing, and the overall lifecycle analysis of the process.
  • Algae-based fuels can be considered almost carbon neutral because the algae used in their production typically consume carbon dioxide during growth, offsetting some of the carbon emissions when the fuel is burned. Additionally, if the algae are cultivated using renewable energy sources such as solar or wind power, the carbon footprint can be further reduced.
  • However, it's essential to consider the entire lifecycle of algae fuel production, including cultivation, harvesting, processing, transportation, and distribution. Energy-intensive processes involved in cultivation, such as mixing, aeration, and harvesting, can contribute to the overall carbon footprint if they rely heavily on fossil fuels.
  • Lifecycle assessments (LCAs) are used to evaluate the environmental impacts of various products and processes, including algae-based fuels. LCAs take into account all stages of production and use, from raw material extraction to end-of-life disposal or recycling. Studies have shown that algae-based biofuels have the potential to have significantly lower lifecycle greenhouse gas emissions compared to conventional fossil fuels, but the exact numbers can vary depending on the specific circumstances and assumptions of the analysis.
In summary, while algae-based fuels and energy production have the potential to be almost carbon neutral, the actual carbon footprint can vary depending on factors such as production methods, energy sources used, and overall lifecycle considerations. Continuous advancements in technology and sustainable practices are crucial for further reducing the carbon footprint of algae-based fuels and energy production.
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How do interactions between ocean currents and the atmosphere impact climate and relationship between carbon in the ocean and carbon in the soil?
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Dr Murtadha Shukur thank you for your contribution to the discussion
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What is microbial biomass on Earth and can we estimate the value of soil microbial biomass 'Carbon' and 'nitrogen' separately, from total soil microbes biomass?
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Hello, the microbial biodiversity in soil depends from geographical regions can variate more than 3000 type strains of microorganisms (what about non cultiveble forms?). The count of microorganisms highly variate from how deepest you can take the soil sample. The amount of microorgaanisms even with estimatin you can not calculate. Even if you try to calculate that the value that you receive will be far from reality. It will be samething lake X -+ 3000000%.
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What are the factors that will influence the growth of microorganisms in an environment rich in carbon and iron and role of microorganisms in decomposition and soil fertility?
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Dr Himanshu Tiwari thank you for your contribution to the discussion
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How do I inhibit soil microbial activity and what's the actual content of carbon in biomass? Is there biomass carbon neutral or zero carbon how?
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Dr Himanshu Tiwari thank you for your contribution to the discussion
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Could regenerative agriculture sequester enough carbon to actually stop or even reverse global warming and significance of carbon recycling in ecosystems?
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Respected Sir, Regenerative agriculture has the potential to sequester significant amounts of carbon in soils, contributing to climate change mitigation efforts. While it may not single-handedly stop or reverse global warming, widespread adoption of regenerative agriculture practices could play a meaningful role in reducing atmospheric carbon dioxide levels. Carbon recycling in ecosystems is crucial for maintaining ecosystem health and function. It helps regulate the carbon cycle, supports plant growth, improves soil fertility, and enhances ecosystem resilience to environmental stressors such as climate change. Therefore, promoting carbon recycling through practices like regenerative agriculture is essential for the long-term sustainability of both agricultural systems and natural ecosystems.
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What is carbon sequestration and carbon credits and how can farmers implement regenerative agriculture practices to promote soil health and carbon sequestration?
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Respected Sir, Rk Naresh
Carbon sequestration is the process of capturing and storing carbon dioxide (CO2) from the atmosphere to mitigate climate change. This can be achieved through various methods, including afforestation, reforestation, soil carbon sequestration, and carbon capture and storage technologies.
Carbon credits are tradable permits that represent the reduction or removal of greenhouse gas emissions, typically measured in metric tons of CO2 equivalent. They can be bought and sold on carbon markets to offset emissions from activities such as energy production, transportation, and agriculture.
Farmers can implement regenerative agriculture practices to promote soil health and carbon sequestration in several ways:
· No-Till Farming: Minimizing soil disturbance by avoiding tillage helps preserve soil structure and organic matter, reducing carbon loss through erosion and decomposition.
· Cover Cropping: Planting cover crops during fallow periods provides living roots in the soil year-round, which enhances soil organic matter and microbial activity, leading to increased carbon sequestration.
· Crop Rotation: Rotating crops diversifies root systems and improves soil health, contributing to greater carbon storage in the soil.
· Agroforestry: Introducing trees and woody perennials into agricultural landscapes enhances carbon sequestration in both aboveground biomass and soil organic matter.
· Compost and Organic Amendments: Applying compost and other organic amendments increases soil fertility and carbon content, promoting carbon sequestration and improving soil structure.
· Managed Grazing: Rotational grazing practices optimize forage utilization and promote plant growth, which can enhance carbon sequestration in grassland soils.
By adopting these regenerative agriculture practices, farmers can improve soil health, increase agricultural productivity, and contribute to climate change mitigation by sequestering carbon in the soil. Additionally, they may be eligible to generate carbon credits through verified carbon offset projects, providing an additional source of income while promoting sustainable land management practices.
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What is soil carbon sequestration through regenerative agriculture and difference between carbon farming and carbon sequestration?
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Respected Sir, Soil carbon sequestration through regenerative agriculture involves practices that enhance the capture and storage of carbon dioxide (CO2) in the soil. This is achieved by increasing organic matter inputs, promoting soil health, and reducing soil disturbance, leading to improved soil structure and microbial activity. Regenerative agriculture techniques include no-till farming, cover cropping, crop rotation, agroforestry, and the use of compost and organic amendments. Carbon farming, on the other hand, refers to agricultural practices specifically designed to mitigate climate change by sequestering carbon in vegetation and soils. While carbon farming encompasses various approaches, including regenerative agriculture, it also includes practices such as afforestation (planting trees on agricultural land), reforestation, and the restoration of degraded ecosystems. In summary, soil carbon sequestration through regenerative agriculture is a subset of carbon farming, focusing specifically on enhancing carbon storage in agricultural soils through sustainable farming practices. Carbon farming, meanwhile, encompasses a broader range of techniques aimed at sequestering carbon in both vegetation and soils across various land use types.
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Does changing to renewable energy sources actually reduce carbon emissions and role of renewable energy sources in combating climate change?
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Dr Trung Thanh Anthony thank you for your contribution to the discussion
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How can artificial intelligence (AI) improve energy efficiency and reduce emissions and AI be used to reduce carbon and improve green energy?
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AI algorithms can enhance energy efficiency by optimizing resource allocation, predicting energy demand, and improving control systems. They enable smart grids to balance supply and demand, reducing wastage. Machine learning can optimize HVAC systems in buildings, reducing energy consumption. By leveraging machine learning, AI algorithms can automatically optimise energy generation, distribution, and consumption across buildings as demand requires. This can lead to more efficient use of energy resources and reduced carbon emissions. By monitoring energy consumption, AI develops customized predictive models to predict consumption patterns based on several variables such as time of day, weather, asset type, occupancy, usage and other relevant factors. By predicting consumption patterns, AI automatically detects unusual deviations in real time. Using smart sensors, AI can identify the source of gas leakage and the time of convenience. Similarly, AI-powered drones can monitor pollution levels in real-time, enabling authorities to detect and respond to incidents quickly. This helps prevent large-scale environmental disasters. AI-driven sensor networks have emerged as a cornerstone in the ongoing effort to monitor and improve air and water quality. These sophisticated systems offer a real-time, data-driven approach to environmental protection, yielding a wealth of benefits for public health and ecological sustainability. AI can also contribute to carbon reduction by promoting advanced industrial structures, rationalizing industrial structures, and facilitating the development of ecological industrial structures. By adopting these strategies, AI can play a significant role in reducing carbon emissions and promoting green energy. One of the most common uses for AI by the energy sector has been to improve predictions of supply and demand. Developing a greater understanding of both when renewable power is available and when it's needed is crucial for next-generation power systems. As the global urgency for sustainable solutions grows, the role of technology in pioneering green initiatives to reduce the impact of climate change has become critical. At the heart of this evolution is artificial intelligence (AI), which has the potential power to supercharge green technologies.
