S0.5% CA used as injection carbon for mills

S0.5% CA used as injection carbon for mills

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Loading Port:: Shanghai

Payment Terms:: TT OR LC

Min Order Qty:: 21.7

Supply Capability:: 1017 m.t./month

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Item specifice

VM:

2%max

Introduction:

Calcined anthracite can be called carbon additive, carbon raiser, recarburizer, injection coke, charging coke, gas calcined anthracite.It is playing more and more important role in the industry

Best quality Anthracite as raw materials through high temperature calcined at over 2000℃ by the DC electric calciner with results in eliminating the moisture and volatile matter from Anthracite efficiently, improving the density and the electric conductivity and strengthening the mechanical strength and anti-oxidation. It has good characteristics with low ash, low resistivity, low sulphur,. It is the best material for high quality carbon products. It is used as carbon additive in steel industry or fuel.

Features:

G-High Calcined Anthracite is produced when Anthracite is calcined under the temperature of 1240°C in vertical shaft furnaces. G-High Calcined Anthracite is mainly used in electric steel ovens, water filtering, rust removal in shipbuilding and production of carbon material.

Specifications:

PARAMETER UNIT GUARANTEE VALUE
F.C.%	95MIN	94MIN	93MIN	92MIN	90MIN	85MIN	84MIN
ASH %	4MAX	5MAX	6 MAX	6.5MAX	8.5MAX	12MAX	13MAX
V.M.%	1 MAX	1MAX	1.0MAX	1.5MAX	1.5MAX	3 MAX	3 MAX
SULFUR %	0.3MAX	0.3MAX	0.3MAX	0.35MAX	0.35MAX	0.5MAX	0.5MAX
MOISTURE %	0.5MAX	0.5MAX	0.5MAX	0.5MAX	0.5MAX	1MAX	1MAX

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S0.5% CA used as injection carbon for mills

FAQ:

Packing:

(1). Waterproof jumbo bags: 800kgs~1100kgs/ bag according to different grain sizes;

(2). Waterproof PP woven bags / Paper bags: 5kg / 7.5kg / 12.5kg / 20kg / 25kg / 30kg / 50kg small bags;

(3). Small bags into jumbo bags: waterproof PP woven bags / paper bags in 800kg ~1100kg jumbo bags.

Payment terms
20% down payment and 80% against copy of B/L.

Workable LC at sight, or as we discuss

Q:What are carbon credits?: The aim of carbon credits is to lessen greenhouse gas emissions and combat climate change by using a market-based mechanism. These credits measure and quantify the reduction, removal, or avoidance of one metric ton of carbon dioxide (or its equivalent) from being released into the atmosphere. The concept behind carbon credits is rooted in the belief that certain activities or projects can offset the emissions caused by other activities. For example, renewable energy projects like wind farms or solar power plants can generate carbon credits by replacing the need for fossil fuel-based electricity generation. Similarly, projects focused on reforestation or afforestation can absorb carbon dioxide from the atmosphere and generate credits. These carbon credits can be purchased and sold in the carbon market, enabling companies or individuals to compensate for their own emissions by buying credits from projects that have successfully reduced or removed carbon dioxide from the atmosphere. This supports environmentally friendly initiatives and contributes to the overall reduction of greenhouse gases. The carbon credit system functions by creating financial incentives for activities that reduce emissions. It encourages businesses to invest in cleaner technologies and practices by assigning a monetary value to the reduction of carbon emissions. This drives the transition to a low-carbon economy and promotes sustainable development. Carbon credits play a crucial role in international efforts to tackle climate change. They are often used as a compliance mechanism for countries or companies to meet their emission reduction targets, as outlined in international agreements like the Kyoto Protocol or the Paris Agreement. Additionally, they contribute to the overall objective of limiting global temperature rise by encouraging emission reductions beyond regulatory requirements. While carbon credits have faced criticism for potentially allowing companies to continue polluting by simply purchasing credits, they remain an important tool in the fight against climate change. They provide economic benefits to sustainable projects and encourage the adoption of cleaner technologies, ultimately helping to mitigate the environmental impact of human activities.

Q:Yes, I have a weapon, want to strengthen 11, said to be advanced furnace rock carbon, do not know how to get, look at the prawns pointing: To strengthen the ordinary senior rock colorless, furnace carbon is used advanced, the mall did not buy, according to that wish gift box can be opened in some special activities in the last device can be bought in, no other time

