Injection Coke FC85% min with stable quality

Injection Coke FC85% min with stable quality

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Loading Port:: Tianjin

Payment Terms:: TT OR LC

Min Order Qty:: 20 m.t.

Supply Capability:: 3000 m.t./month

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Packaging & Delivery

25kgs/50kgs/1ton per bag or as buyer's request

Specifications

Calcined Anthracite
Fixed carbon: 90%-95%
S: 0.5% max
Size: 0-3. 3-5.3-15 or as request

It used the high 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 resistvity, low sulphur, high carbon and high density. It is the best material for high quality carbon products.

Advantage and competitive of caclined anthracite:

1. strong supply capability

2. fast transportation

3. lower and reasonable price for your reference

4.low sulphur, low ash

5.fixed carbon:95% -90%

6..sulphur:lower than 0.3%

General Specification of Calcined Anthracite:

FC	80%	83%	85%	88%	90%
ASH %	16	14	13	10	8.5
V.M. %	3	3	2	2	1.5
S %	0.5	0.5	0.5	0.5	0.35
MOISTURE %	2	2	1	1	0.5

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Injection Coke FC85% min with stable quality

Q:How does carbon affect the formation of blizzards?: Blizzards, characterized by strong winds, low temperatures, and heavy snowfall, are not directly affected by carbon. Blizzards typically occur when a low-pressure system moves into an area with enough moisture and cold air. Temperature, moisture, and wind patterns are the main factors that influence the formation of blizzards. Nevertheless, carbon emissions and their impact on the climate can indirectly affect the frequency and intensity of blizzards. Carbon dioxide (CO2) and other greenhouse gases trap heat in the atmosphere, causing global warming. This warming effect can change weather patterns, including the conditions required for blizzard formation. Carbon emissions can lead to warmer temperatures, altering precipitation patterns and increasing moisture in the atmosphere. This additional moisture, along with the necessary cold air, can contribute to heavier snowfall during blizzards. Furthermore, climate change can influence wind patterns, impacting the intensity and duration of blizzards. Changes in atmospheric circulation patterns can modify the tracks and strength of storms, potentially resulting in more or fewer blizzard events in specific regions. It is worth noting that the specific impact of carbon emissions on blizzard formation varies depending on regional and local factors. The intricate nature of weather systems and the interaction between different variables make it difficult to attribute any single weather event solely to carbon emissions. However, the overall influence of carbon emissions on the climate system increases the potential for more extreme weather events, including blizzards.

Q:How does carbon affect the melting of polar ice caps?: Carbon affects the melting of polar ice caps by contributing to global warming. As carbon dioxide levels increase in the atmosphere, it acts as a greenhouse gas, trapping heat and causing the Earth's temperature to rise. This leads to the melting of polar ice caps, as the increased temperatures accelerate the melting process, causing the ice to melt at a faster rate.

Q:Appearance, hardness, electrical conductivity, use of carbon 60: For gas storageThe unique molecular structure of C60, C60 can be used as more effective and new hydrogen absorbing material than metal and alloy. There are 30 carbon carbon double bonds, each molecule of C60 so that the C60 molecules in the double bond open can absorb hydrogen. Stable C60 hydride has known C60 C60H24, C60H36 and C60H48. in the control of temperature and pressure conditions, can be simply made by C60 C60 and hydrogen hydrides, it at room temperature is very stable, and in the 80 to 215 DEG C, C60 hydride will release hydrogen, leaving the pure C60, it can be 100% recovery, and was used to prepare C60 hydride. Compared with the hydrogen storage materials of metal or its alloys, C60 hydrogen storage has the advantages of low price, and lighter than C60, metals and alloys, therefore, the same quality of material, the hydrogen storage of C60 metal or its alloy than more.C60 not only can store hydrogen, can also be used to store oxygen. Compared with high-pressure cylinders of oxygen storage, high pressure cylinder pressure is 3.9 * 106Pa, belongs to the high pressure oxygen storage method, and storage of C60 oxygen pressure is only 2.3 * 105 Pa, which belongs to low pressure oxygen storage method. Using C60 under low pressure, large storage has many uses of oxygen in the medical departments, military departments and the business sector will be.