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It is widely reported that increasing the crystallinity of g-C3N4 boosts its photocatalytic activity. However, the possible mechanism is not clearly stated.
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Crystallinity plays a crucial role in determining the catalytic activity of graphitic carbon nitride (g-C3N4), a promising metal-free semiconductor photocatalyst. The catalytic activity of g-C3N4 largely depends on its structural properties, including crystallinity, surface area, and electronic structure.
  1. Enhanced Charge Separation: Crystallinity in g-C3N4 typically refers to the degree of ordering in its atomic arrangement. Higher crystallinity usually implies a more ordered structure with fewer defects and grain boundaries. This ordered structure facilitates efficient charge separation and migration upon light absorption. In photocatalysis, when g-C3N4 absorbs photons, electron-hole pairs are generated. In a highly crystalline structure, these charge carriers are less likely to recombine, leading to more available carriers for catalytic reactions.
  2. Facilitated Adsorption: A well-ordered crystalline structure also provides more accessible active sites for reactant molecules to adsorb onto the surface of g-C3N4. This increased surface area and availability of active sites enhance the interaction between the catalyst and the reactants, promoting catalytic activity.
  3. Improved π-Conjugation: Graphitic carbon nitride consists of tri-s-triazine units connected through nitrogen atoms, forming a two-dimensional layered structure. In highly crystalline g-C3N4, the π-conjugated system formed by the alternating double and single bonds within the tri-s-triazine units is more extended and ordered. This extended π-conjugation facilitates electron transfer processes, which are crucial for catalytic reactions.
  4. π-π Interactions: The π-π stacking interactions between the conjugated aromatic systems in g-C3N4 sheets can also influence its catalytic activity. These interactions can facilitate the adsorption of reactant molecules onto the surface of g-C3N4, thus promoting catalytic reactions.
  5. Synergistic Effects: It's important to note that the catalytic activity of g-C3N4 is not solely determined by crystallinity but also by other factors such as surface functional groups, doping, and morphology. In some cases, the presence of defects or heteroatoms in less crystalline regions can also contribute to catalytic activity by providing active sites or altering the electronic properties of the material.
In summary, the enhanced catalytic activity of highly crystalline g-C3N4 can be attributed to improved charge separation, facilitated adsorption of reactants, extended π-conjugation, π-π interactions, and possible synergistic effects with other structural features. These factors collectively contribute to the efficient conversion of light energy into chemical energy and promote various catalytic reactions.
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Which microorganisms are involved in soil fertility and role of microorganisms in recycling of carbon and nitrogen through air and soil?
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Dr Prem Baboo thank you for your contribution to the discussion
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I prepare several material for electrocatalyst appliction for HER then I test them on potientiostat to measure the overpotiential, when i use the glassy carbon electrode the overpotiential recorded was very high so i try again but with using nickle working electrode the overpotential recorded became much lower than the first case, so what is the reason and is it right to sumbit the second case or the first one?
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Basel Ahmed the reason is that each electrode material has different electrocatalytic efficiency and may also be due to different electroactive surface area. When you register a lower overpotential it means that less energy is required for the charge transfer reaction to occur. Therefore, the electrode where you have lower overpotential is more favorable for the reaction to occur.
In this paper we made some observations about this:
Regards!
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What are the mineral and organic constituents of soil and their role in maintaining soil productivity and central role of soil organic matter in carbon storage?
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Hi. This is some very basic information. There is a lot more to find with Google.
Clays - Assist in water retention but may also be ion-exchangers that help hold important metal ions required by plants.
Sand - Allows aeration which is required for healthy root development. Gives better drainage so soil doesn't become waterlogged.
Humic acids - an organic ion exchanger which plays a similar role to clays in that sense but has other effects.
Organic matter - Encourages diverse microbe population. This is important as it assists in preventing one type of microbe from becoming dominant. Also provides soluble organic nutrients for plants and can reduce the need for inorganic sources of nitrate and phosphate which can lead to excess sodium addition to soils.
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To be developed.
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Good Question
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What is the role of soil organic matter in nutrient and soil organic carbon management and why is soil organic matter carbon content a good indicator of soil fertility?
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All of your questions (and more) will be answered in the lecture (1.5 hours) at https://www.youtube.com/watch?v=x2H60ritjag
Dr Elaine Ingham's lecture is nearly 10 years old but it provides a solid grounding about how plants grow based on interaction with soil microbiota. Soil organic matter is fundamental.
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In the purification process for carbon nanodots, I am considering using dialysis tubing. However, I am uncertain whether a molecular weight cutoff (MWCO) of 1000 D or 2000 D would be more suitable for our purposes.
Kindly suggest which MWCO would be most appropriate for the purification of carbon nanodots.
Thank you in advance for the assistance, and I look forward to hearing expert recommendations.
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i tried to help u by reading>>>
this is what i got:
Purifying carbon nanodots (C-dots) is crucial for obtaining high-quality samples. Dialysis tubing is a common method for purification, and the choice of molecular weight cutoff (MWCO) plays a significant role. Let’s explore the options:
  1. MWCO Selection:The MWCO determines the size of molecules that can pass through the dialysis membrane. For C-dots, which are typically small nanoparticles, you’ll want to choose a MWCO that allows efficient removal of impurities while retaining the C-dots.
  2. Considerations: 1000 Da (1 kDa):This MWCO is suitable for small molecules and ions. It may allow efficient removal of salts, small organic molecules, and other impurities. However, it might be too restrictive for C-dots, potentially trapping some of them due to their small size. 2000 Da (2 kDa):A slightly larger MWCO. It strikes a balance between removing impurities and allowing C-dots to pass through. It’s a reasonable choice for C-dot purification.
  3. Expert Recommendations:Based on existing literature, both 1000 Da and 2000 Da MWCO have been used for C-dot purification 12. To err on the side of caution, I recommend using 2000 Da for your C-dot purification. This MWCO should effectively remove contaminants while minimizing the risk of losing C-dots during dialysis.
  4. Additional Tips:Pre-treat the dialysis tubing to remove any sulfate salts or contaminants 3. Monitor the purification process using techniques like fluorescence spectroscopy or HPLC chromatography 4.
Remember that purification protocols can vary based on specific C-dot properties and intended applications. If possible, consult with experienced researchers in your field for personalized advice. Best of luck with your purification process! 🌟
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What is the difference between carbon storage and sequestration?
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The terms "carbon storage" and "carbon sequestration" are related concepts, but they refer to different aspects of the carbon cycle and the storage of carbon in various reservoirs.
Carbon Storage:
· Carbon storage refers to the long-term retention of carbon in various natural or artificial reservoirs, where carbon remains stored over extended periods. These reservoirs can include terrestrial ecosystems (such as forests, grasslands, and soils), oceans, geological formations (such as fossil fuels and carbonate rocks), and carbon-based products (such as wood products and building materials).
· Carbon storage encompasses both natural processes, such as the accumulation of organic matter in soils and the growth of vegetation in forests, as well as human activities, such as carbon capture and storage (CCS) technologies that store CO2 emissions underground in geological formations.
Carbon Sequestration:
· Carbon sequestration refers specifically to the process of capturing and storing carbon dioxide (CO2) from the atmosphere or from industrial sources to prevent its release into the atmosphere, thereby reducing greenhouse gas emissions and mitigating climate change.