Q:How does carbon impact the fertility of soil?: Carbon plays a crucial role in the fertility of soil as it is the foundation of organic matter, which is vital for soil health and productivity. When carbon-rich organic matter, such as decaying plant and animal residues, is added to the soil, it helps improve its structure, nutrient-holding capacity, and water retention. This, in turn, enhances the soil's ability to support plant growth and sustain microbial activity. Organic matter serves as a source of carbon for soil microorganisms, fungi, and bacteria, which decompose it and release nutrients for plants. This decomposition process, known as mineralization, releases essential macronutrients (nitrogen, phosphorus, and potassium) and micronutrients into the soil, making them available for plant uptake. Additionally, carbon in organic matter helps bind soil particles together, improving soil structure and preventing erosion. Moreover, carbon improves the soil's water-holding capacity, reducing the risk of drought stress for plants. It acts as a sponge, absorbing and retaining moisture, which helps to sustain plant growth during dry periods. Carbon also promotes the development of a healthy and diverse soil microbial community, including beneficial bacteria and fungi. These microorganisms enhance nutrient cycling, disease suppression, and plant nutrient uptake, further contributing to soil fertility. However, excessive carbon inputs, such as from excessive organic matter addition or improper land management practices, can have negative effects on soil fertility. An imbalance in carbon availability can lead to nitrogen immobilization, where soil microorganisms consume nitrogen for their own growth, depriving plants of this essential nutrient. Additionally, high carbon content can create anaerobic conditions, reducing the availability of oxygen for plant roots and beneficial soil organisms. In summary, carbon is essential for maintaining soil fertility as it improves soil structure, nutrient availability, water retention, and microbial activity. However, it is crucial to maintain a balanced carbon-to-nitrogen ratio and adopt sustainable land management practices to ensure the optimal fertility of soil.

Q:What are the limitations of carbon dating?: Carbon dating, also known as radiocarbon dating, is widely used to determine the age of organic materials up to 50,000 years old. Despite its significant contributions to archaeology and paleontology, researchers must be aware of its limitations. One limitation is the inability of carbon dating to accurately date materials beyond the 50,000-year mark. This is because the isotope carbon-14, used in carbon dating, has a half-life of only 5,730 years. Consequently, after multiple half-lives, there is insufficient carbon-14 remaining in a sample to determine its age accurately. Another limitation is the reliance on organic material. Carbon dating can only be applied to organic materials like bones, shells, wood, and charcoal. It is not applicable to inorganic materials such as rocks or minerals. Additionally, the presence of contaminants like humic acids or carbonates can distort the carbon dating results. Furthermore, carbon dating is limited in that it provides only a relative age for the sample. It establishes the ratio of carbon-14 to carbon-12 in the sample and compares it to the known ratio in the atmosphere. By assuming that this ratio has remained constant over time, an estimate of the sample's age can be made. However, variations in atmospheric carbon-14 levels over time can affect the accuracy of this method. Moreover, carbon dating can be influenced by nuclear testing and other human activities that release significant amounts of carbon-14 into the atmosphere. This phenomenon, known as the "bomb effect," can lead to artificially younger dates for samples collected after the mid-20th century. Lastly, the size and condition of the sample can limit the accuracy of carbon dating. Sufficient organic material is required for analysis to obtain precise results. This poses challenges when dealing with small or degraded samples, as the carbon-14 content may be insufficient or contaminated. In conclusion, while carbon dating is a valuable tool for determining the age of organic materials, it has limitations. Researchers must consider these limitations and exercise caution when interpreting the results, taking into account factors such as the age range, sample type, presence of contaminants, atmospheric variations, and sample size.

Q:How is carbon dioxide formed?: Carbon dioxide is formed through various natural and human activities. It is naturally produced by the respiration of animals, the decay of organic matter, and volcanic eruptions. Additionally, human activities such as the burning of fossil fuels, deforestation, and industrial processes also contribute to the formation of carbon dioxide.

Q:What are the impacts of carbon emissions on the stability of permafrost?: Carbon emissions have a significant impact on the stability of permafrost. Permafrost refers to the layer of soil, sediment, and rock that remains frozen for at least two consecutive years. It covers vast areas in the Arctic, subarctic regions, and high-altitude mountain ranges. One of the main impacts of carbon emissions on permafrost stability is the acceleration of climate change. Carbon dioxide (CO2) and other greenhouse gases trap heat in the atmosphere, leading to global warming. As temperatures rise, permafrost starts to thaw, causing a range of negative consequences. Thawing permafrost releases large amounts of stored carbon into the atmosphere. This carbon was previously locked in the frozen organic matter, such as dead plants and animals, which accumulated over thousands of years. As permafrost thaws, microbes decompose this organic matter and release greenhouse gases like carbon dioxide and methane. These emissions create a positive feedback loop, further exacerbating climate change and leading to more permafrost thawing. The release of carbon from thawing permafrost contributes to the overall increase in atmospheric greenhouse gas concentrations. This, in turn, amplifies global warming and global climate change. The impacts are not limited to the Arctic; they affect the entire planet. Rising temperatures, sea-level rise, extreme weather events, and disruptions to ecosystems are some of the consequences of global climate change. Permafrost thaw also affects infrastructure and human settlements in the Arctic and subarctic regions. Buildings, roads, pipelines, and other infrastructure built on permafrost can be destabilized as the ground beneath them softens. This can lead to structural damage and economic losses. Additionally, communities that rely on permafrost for traditional activities such as hunting, fishing, and transportation face challenges as the landscape changes. The impacts of carbon emissions on permafrost stability are not only local but also global. The release of stored carbon from permafrost contributes to climate change, which has far-reaching consequences for ecosystems, economies, and societies worldwide. It is crucial to reduce carbon emissions and mitigate climate change to preserve permafrost and its vital role in the Earth's climate system.