Q:How does carbon impact the prevalence of tropical storms?: The prevalence of tropical storms is greatly influenced by carbon, specifically carbon dioxide (CO2) emissions. Human activities like burning fossil fuels, deforestation, and industrial processes have led to an increase in atmospheric CO2 levels, resulting in global warming. This phenomenon of rising global temperatures has various implications for the formation and intensity of tropical storms. To begin with, warmer temperatures lead to higher levels of moisture in the atmosphere due to increased evaporation of seawater. Moisture is crucial for the development and sustenance of tropical storms as it provides the necessary fuel. With more moisture available, the potential for tropical storms to form and strengthen is enhanced. Moreover, rising global temperatures cause tropical oceans to expand, providing a larger area for tropical storms to form and intensify. This expansion allows for greater energy exchange between the ocean and the atmosphere, further enhancing the potential for storm development. Additionally, elevated levels of CO2 contribute to ocean acidification, which negatively affects marine ecosystems like coral reefs. Coral reefs act as natural barriers that protect coastal areas from storm surges and waves generated by tropical storms. However, the acidification of oceans weakens and destroys these reefs, leaving coastal regions more vulnerable to storm impacts. Lastly, carbon emissions causing climate change alter atmospheric and oceanic circulation patterns, which can affect the movement and tracks of tropical storms. Changes in wind patterns and ocean currents may cause storms to deviate from their usual paths, leading to increased uncertainty and potential impacts on regions not typically prone to these events. In summary, carbon emissions and the resulting global warming have significant effects on the prevalence of tropical storms. Increased moisture content, expanded warm ocean areas, weakened coastal defenses, and altered storm tracks are all consequences of rising carbon levels, ultimately contributing to more frequent and intense tropical storms.

Q:How do human activities contribute to carbon emissions?: Human activities contribute to carbon emissions in several ways. The burning of fossil fuels for electricity, transportation, and industry is one of the main sources of carbon dioxide emissions. When we burn coal, oil, or natural gas, carbon is released into the atmosphere. Additionally, deforestation and land-use changes also contribute to carbon emissions. Trees play a crucial role in absorbing carbon dioxide, so when forests are cleared for agriculture or urbanization, the stored carbon is released back into the atmosphere. Moreover, industrial processes such as cement production and chemical manufacturing also release carbon emissions. Finally, human activities like agriculture and livestock farming can produce methane, a potent greenhouse gas that contributes to global warming. Overall, our reliance on fossil fuels, deforestation, industrial processes, and certain agricultural practices all contribute to carbon emissions, exacerbating the problem of climate change.

Q:How does deforestation affect carbon levels?: Deforestation has a significant impact on carbon levels in the atmosphere. Trees play a crucial role in the carbon cycle by absorbing carbon dioxide (CO2) through photosynthesis and storing it in their trunks, branches, leaves, and roots. When forests are cleared or burned, this stored carbon is released back into the atmosphere as CO2, contributing to the greenhouse effect and climate change. Deforestation not only reduces the number of trees available to absorb CO2 but also disrupts the natural balance of the carbon cycle. Forests act as carbon sinks, meaning they absorb more CO2 than they release, helping to regulate the Earth's climate. When forests are cut down, the carbon stored in their biomass is rapidly released, exacerbating the problem of excess CO2 in the atmosphere. In addition to the immediate release of carbon, deforestation also impacts the long-term carbon storage capacity of the planet. Young trees and newly regrown forests have a lower carbon storage capacity compared to older, mature forests. Therefore, when forests are cleared and replaced with young vegetation or non-forest land uses, the ability to absorb and store carbon is greatly reduced. The consequences of increased carbon levels in the atmosphere are far-reaching. Carbon dioxide is a greenhouse gas that traps heat in the Earth's atmosphere, contributing to global warming and climate change. Rising temperatures have a cascade of effects, including increased frequency and intensity of extreme weather events, rising sea levels, and disruptions to ecosystems and biodiversity. To mitigate the impact of deforestation on carbon levels, it is crucial to prioritize sustainable forest management practices and reforestation efforts. Protecting existing forests and promoting afforestation and reforestation can help restore the carbon-absorbing capacity of the planet and contribute to global efforts in combating climate change.