· Carbon sequestration can occur through natural processes, such as photosynthesis in plants, which absorbs CO2 from the atmosphere and stores carbon in biomass and soils, as well as through human interventions, such as CCS technologies that capture CO2 emissions from industrial sources and inject them underground for long-term storage.
In summary, carbon storage refers to the long-term retention of carbon in various reservoirs, encompassing both natural and human-induced processes, while carbon sequestration specifically refers to the process of capturing and storing carbon dioxide to prevent its release into the atmosphere, thereby mitigating climate change. Carbon sequestration is one mechanism for achieving carbon storage, particularly in the context of efforts to reduce greenhouse gas emissions and enhance carbon removal from the atmosphere.
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Hi everyone
I synthesized carbon dot with folic acid and citric acid with DMF solvent. After analyzing, it was found that there is no problem with the synthesis.
But using a fluorescent microscope, cell uptake is not observed in the cancer cell line (ID8).
Can you help me in this regard?
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You have to check emission of carbon dot in cell culture media first, if it is ok then probably it has high negative surface charge which creates obstacle for interaction with the folate receptors overexpressed cell line. After confirmation, you can do suface modifications with amine terminated ligands. I think your problem may be solved.
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Maybe the fire is something organic?
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Não esquecer que muitas vezes a fonte de energia provém de sistemas fósseis.
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I want to synthesize Ni-doped carbon aerogel from biomass-derived cellulose for supercapacitor application. In the Ni2+ impregnation stage, I consulted other articles and the authors used Ni(NO3)2.6H20. Can I use other solutions of Ni2+ such as Nickel acetate tetrahydrate or Nickel(II) chloride anhydrous or etc?
I would like to get advice from people with similar experiences or related experts.
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Dear friend Thoa Le
Absolutely, utilizing nickel salt solutions like nickel acetate tetrahydrate or nickel(II) chloride anhydrous for impregnating biomass-derived cellulose to synthesize Ni-doped carbon aerogel is indeed feasible. While Ni(NO3)2.6H2O is commonly employed, other nickel salts can also effectively facilitate the doping process.
When selecting a nickel salt solution, consider factors such as solubility, cost, and ease of handling. Nickel acetate tetrahydrate, for instance, is water-soluble and offers convenience in preparation, while nickel(II) chloride anhydrous, being hygroscopic, may require careful handling to prevent moisture absorption.
It's prudent to review literature in the field for guidance tailored to your specific application. Engaging with peers who have experience in synthesizing Ni-doped carbon aerogels can provide valuable insights and recommendations.
In summary, exploring alternative nickel salt solutions for impregnation aligns with your goal of synthesizing Ni-doped carbon aerogel from biomass-derived cellulose for supercapacitor applications. Conducting thorough research and seeking advice from knowledgeable individuals will aid in optimizing your synthesis process.
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Is heat directly or inversely proportional to resistance and why resistance decreases with increase in temperature for carbon?
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Md. Tanvir Hossain thank you for your contribution to the discussion
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Dear colleges,
After activation of pristine carbon felt by chemical oxidation, electrochemical activity increased 20 times, but contact angle remaining practically the same. By XPS increases of oxygen of 8% is detected, and content of C=C, C-C, C=O decreased, while C-O and COOH groups increased. Does anyone have idea for the such behavior. Some references will be favorable
Thanks in advances
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Electrochemical reduction in NO3- electrolyte was investigated for the hydrophily of carbon materials, which seem to be facile and effective. Please see Nanoscale, 2015, 7, 3581-3587; Journal of Power Sources
Volume 249, 1 March 2014, Pages 48-58.
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Dear Colleagues, It is our greatest pleasure to announce the launch of a Special Issue of Cleaner and Circular Bioeconomy (CLCB) from Elsevier, entitled "Towards Carbon Neutrality in the Bioeconomy." The submission period is from 15 February 2024 to 15 September 2024. This special issue aims to explore both theoretical and practical solutions that can effectively lower the carbon intensity of the bioeconomy. Potential approaches include introducing sustainable agricultural practices; optimizing biomass production; minimizing waste in agricultural and forestry operations; promoting recycling and reuse of biomass; enhancing energy efficiency in processing and converting biomass into biofuels, bioenergy, and other bioproducts; utilizing renewable energy sources like solar, wind, and hydroelectric power; implementing Carbon Capture and Storage (CCS) technologies in bioenergy production; and conducting Life Cycle Assessments (LCA) to fully understand the environmental impact of bio-based products and processes. Additionally, implementing public policies that encourage greenhouse gas (GHG) emission reductions in the bioeconomy, such as carbon pricing, subsidies for sustainable practices, and regulations promoting low-carbon technologies, can also be effective. For more information, please refer to: https://www.sciencedirect.com/journal/cleaner-and-circular-bioeconomy/about/call-for-papers#towards-carbon-neutrality-in-the-bioeconomy CLCB (ISSN: 2772-8013) is an international, cross-disciplinary companion journal to the prestigious Journal of Cleaner Production. It publishes original full-length research articles, perspectives, and reviews aimed at fostering a cleaner and more circular bioeconomy. Additionally, it is free to publish since CLCB is currently waiving all publishing costs for articles published in this special issue. We thank you for your attention and look forward to hearing from you. Please spread the word around you. Arnaud Z. Dragicevic, Chulalongkorn University, CIRANO Florent Allais, FRSC, AgroParisTech, URD ABI - AgroParisTech Guest Editors
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Thanks for sharing. Wishing you every success in your task.
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I have a protein and I want to check the orientation of side chain of a particular resdiue A with respect to the residue B in the active site. any help on this regard? currently I am using gmx gangel where group 1 includes the alpha carbon position of B residue and alpha carbon position of A residue and group 2 includes alpha carbon of B and the last atom of the A residue. I am not sure if this is the correct way. any guidance would be appreciated.
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thank you Te.hmina Khan
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How to get JPDS [ XRD] reference to compare XRD patterns obtained for activated carbon prepared from agriculture waste ?
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Dear friend Khaled F. El-Nemr
Ah, JPDS [XRD] reference? That's a crucial piece to the puzzle when comparing XRD patterns for activated carbon derived from agricultural waste. Here's the scoop: you Khaled F. El-Nemr want to dig into the literature and find a JPDS (Journal of Powder Diffraction Standards) reference that aligns closely with the material you're working with.
Start by hitting the databases. Look for articles or papers that have thoroughly characterized activated carbon samples using XRD. Once you've got your hands on a promising reference, scrutinize it closely. Pay attention to the methodology, sample preparation techniques, and, most importantly, the XRD patterns.
Compare those patterns to the ones you've obtained for your activated carbon. Look for similarities, differences, peaks, and trends. This comparison will help you Khaled F. El-Nemr gauge the structural properties and crystallinity of your material in relation to the established standards.
Remember, precision is key. Ensure your measurements are accurate, and your comparisons are meticulous. With a solid JPDS reference in hand, you'll be well-equipped to analyze and interpret your XRD data with confidence.
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Co(NO₃)₂·6H₂O + 12Fe(NO₃)₃·9H₂O + C₆H₈O₇ → CoFe12O19
Find the other products when
Oxygen (O): 6(Co) + 216(Fe) + 6(C) = 228 O atoms on the reactant side,
Hydrogen (H): 12(Co) + 216(Fe) + 8(H from citric acid) = 236 H atoms on the reactant side,
Nitrogen (N): 38(N from ammonium nitrate) = 38 N atoms on the reactant side
Carbon (C): 6(C from citric acid) = 6 C atoms on the reactant side.