Q:How does carbon affect the formation of earthquakes?: Carbon does not directly affect the formation of earthquakes. Earthquakes are primarily caused by the movement of tectonic plates, which are large sections of the Earth's crust that float on the semi-fluid layer below. These plates can collide, slide past each other, or move apart, causing stress to build up along the plate boundaries. When the stress becomes too great, it is released in the form of an earthquake. However, carbon can indirectly impact the occurrence of earthquakes through its role in the Earth's carbon cycle and its contribution to climate change. Carbon dioxide (CO2) is a greenhouse gas that is released into the atmosphere through various human activities, such as burning fossil fuels. This excess CO2 in the atmosphere leads to global warming and climate change. Climate change can have several effects on the Earth's crust, some of which may indirectly influence seismic activity. For example, the melting of glaciers and polar ice caps due to global warming can lead to changes in the distribution of mass on the Earth's surface. This redistribution of mass can cause the Earth's crust to adjust, leading to increased stress along fault lines and potentially triggering earthquakes. Additionally, changes in precipitation patterns and the hydrological cycle caused by climate change can affect groundwater levels and pore pressure within rocks. These changes in water content can alter the strength and stability of fault lines, potentially making them more prone to slipping and causing earthquakes. It is important to note that the direct impact of carbon on earthquake formation is minimal compared to the primary factors such as plate tectonics. However, the relationship between carbon emissions, climate change, and seismic activity is an area of ongoing research and scientific investigation.

Q:How does carbon affect the formation of avalanches?: The formation of avalanches is not directly affected by carbon. Rather, factors such as snowpack stability, slope angle, and weather conditions primarily contribute to their occurrence. Nevertheless, avalanche formation can be indirectly influenced by carbon emissions and climate change, which impact snowpack stability. Increased levels of carbon dioxide in the atmosphere contribute to global warming, consequently affecting the overall climate. This warming leads to changes in precipitation patterns, snowfall amounts, and snowpack characteristics. Higher temperatures can cause rain instead of snow, resulting in a less stable snowpack. Climate change, in addition to altered precipitation patterns, can cause the melting and refreezing of snow. This process creates weak layers within the snowpack. When combined with subsequent snowfall and wind, these weak layers can lead to unstable snowpacks that are prone to avalanches. Moreover, carbon emissions contribute to the overall warming of the planet, which in turn can lead to the retreat of glaciers. Glaciers act as natural barriers and stabilizers in mountainous regions, reducing the likelihood of avalanches. However, as glaciers shrink, they leave behind unstable slopes, thereby increasing the potential for avalanches. It is important to emphasize that while carbon emissions and climate change indirectly influence avalanche formation, they are not the primary or sole cause. Local weather conditions, slope angles, and snowpack stability assessments conducted by avalanche experts play a more immediate role in determining the likelihood of avalanches.

Q:How does carbon impact the prevalence of heatwaves?: Carbon impacts the prevalence of heatwaves by contributing to the greenhouse effect. When carbon dioxide and other greenhouse gases are released into the atmosphere, they trap heat from the sun, leading to a rise in global temperatures. This increase in temperature makes heatwaves more frequent, intense, and longer-lasting, posing significant risks to human health, ecosystems, and infrastructure.

Q:How do you remove the carbon stains on your clothes?: Cleaning instructions for clothing * collar / cuff: Soak clothes in warm water with detergent powder for 15-20 minutes before washing. * Yellow White Sox: soaking washing powder for 30 minutes, then normal washing. * milk stains: use washing powder to do stain pretreatment and normal washing. If the milk stains are stubborn, you may need to use a bleach that is harmless to the clothes. * ordinary oil: a strong detergent is used for pre treatment and normal washing; if desired, bleaching of stubborn stains can also be done with bleach. The clothing removal method of rubber and plastic sex pigment stains with rubber and plastic pigment stains, it is difficult to remove, only use a suitable way to remove. 1, adhesive removal of stains clothes with glue stains, can use acetone or banana on glue water stains, use a brush to repeated washing, until soft glue stains off from the fabric, and then rinse with water. Once, can be repeated scrubbing several times, and finally wash. Do not use this method to avoid fabric damage. 2, white latex stain removal of white latex is a kind of synthetic resin, polyvinyl acetate emulsion. It is characterized by the addition of nylon silk and so on, the vast majority of fiber quality materials have bonding role, it can firmly adhere to the clothing. It has another characteristic that can dissolve in a variety of solutions. We will use its own characteristics to find ways to remove. By 60 DEG C or 8:2 alcohol liquor (95%) and a mixture of water, white glue stains on the clothes soak, soak about half an hour later, you can wash with water scrubbing, until...

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