Q:How do plants and trees absorb carbon dioxide?: Through photosynthesis, plants and trees engage in a process known as carbon dioxide absorption. This process entails the conversion of sunlight, water, and carbon dioxide into glucose and oxygen. Within the plant cells, this transformation occurs in specialized structures called chloroplasts. During photosynthesis, plants absorb carbon dioxide from the atmosphere via small openings on their leaves called stomata. The carbon dioxide then infiltrates the plant's cells and travels to the chloroplasts. Within these chloroplasts, the energy from sunlight is utilized to convert the carbon dioxide and water into glucose and oxygen. The glucose generated through photosynthesis serves as a vital energy source for the plant's growth, reproduction, and other metabolic activities. Some of this glucose is stored as starch within the plant, while the remainder is used to produce other crucial compounds. The oxygen produced during photosynthesis is subsequently released back into the atmosphere through the stomata. This oxygen is indispensable for the survival of various animals, including humans, as it is necessary for respiration. In essence, the absorption of carbon dioxide through photosynthesis is an essential function performed by plants and trees. They function as natural carbon sinks, playing a vital role in regulating the levels of this greenhouse gas and mitigating the impacts of climate change.

Q:How does carbon affect the formation of haze?: Haze formation is significantly influenced by carbon, as it has the ability to interact with other pollutants and atmospheric conditions. When carbon-containing compounds, such as emissions from fossil fuels or organic matter from wildfires, are released into the atmosphere, they undergo chemical reactions with gases like nitrogen oxides and volatile organic compounds. These reactions lead to the creation of tiny particles called secondary organic aerosols (SOAs), which are suspended in the air. The presence of these SOAs can contribute to the formation of haze by scattering and absorbing sunlight, resulting in reduced visibility and a hazy appearance. Additionally, the carbon particles act as nuclei for condensation, attracting other pollutants and water vapor, ultimately leading to the formation of larger particles and, consequently, haze. Moreover, the interaction between carbon and atmospheric moisture can result in the formation of secondary organic aerosol particles, further contributing to haze formation. Furthermore, carbon particles also play a role in the formation of photochemical smog, a specific type of haze characterized by high levels of ozone. Carbon-containing pollutants can react with sunlight and other pollutants, leading to the production of ozone. The presence of ozone, combined with other pollutants, contributes to the formation of haze and decreases air quality. To summarize, the impact of carbon on haze formation is significant, as it contributes to the creation of secondary organic aerosols, acts as condensation nuclei, and promotes the production of ozone. Understanding the role of carbon in haze formation is crucial for implementing effective measures to control air pollution and mitigate the adverse effects of haze on human health and the environment.

Q:Something that seems to be used in the locomotive brake system. I haven't seen it, either. Who knows? It's better for the locomotive system to go back. Thank you！！: The texture of the skateboard is relatively soft, so the main loss in contact with the contact wire is on the slide plate, and the wear of the contact wire is very small.

Q:What are the effects of carbon emissions on the stability of ice shelves?: Carbon emissions have significant effects on the stability of ice shelves. As carbon dioxide (CO2) and other greenhouse gases are released into the atmosphere, they trap heat and contribute to global warming. This increased global temperature leads to the melting of ice shelves and glaciers. One of the primary effects of carbon emissions on ice shelves is the acceleration of their melting rates. Higher atmospheric temperatures cause more ice to melt, which in turn increases the amount of water flowing into the ocean. This added influx of freshwater can disrupt the delicate balance between the ice shelf and the ocean, potentially leading to ice shelf collapse. Additionally, carbon emissions contribute to the thinning of ice shelves. As the atmosphere warms, the air temperature above the ice shelves rises, leading to increased surface melting. This meltwater then flows into crevasses and cracks, causing further fracturing and weakening of the ice shelves. Over time, this thinning can make the ice shelves more susceptible to breaking apart. The melting of ice shelves due to carbon emissions also has indirect effects on the stability of surrounding ice sheets. Ice shelves act as a buttress, providing resistance to the flow of ice from the glaciers into the ocean. When ice shelves collapse or thin, this resistance is diminished, allowing glaciers to flow more freely into the ocean. This process leads to increased sea level rise, which has significant implications for coastal regions around the world. Furthermore, the loss of ice shelves can disrupt the ecosystem and biodiversity of the surrounding areas. Ice shelves provide a platform for various species, including seals and penguins, to breed and feed. When ice shelves disintegrate, these habitats are destroyed, impacting the entire food chain and ecosystem dynamics. Overall, carbon emissions from human activities have profound effects on the stability of ice shelves. The melting, thinning, and collapse of ice shelves contribute to rising sea levels, disrupt ecosystems, and have far-reaching consequences for coastal communities. It is crucial to mitigate carbon emissions and take proactive measures to protect these vulnerable ice shelves and the delicate balance they maintain in our global climate system.

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