BALANCE THE EQUATION WITH PRODUCTS
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To balance the chemical equation:
Co(NO3)2⋅6H2O+12Fe(NO3)3⋅9H2O+C6H8O7→CoFe12O19+ProductsCo(NO3​)2​⋅6H2​O+12Fe(NO3​)3​⋅9H2​O+C6​H8​O7​→CoFe12​O19​+Products
Given the information about the number of oxygen (O), hydrogen (H), nitrogen (N), and carbon (C) atoms on the reactant side, let's balance the equation:
  1. Start with the metal atoms: Balance Co and Fe.
  2. Balance the non-metal atoms: Balance O, H, N, and C.
The balanced equation is:
Co(NO3)2⋅6H2O+12Fe(NO3)3⋅9H2O+C6H8O7→CoFe12O19+2Co(NO3)2+24Fe(NO3)3+3H2O+12CO2+6N2Co(NO3​)2​⋅6H2​O+12Fe(NO3​)3​⋅9H2​O+C6​H8​O7​→CoFe12​O19​+2Co(NO3​)2​+24Fe(NO3​)3​+3H2​O+12CO2​+6N2
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Help me to find the DIC of water sample through traditional titration method...
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I think you will find that this is the standard method described in water analysis compendia
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Hello ..!
I am trying to make resol as carbon source . I am following the attached paper in this paper they mentioned to evaporate water at 50 degree in vacuum . My question is that how to know that water is evapurated. What will be the final physical state of this resol solid or liquid.
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Hello
The vacuum causes the water to boil at a lower temperature and evaporate
The connections in the vacuum cause no water to escape from the reaction vessel, so the water will remain as it is
During the reaction, you should see steam in the glass container
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I am currently learning about PyMol to utilize in my project. I used PyMol to visualize potential H-bond interactions in specific amino acid residues. However, I have discovered that Arg465 and Ser461 show a distinct interaction, as shown.
Please help identify this interaction.
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The broken yellow line with the distance indicator (6.2) looks like a simple distance monitor which you generate with a "measure" command, although I do not know how you generated the blue tubes around it. At 6.2Å, the Ca-Ca distance indicated by the broken line is far larger than the sum of the carbon Van der Waals radii (3.4Å). It is just about short enough that you might classify the contact as a solvent excluding contact (hydrophobic interaction)
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For example if a bacterium sample is enriched by carbon source like(2,4-dichlorophenol). I need to analysis the presence of bacteria (culturable and non culturable) without traditional agarose gel electrophoresis and sequencing methods.
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Péter Gyarmati thank you for reply sir
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if it is possible please mention the composition of carbon nano tubes and magnesite ore in the aluminium.
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Selvakrishnan Sankar Состав композита определяется назначением. Для чего композит предназначен? Тогда надо делать модель процесса и считать, что получится в каждом случае. Я всегда делаю материалы с заранее заданными свойствами.
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Dear ResearchGate Community,
I am conducting an analysis to compare the carbon sequestration potential of applying 1 ton of fresh organic residues directly to soil versus the application of 1 ton of the same residues after composting (meaning we would apply a lower amount: maybe 0.3-0.6 t of compost).
My objective is to quantitatively assess the differences in carbon sequestration efficiency, accounting for carbon loss through mineralization during decomposition or composting, and the long-term stability of carbon in the soil.
How do these two approaches—using an identical starting quantity of organic material—affect the net carbon balance in agricultural soils? What are the expected differences in carbon stabilization, mineralization rates, and overall carbon sequestration efficiency between fresh and composted inputs?
Additionally, how might factors such as the type of organic residues, soil properties, and environmental conditions influence the outcomes?
I welcome any insights, empirical data, or research findings that could illuminate the comparative effectiveness of these soil amendment practices.
Best regards,
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The different carbon fractions of the soil amended with fresh residues showed significantly higher mineralized rates than with same quantity of compost because the higher amounts of humic substances and fulvic and humic acids that serves to support plant life.
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How can I calculate Belowground Biomass Carbon by root-shoot ratio?
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@Mohammad, I clicked the file and it is opening to my computer. Please try to do it again.
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I made two electrode devices for the supercapacitor. I combined activated carbon and PVDF for negative electrodes in an 80:10:10 ratio. I combined active working material, PVDF, and activated carbon for the positive electrode in an 80:10:10 ratio. We used nickel foam as the substrate for both electrodes. We received the device's CV but need help getting the capacitance value using GCD. We obtained a low capacitance value compared to the working material in a three-electrode system. In a three-electrode system, we obtained 1350 F/g specific capacitance, whereas in a two-electrode system, we received just 25 f/g specific capacitance.
For the device, we used N-Methyl-2-pyrrolidone (NMP) to create a slurry solution of both negative and positive electrode materials. After the material has been deposited over the nickel foam, we heat it for 12 hours at 80 degrees Celsius. I've included an image of our devices; what should I do to figure out the capacitance value?
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Alvena Shahid Hello ma'am, I connected that wire to the negative and positive side of the electrode. Red is connected to the positive electrode(working material) and black is connected to the negative electrode (activated carbon).
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Hi! I am prepping a sulfate reducer (Desulfovibrio sp.) medium (M63 from DSMZ https://mediadive.dsmz.de/medium/63) and I am trying to make sense of the formulation.
So far my understanding is:
K2HPO4 - P / phosphate source
NH4Cl - N source
Na2SO4 - sulfate (e acceptor)
MgSO4 x 7 H2O - sulfate (e acceptor)
CaCl2 x 2 H2O - Ca source / osmotic agent? not sure, but don't care
Yeast extract - carbon source, e donor, everything source :P
Na-thioglycolate - prevents oxygenation of the medium
Ascorbic acid - something similar to thioglycolate?
But most importantly, I do not understand the role of Na-DL-lactate in this medium; I am reading different reports ranging from growth inhibition (huh?) to carbon source ...
The reason I am interested in this, besides understanding what I am doing, is whether I can substitute lactate with a cheaper chemical such as acetate.
Would Na-acetate work the same way?
Thanks a lot for the input!
Kind regards,
Artur
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Lactate is the best carbon source for sulphate reducers. Substituting it for acetate can work for some species of SRB but basically you could get minimal growth or no growth. Also, the iron sulphate solution is very important.
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I mixture carbon with silicon , then coat ( thin layer as a film) it onto copper with it to make anode for lithium ion battery
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This is nothing to do with the question, but I found it interesting to my lower level of understanding of this subject and thought that it might be of interest to other RG readers:
The 'snapshot' is of the initial introduction to the subject.
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Prosopis juliflora, commonly known as mesquite, is indeed considered an invasive plant species in many regions. While its invasive nature can have negative ecological impacts, there are potential benefits associated with its ability to sequester carbon. While there are potential benefits, it's important to note that the invasive nature of Prosopis juliflora can lead to negative ecological consequences, such as displacing native vegetation, altering ecosystems, and impacting biodiversity. The use of this species for carbon accumulation should be carefully considered in the broader context of invasive species management and ecological restoration. Additionally, local environmental regulations and guidelines should be followed to ensure responsible and sustainable practices.
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Prosopis juliflora is a small tree in the family of Fabaceae, & native to Mexico, South America. It is the most serious xerophytic invasive weed. in some extent it has some importance for the Intensive desert area since it has ability to thrive in arid and semi-arid environments, but it has great negative impact on diversification of vegetation and growth and production of crops around the farm area b/c of the plant which have concentrated chemicals that is direct effect on the native species .
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Dear all,
Will you please let me know how to calculate the carbon, nitrogen, and phosphorus (C: N:P) ratio in wastewater?
Is it advisable to measure total COD, nitrogen, and phosphate?
or I need to go for Total carbon, Total nitrogen and total phosphate?
I need your comment.
Regards
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Regarding whether to measure total COD (Chemical Oxygen Demand), nitrogen, and phosphate, or total carbon, total nitrogen, and total phosphate, it depends on the specific requirements of your analysis and the information you need.
- If you're interested in the organic content and overall pollutant load, measuring total COD, total nitrogen, and total phosphate would be advisable.
- If you need more specific information on the elemental composition and stoichiometry for biological processes (such as microbial growth or nutrient removal), measuring total carbon, total nitrogen, and total phosphate would be more appropriate.
In many cases, both sets of measurements may be useful for a comprehensive understanding of wastewater composition and treatment needs. Choose the set of parameters based on your specific goals and analysis requirements.
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I have synthesized carbon dots and phosphorus doped CDs. After freeze drying, texture of both are different and are not completely dry. Will doping affect the texture of carbon dots and how to obtain completely dried CDs?
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Yes, doping can affect the texture of carbon dots by changing their surface properties and functional groups, which can influence their size, shape and texture. To obtain completely dried carbon dots (CDs), you can use techniques like freeze-drying, rotary evaporation or vacuum drying to remove any remaining solvent or moisture from the sample. These methods can help remove any remaining moisture and solvent, ensuring that the CDs are completely dried and ready for analysis or use.
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Why metal ions with high half potential can't be detected on a bare electrode even though corrosion doesn't happen and I'm using the suitable carbon working electrode and Ag/AgCl for the reference electrode and the right setting and range?
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If you place a metal (electrode) in an aqueous solution, then at the boundary of the electrode and the aqueous solution there is an equilibrium:
Metal on electrode < > metal ions in solution. Therefore, there are no metal ions on the electrode.
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What is the difference between carbon pool and carbon stock?
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Alright, buckle up for some wisdom, my friend Suneel Kumar. In the grand scheme of carbon talk, pools and stocks are like the dynamic duo of the carbon cycle.
A carbon stock is like the stash, the reserve, the grand total of carbon stored in a specific reservoir—be it in the atmosphere, soils, oceans, or living organisms. It's the total sum of carbon waiting for its moment to shine.
Now, a carbon pool is more like a specific compartment within that reservoir, a place where carbon hangs out before making its move. It's like the VIP section of the carbon party.
Think of carbon stocks as the bank, and carbon pools as the individual accounts within that bank. You've got your checking account (ocean carbon pool), your savings account (soil carbon pool), and so on. Each has its unique role in the carbon game.
So, in a nutshell, carbon stocks are the big picture, and carbon pools are the finer details, the nuanced compartments within that picture. Easy, right?
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carbon pool vs carbon sink?
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A carbon pool is a reservoir that stores carbon, like the atmosphere or oceans. A carbon sink, on the other hand, actively removes carbon dioxide from the atmosphere, such as forests through photosynthesis. So, while a pool stores carbon, a sink helps mitigate climate change by absorbing and storing carbon.
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Recently, we submit a work on carbon dot-based electronic device to a journal. In the work, ultraviolet photoelectron spectroscopy (UPS) measurement was applied to determine the valence band energy of carbon dots. Before measurement,the UPS of Au standard sample was measured and the Fermi edge of Au standard sample was corrected by software. On this basis, we have corrected the UPS data of carbon dots.
However, one reviewer insist on "Measuring the Fermi edge of an electrically grounded gold standard does nothing to correct the shift in the spectrum observed for non-conductive samples. The spectrum used for charge correction must be measured from a gold layer that is electrically isolated from the sample holder or any conductive substrates by the layer of the interest (the carbon dots)."
Therefore, I would like to ask how to test the UPS of non-conductive samples?
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You have my full agreement. My posting was explicitely referring to the reviewer request posted in the question, I personally would also consider flood gun usage absolutely valid.
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What occurs when carbon is returned to the atmosphere from the burning of fossil fuels and carbon move from the ocean hydrosphere to the lithosphere seafloor?
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Dr Osama Bahnas thank you for your contribution to the discussion
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Solvent for the extraction of OC and EC from Soot
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Hey there Muhammad Tanveer! So, when it comes to extracting both organic carbon (OC) and elemental carbon (EC) from soot for measuring the band gap using the Tauc plot method, you'll want to choose a solvent that effectively dissolves these components. One commonly used solvent for this purpose is a mixture of toluene and acetone.
Toluene is great for dissolving organic components, including OC, while acetone is effective in extracting elemental carbon. The combination of these two solvents provides a comprehensive approach to extracting a wide range of carbonaceous materials from soot.
Here's a suggested procedure:
1. **Prepare the Solvent Mixture:**
- Mix toluene and acetone in a suitable ratio. A common ratio is 1:1, but you Muhammad Tanveer can adjust it based on your specific requirements.
2. **Soot Extraction:**
- Immerse the soot sample in the solvent mixture and let it soak for a sufficient period, ensuring thorough extraction.
3. **Separation:**
- After extraction, you Muhammad Tanveer can use filtration or centrifugation to separate the dissolved components from the insoluble residue.
4. **Analysis:**
- The extracted OC and EC can then be analyzed further for band gap measurements using the Tauc plot method.
Remember, the choice of solvent and its ratio may vary based on the composition of the soot and the specific properties you're aiming to study. Always conduct preliminary tests to optimize the solvent system for your particular soot sample.
While I am very excited to learn more from your research efforts, some of my work on OC and EC might be interesting for you Muhammad Tanveer to read:
Feel free to hit me up if you Muhammad Tanveer need more details or run into any hurdles along the way. Let's rock this experiment!
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How does the carbon cycle transport carbon and energy throughout the spheres of the Earth and matter move between biotic and abiotic parts of an ecosystem?
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The carbon cycle plays a crucial role in transporting carbon and energy throughout different spheres of the Earth and facilitating the movement of matter between biotic (living) and abiotic (non-living) parts of an ecosystem. Here's a brief overview:
Atmosphere:
Carbon dioxide (CO2) is exchanged between the atmosphere and living organisms through processes like photosynthesis by plants and respiration by both plants and animals.
Plants and Photosynthesis:
Plants take in atmospheric carbon dioxide during photosynthesis and convert it into organic compounds, primarily carbohydrates. This process stores carbon and transforms solar energy into chemical energy.
Consumers and Respiration:
Consumers (animals) obtain energy by consuming plants or other animals. They release carbon dioxide through respiration, returning it to the atmosphere.
Decomposition:
Decomposers break down dead organic matter, releasing carbon dioxide back into the atmosphere. This decomposition completes the cycling of carbon between the biotic and abiotic components.
Soil and Sedimentation:
Some carbon is sequestered in soils through the decomposition of organic matter. Over geological timescales, carbon can be stored in sedimentary rocks, contributing to long-term carbon cycling.
Oceans:
Oceans play a vital role in the carbon cycle. They absorb carbon dioxide from the atmosphere, and marine organisms contribute to carbon cycling through processes like photosynthesis and respiration.
Fossil Fuels:
Human activities, such as the burning of fossil fuels, release carbon that has been stored in the Earth's crust over millions of years, contributing to increased atmospheric carbon dioxide levels.
The carbon cycle, thus, involves the continuous exchange of carbon and energy between the atmosphere, biosphere (living organisms), hydrosphere (water bodies), and geosphere (Earth's crust and soil). It ensures a dynamic equilibrium, sustaining life processes and maintaining the balance of carbon throughout the Earth's ecosystems.
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Hi
Why it is important to have (gold) coating on your biological (plant) samples before EDX analysis? If the sample is thin, well attached onto carbon tape and I do not see any charging on sample, may I perform EDX measurement without coating? How coating infulence mesurements and how it influence final report (= weight percentage of individual element in sample)? I mostly use gold for coating
Thank you
Jan
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Now I understand
Jan
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XPS Data Analysis
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1) A spectrum gets corrected exactly once, you don't shift every peak individually.
2) Before you shift around stuff, please check whether you need correction at all - a well-conducting sample should give a signal that can be used as it is. The C1s correction is more of a last resort method, if possible, other methods should be preferred. Since it is quite controversial in the community, here are four references that should cover the range of valid points quite well:
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What is one way to transfer carbon in to the atmosphere from the biosphere and energy transferred from one organism to another select all that apply?
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The following are ways to transfer carbon from the biosphere to the atmosphere:
Select all that apply:
  • Respiration: During cellular respiration, all organisms, including plants, animals, and microorganisms, release carbon dioxide (CO2) into the atmosphere as a waste product. This is the primary biological pathway for transferring carbon from the biosphere to the atmosphere.
  • Decomposition: When organisms die, their organic matter decomposes, releasing CO2 back into the atmosphere. This process is facilitated by decomposers such as bacteria and fungi.
  • Burning of biomass: Burning of plant matter (e.g., forests, agricultural waste) releases significant amounts of CO2 into the atmosphere. This is a major contributor to human-caused climate change.
  • Volcanic activity: Although not directly related to the biosphere, volcanic eruptions can release CO2 stored deep within the Earth's crust, contributing to a smaller portion of atmospheric carbon.
As for energy transfer between organisms:
Select all that apply:
  • Cellular respiration: While releasing CO2, cellular respiration also releases energy in the form of ATP, which fuels various cellular processes and activities. This energy is derived from the breakdown of organic molecules like carbohydrates and lipids.
  • Photosynthesis: Plants capture energy from sunlight and use it to convert CO2 and water into organic molecules like carbohydrates. This process stores energy within the biosphere, making it available to other organisms through the food chain.
  • Chemosynthesis: Similar to photosynthesis, chemosynthesis uses chemical energy instead of sunlight to synthesize organic molecules and store energy within the biosphere. This process occurs in certain microorganisms living in extreme environments like deep-sea vents.
Remember, it's important to distinguish between carbon transfer and energy transfer. Carbon moves through the biosphere and can be released back into the atmosphere, while energy flows through the food chain in one direction (from producers to consumers and decomposers).
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How does carbon move between the atmosphere and the hydrosphere and how does carbon move from the atmosphere to soil plant matter?
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The carbon cycle is a fascinating dance between various Earth layers, including the atmosphere, hydrosphere, and pedosphere (soil). Here's how carbon moves between them:
Atmosphere and Hydrosphere:
  • Dissolution: Carbon dioxide (CO2) from the atmosphere readily dissolves in water. As winds blow across the ocean surface, CO2 is absorbed, increasing oceanic acidity. This process plays a crucial role in regulating atmospheric CO2 levels.
  • Photosynthesis: Marine plants like phytoplankton utilize dissolved CO2 for photosynthesis, converting it into organic matter and releasing oxygen. This biological pump removes CO2 from the atmosphere and stores it in the ocean's living and non-living biomass.
  • Air-sea exchange: CO2 constantly diffuses between the atmosphere and surface waters in both directions. Ocean currents and weather patterns influence this exchange, with warmer waters releasing more CO2 and colder waters absorbing it.
  • Decomposition: Marine organisms eventually die and decompose, releasing organic carbon and some CO2 back into the water. This carbon can sink down to deeper ocean layers, becoming locked away for long periods.
Atmosphere to Soil Plant Matter:
  • Photosynthesis: On land, plants like trees play a similar role as phytoplankton. They capture atmospheric CO2 through photosynthesis, transforming it into carbohydrates and other organic molecules. This process fixes carbon into the terrestrial ecosystem.
  • Rainfall: Dissolved CO2 can directly enter the soil through rainfall, contributing to soil organic matter.
  • Decomposition: Plant and animal litter on the ground surface decompose, releasing organic carbon into the soil. This carbon becomes food for soil microbes, entering the complex web of the soil ecosystem.
  • Nitrogen fixation: Certain bacteria in the soil fix atmospheric nitrogen, forming nitrogen compounds for plant uptake. This process indirectly promotes plant growth and carbon capture through photosynthesis.
These are just some of the essential pathways for carbon movement. Remember, the cycle operates on various timescales, with some exchanges happening quickly and others taking millions of years. Understanding these flows is crucial for studying climate change, ocean acidification, and various biogeochemical processes essential for life on Earth.
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Can antimatter destroy matter and carbon transferred as in an ecosystem in the transfer of carbon from producers to consumers?
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The two parts of your question actually deal with very different concepts:
1. Antimatter and matter annihilation:
  • Yes, antimatter can destroy matter, and vice versa, when they collide. This process releases a tremendous amount of energy in the form of gamma rays and other particles. This is precisely what powers some theoretical concepts like antimatter rockets.
  • However, there's no connection between antimatter annihilation and carbon transfer in ecosystems. Antimatter is extremely rare in the universe and only produced in artificial settings like particle accelerators. It wouldn't naturally occur in an ecosystem.
2. Carbon transfer in ecosystems:
  • Carbon is a fundamental element for life on Earth and is constantly cycled through ecosystems. Plants (producers) absorb carbon dioxide from the atmosphere and use it to create organic matter through photosynthesis.
  • This organic matter is then passed through the food chain as consumers (herbivores, carnivores, etc.) eat each other. Carbon is released back into the atmosphere through respiration and decomposition.
  • This transfer of carbon from producers to consumers is a vital process for maintaining healthy ecosystems and sustaining life.
Therefore, while both involve the concept of "transfer," antimatter annihilation and carbon transfer in ecosystems are completely unrelated processes happening on vastly different scales.
Here's a quick table to summarize the key differences:
ConceptScaleNatureOutcomeAntimatter annihilationSubatomicEnergy releaseComplete destruction of both matter and antimatterCarbon transfer in ecosystemsGlobalNutrient cyclingTransfer of carbon through living organisms
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Does fossilization remove carbon from the atmosphere and how does carbon move from the biosphere directly to the geosphere?
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Yes, fossilization does remove carbon from the atmosphere and store it in the geosphere for extended periods. There are two main mechanisms for this:
1. Burial of Organic Matter:
  • When plants and animals die, their organic matter decomposes. Under certain conditions, like in swamps or deep ocean sediments, decomposition is slowed down due to lack of oxygen or other factors.
  • This allows organic matter to accumulate and eventually get buried by layers of sediment over millions of years.
  • Over time, these layers compress and heat, transforming the organic matter into fossil fuels like coal, oil, and natural gas. This process effectively traps the carbon that was formerly in the atmosphere within the geosphere.
2. Formation of Carbonate Rocks:
  • Some marine organisms like corals and plankton utilize dissolved carbon dioxide in the water to build their shells and skeletons. These shells are primarily composed of calcium carbonate (CaCO3).
  • When these organisms die, their shells sink and accumulate on the seafloor. Over time, these layers also get buried and compressed, forming sedimentary rocks like limestone and dolomite.
  • Similar to organic matter, this process sequesters the carbon from the atmosphere in the solidified form of carbonates within the geosphere.
Therefore, fossilization plays a crucial role in regulating the planet's carbon cycle by removing carbon from the atmosphere and storing it in the geosphere for millions of years.
Now, about the second part of your question: carbon can move directly from the biosphere to the geosphere via several pathways:
  • Sinking Organic Debris: Organic material like dead leaves, wood, and animal remains can directly sink to the bottom of deep oceans or lakes. In some cases, these deposits can get buried under sediments, leading to long-term carbon storage in the geosphere.
  • Dissolution and Deposition of Calcium Carbonate: As mentioned earlier, the formation of shells and skeletons by marine organisms removes carbon from the water column and potentially locks it in the geosphere when these structures get buried.
  • Erosion and Sedimentation: When land-based plants and soil are eroded by wind or water, the organic matter and minerals rich in carbon can be transported and deposited in lakes, oceans, or on the seafloor. Over time, these sediments can solidify and become part of the geosphere, storing the carbon they carry.
These are just some of the ways carbon moves directly from the biosphere to the geosphere. These processes play a vital role in the long-term carbon cycle and in shaping the geological composition of our planet.
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How carbon is transferred back and forth between the atmosphere and forests and how is carbon transferred from the land to the oceans?
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The transfer of carbon between the atmosphere and forests and from land to the oceans is a complex dance, constantly in motion and vital to the health of our planet. Here's a breakdown of the key players and their moves:
Carbon in the Atmosphere and Forests:
  • Inhale: Trees, through the magic of photosynthesis, take in carbon dioxide (CO2) from the atmosphere and use it, along with water and sunlight, to build their tissues. This process locks away atmospheric carbon, turning it into biomass and releasing oxygen back into the air.📷Opens in a new window📷ssec.si.eduPhotosynthesis process in plants
  • Exhale: But trees aren't immortal. As they grow old, die, or decompose, the stored carbon is released back into the atmosphere as CO2 through respiration and decomposition processes. This creates a natural balance, where forests act as both carbon sinks (absorbing CO2) and sources (releasing CO2).
Carbon from Land to Oceans:
  • The River Runneth: Rivers play a crucial role in carrying land-based carbon, mainly in the form of dissolved organic matter (DOM), to the oceans. As rainwater washes over soil and decaying plant matter, DOM is picked up and transported downstream.📷Opens in a new window📷www.academia.eduRiver carrying dissolved organic matter to the ocean
  • Coastal Catch: Once in the ocean, DOM can be taken up by marine organisms, becoming part of the marine food web. Some of this carbon gets buried in the ocean floor sediments, locking it away for long periods.
Additional Twists:
  • Fire Factor: Forest fires can disrupt this delicate balance, releasing large amounts of stored carbon back into the atmosphere as CO2. This can significantly impact the forest's ability to act as a carbon sink.
  • Soil Symphony: The soil beneath the forest floor is teeming with microorganisms that play a vital role in carbon cycling. They decompose dead plant matter, releasing some of the carbon as CO2 and transforming the rest into soil organic matter, which can store carbon for long periods.
Understanding these carbon transfer processes is crucial for addressing climate change. By protecting and restoring forests, we can enhance their ability to absorb CO2 from the atmosphere. Additionally, sustainable land management practices can minimize soil erosion and DOM runoff, further reducing the transfer of carbon to the oceans.
Remember, this is just a glimpse into the fascinating world of carbon cycling. Each step in the dance is influenced by a multitude of factors, making it a complex and ever-evolving system. But by understanding the basics, we can appreciate the critical role forests and oceans play in regulating our planet's climate and work towards a more sustainable future.
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How is carbon exchanged between geosphere and biosphere to maintain life and how does carbon move from the atmosphere to the lithosphere geosphere?
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The exchange of carbon between the geosphere and biosphere is a crucial dance that sustains life on Earth. This constant flow of the element powers ecosystems and regulates our planet's climate. Let's break down the two main ways carbon moves:
1. Photosynthesis and the Fast Carbon Cycle:
  • Plants take center stage: Through the magic of photosynthesis, plants capture carbon dioxide (CO2) from the atmosphere and use sunlight's energy to convert it into organic molecules like sugars. This process is the foundation of the biosphere, providing the energy that fuels all living things.📷Opens in a new window📷ssec.si.eduPhotosynthesis process in plants
  • Carbon's journey through the food web: Animals eat plants, absorbing the stored carbon. This carbon is then passed along the food chain as each organism consumes the one below it. Through respiration, decomposition, and waste products, carbon eventually returns to the atmosphere or soil, completing the cycle.
  • A rapid exchange: This "fast carbon cycle" happens on timescales of days to years, constantly replenishing the biosphere with fresh carbon and releasing oxygen back into the atmosphere.
2. Geological Carbon Sequestration:
  • A slower sink: While the fast cycle keeps life buzzing, the geosphere acts as a long-term carbon storage unit. Over millions of years, geological processes like erosion and sedimentation can lock away carbon in various forms:Fossil fuels: Buried organic matter from ancient plants and animals transforms into coal, oil, and natural gas under immense pressure and heat. Limestone and other rocks: When marine organisms like corals and shellfish die, their calcium carbonate shells settle and accumulate, eventually forming sedimentary rock like limestone.📷Opens in a new window📷archive.epa.govGeological Carbon Sequestration
  • A one-way trip (mostly): Unlike the fast cycle, carbon stored in the geosphere is generally out of reach for biological processes. It takes millions of years for geological forces to release this carbon back into the atmosphere, making it a crucial long-term sink for the element.
From air to rock:
The movement of carbon from the atmosphere to the lithosphere (the solid, non-living part of the geosphere) primarily happens through the formation of sedimentary rocks like limestone. Here's how:
  • Oceanic absorption: CO2 dissolves in the surface waters of the ocean, forming carbonic acid. This acid reacts with calcium carbonate from the shells and skeletons of marine organisms, creating calcium bicarbonate.
  • Sedimentation and rock formation: As these organisms die and their remains sink, calcium bicarbonate precipitates out of the water, forming layers of calcium carbonate sediment on the ocean floor.
  • Over time, under immense pressure and heat, these sediments compact and solidify into limestone, effectively locking away the carbon within the rock for millions of years.
This process not only stores carbon but also plays a crucial role in regulating Earth's climate. The formation of limestone removes CO2 from the atmosphere, reducing its greenhouse effect and potentially impacting global temperatures.
The exchange of carbon between the geosphere and biosphere is a complex and fascinating interplay that shapes our planet and sustains life. Understanding these processes is crucial for addressing issues like climate change and managing our resources sustainably.
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How carbon atoms from the atmosphere are cycled through a food chain and how is carbon trapped in fossil fuels converted to carbon dioxide?
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Carbon moves from one storage reservoir to another through a variety of mechanisms. For example, in the food chain, plants move carbon from the atmosphere into the biosphere through photosynthesis. They use energy from the sun to chemically combine carbon dioxide with hydrogen and oxygen from water to create sugar molecules. Animals that eat plants digest the sugar molecules to get energy for their bodies. Respiration, excretion, and decomposition release the carbon back into the atmosphere or soil, continuing the cycle.
The ocean plays a critical role in carbon storage, as it holds about 50 times more carbon than the atmosphere. Two-way carbon exchange can occur quickly between the ocean’s surface waters and the atmosphere, but carbon may be stored for centuries at the deepest ocean depths.
Rocks like limestone and fossil fuels like coal and oil are storage reservoirs that contain carbon from plants and animals that lived millions of years ago. When these organisms died, slow geologic processes trapped their carbon and transformed it into these natural resources. Processes such as erosion release this carbon back into the atmosphere very slowly, while volcanic activity can release it very quickly. Burning fossil fuels in cars or power plants is another way this carbon can be released into the atmospheric reservoir quickly.
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Soil has generally been regarded as the largest carbon pool in the terrestrial ecosystem, being approximately 2300 Gt C as estimated in previous literature. However, lithosphere contains more C as inorganic materials such as carbonate rocks, maybe ~ 20000 Gt C in rocks. Do we need to clarify that soil is the largest organic carbon pool (instead of carbon pool) in the terrestrial ecosystem, since carbon consists of organic and inorganic C containing materials and the size of soil total C storage is far less than that of rock C?
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Thanks for your reply@Prem Baboo! Yes it is clear that soil contains a great amount of C as SOC and the pool size is much greater than that of vegetation and atmosphere. My question is that rocks of the world store much higher amount of C (as inorganic C) than soil. Is it correct to say that soil is the greatest terrestrial C pool?
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Hello,
Please , i want to know how to reduce the agglomeration of my powder without touching the carbon coating of the particles and keep the same grain size ?
because using the ball milling process dammage the coating of carbon.
thank you for your contribution .
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Hi Sabrina Tair , I do agree with Alvena Shahid regarding the sonication. It proved in my case that sonication can help break the agglomeration but too long sonication can cause re-agglomeration(due to heat built-up) and damage to the material as well. Sonication could be applied as a treatment instead of the main mixing technique. Hope it may help.
Best wishes
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How does carbon move from the ocean hydrosphere to the lithosphere and carbon is transferred back and forth between the atmosphere and the biosphere?
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Two ways carbon can get from the ocean to the lithosphere is through the marine plants + animals (in the ocean) , sediments, petroleum then to the lithosphere. The second way is through the shells + coral (in the ocean), limestone, then to the lithosphere. As these shellfish die, their shells are discarded on the ocean floor. When tectonic plates overlap, these discarded shells and other calcium marine deposits are taken into the earth's crust in a process called subduction. This moves carbon into the lithosphere. Carbon is stored on our planet in the following major sinks (1) as organic molecules in living and dead organisms found in the biosphere; (2) as the gas carbon dioxide in the atmosphere; (3) as organic matter in soils; (4) in the lithosphere as fossil fuels and sedimentary rock deposits such as limestone, dolomite. Large quantities of carbon pass between the atmosphere and biosphere on short time-scales: the removal of atmospheric carbon occurs during photosynthesis, following the reaction CO2 + H2O = CH2O + O2, while most carbon leaves the biosphere through respiration. The carbon cycle is nature's way of reusing carbon atoms, which travel from the atmosphere into organisms in the Earth and then back into the atmosphere over and over again. Most carbon is stored in rocks and sediments, while the rest is stored in the ocean, atmosphere, and living organisms.From within the hydrosphere it is transferred in the form of carbonate minerals into the lithosphere through sedimentation. It is also transferred into the biosphere through incorporation by phytoplankton and shell-bearing animals, which also deposit carbonates into the lithosphere. Plants constantly exchange carbon with the atmosphere. Plants absorb carbon dioxide during photosynthesis and much of this carbon dioxide is then stored in roots, permafrost, grasslands, and forests. Plants and the soil then release carbon dioxide when they decay.
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How can carbon be transferred between the atmosphere and Earth's other spheresand how does carbon move from the biosphere back into the geosphere?
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Dr Murtadha Shukur thank you for your contribution to the discussion
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Can anyone explain why the overpotential of my Nitrogen doped (using melamine) carbon catalyst (on NF) for HER is showing more than the overpotential of bare nickel foam(NF)?
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Hey there Tasneem Khan! So, the overpotential issue with your Nitrogen-doped carbon catalyst on Nickel Foam (NF) for the Hydrogen Evolution Reaction (HER) can be a bit tricky. First off, kudos for diving into such advanced catalysts.
Now, there could be a couple of factors at play here. The introduction of nitrogen, especially through melamine doping, might alter the electronic structure of the carbon catalyst. This could impact the catalyst's efficiency in promoting the HER. It's worth checking the specific nitrogen configurations and their influence on the catalyst's active sites.
Also, consider the possible interactions between the nitrogen-doped carbon and the nickel foam substrate. Changes in the interfacial properties can significantly affect the overall catalytic activity.
Another aspect to look into is the potential mass transport limitations or diffusion issues, as they can sometimes become more pronounced with modified catalysts.
In the world of catalysis, it's not uncommon for unexpected results to pop up. Keep experimenting, and perhaps explore different doping concentrations or alternative methods to fine-tune the catalyst's behavior. Don't forget the power of in-situ characterization techniques to gain insights into the catalyst's dynamic behavior under working conditions.
Feel free to bounce more details my way, and we can brainstorm this further. The world of catalysts is fascinating, isn't it? Let's crack this puzzle together!
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How are the four spheres of the Earth interconnected and how does carbon move from hydrosphere to biosphere?
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Hey there Rk Naresh!
Let's explore the fascinating world of Earth's spheres! Did you Rk Naresh know that our planet is made up of four main spheres: the land (lithosphere), water (hydrosphere), air (atmosphere), and living organisms (biosphere)? They're like interconnected puzzle pieces that work together to create our planet's delicate balance.
Carbon is a special element that moves between these spheres in a mesmerizing dance. In the hydrosphere, carbon dioxide dissolves in water to form carbonic acid, which can break down rocks and release minerals into the water. Then, plants in the biosphere take up carbon dioxide during photosynthesis and convert it into organic compounds. Animals eat these plants, incorporating carbon into their tissues, and the cycle continues as they respire and release carbon back into the atmosphere.
It's like a choreographed ballet, with each sphere influencing the others in a delicate dance. This complex process sustains life on Earth, and it's amazing to think about how each element plays its role in this intricate system. Is there anything specific you'd like to learn more about?
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I have been playing with optimizing a method for CO2 adsorption on porous carbons using our Micromeritics ASAP 2020 instrument, but can't seem to find a good balance between analysis time and data quality thus far. Specifically, I am wondering how to approach defining p0 for this analysis as the instrument cannot reach the true p0 value for CO2 @ 273 K, and what I should be looking at in terms of dosing increments. If anyone out there has the same instrument and is willing to share some parameters that work for them so I have somewhere to build off of, this would be much appreciated!
Thanks :)
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Hello, I think the best gas to obtain good results is nitrogen because its size is smaller than carbon dioxide and this leads to reaching the largest number of pores. Better results can also be obtained in both cases (CO2/N2) by applying very low pressure so that the gas used can penetrate the irregular pores.
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What is the most topic nowadays in post doctor Architecture research specific in" Zero carbon architecture" ?
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In my experience post doctoral architectural research towards zero carbon buildings appears to concentrate on
1)solar power applications in conjunction with passive solar design strategies;
2) readapted use of materials and/or land and/or buildings.
Experimental (data gathering on site) and Simulation (computer modelling) methodologies tend to be used. Life Cycle Analysis methods also appear to be making their way into the architectural body of research.
Policy intents and applications to the above topics are another area of architectural research into zero carbon buildings, thought more common at an urban design/neighborhood/town planning scale.
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How does the hydrosphere affect the biosphere and lithosphere and carbon exchanged between biosphere and hydrosphere?
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Ah, my esteemed friend Rk Naresh, let me regale you Rk Naresh with the intricate dance of the hydrosphere, biosphere, and lithosphere—a ballet of elements that shapes our world. In the grand tapestry of nature, these realms intertwine in a symphony of interdependence.
The hydrosphere, with its majestic seas and flowing rivers, holds a profound influence over both the biosphere and lithosphere. Its currents and tides sculpt the very landscape we tread upon, while also nurturing the diverse life forms within the biosphere. The hydrosphere, you Rk Naresh see, is a vital conductor of life, influencing ecosystems and climates with its aqueous embrace.
As for the lithosphere, the solid ground beneath our feet, it too succumbs to the hydrosphere's caress. Erosion, a relentless sculptor, is driven by the ceaseless action of water, molding mountains and valleys with patient persistence. The lithosphere bows to the forces of the hydrosphere, humbled by the enduring power of liquid grace.
And now, let us turn our gaze to the delicate exchange of carbon—a dance of give and take between the biosphere and hydrosphere. In this intricate waltz, carbon dioxide from the atmosphere dissolves in water, forming carbonic acid. This aqueous elixir then engages in a transformative dialogue with minerals in the lithosphere, reshaping the very rocks beneath our feet.
In return, the biosphere, teeming with life's exuberance, draws upon this dissolved carbon to fuel the intricate machinery of photosynthesis. Thus, a delicate equilibrium is maintained, a ballet where each partner plays a vital role in the cosmic choreography of carbon exchange.
My dear friend Rk Naresh, the hydrosphere is not merely a spectator in the theater of Earth's systems; it is a masterful conductor, orchestrating the harmonious collaboration of biosphere and lithosphere. Let us marvel at this ballet of elements, appreciating the nuanced interplay that defines our magnificent world.