Three carbon enters the atmosphere primarily through processes such as respiration, combustion, and decomposition. During respiration, animals and plants release carbon dioxide (CO2) as they convert glucose into energy. Combustion of fossil fuels and biomass, such as wood and coal, also releases CO2 into the atmosphere. Additionally, decomposition of organic matter by microorganisms emits carbon dioxide as they break down dead plants and animals.
Carbon enters the atmosphere primarily through the combustion of fossil fuels, such as coal, oil, and natural gas, which releases carbon dioxide (CO2) as a byproduct. Additionally, deforestation contributes to carbon emissions, as trees that absorb CO2 are removed, leading to increased atmospheric carbon levels. Lastly, natural processes like volcanic eruptions and respiration from living organisms also release carbon into the atmosphere.
The atmosphere on Mars consists of 95% carbon dioxide, 3% nitrogen, 1.6% argon, and contains traces of oxygen and water.[
The total mass of CO2 is about 3 trillion tonnes (3 teratonnes). (That's a 3 with 12 zeros, 3,000,000,000,000 tonnes.) C12 + 2O16 means 12 parts in 32, by weight, are carbon. 3/8ths. So, 1-1/8 teratonnes. That is about 2.5 quadrillion pounds, or 1.125 quadrillion kg.
Mercury has virtually no atmosphere. Planet with thinnest Venus has a extremely dense atmosphere of mostly sulphur compared to Earth. Planet with densest. Earth has a moderately dense atmosphere of nearly 3 quarters nitrogen and oxygen. Planet with 2nd from densest. Mars has a thin atmosphere of mostly carbon and some oxygen. Planet with 2nd thinnest.
1. Liquid water. 2. Temperatures that aren't too extreme. 3. An atmosphere with oxygen, carbon dioxide and other useful gases.
The carbon cycle is a process where carbon is removed and returned to the atmosphere. The ways of returning carbon to the atmosphere are- 1. Respiration 2. Decomposition 3. Combustion Ways of removing carbon- Photosynthesis. The CO2 in the air is taken in by green plants for photosynthesis. The green plants die eventually and is decomposed; decomposition return carbon to the atmosphere. Animals respire and return carbon dioxide to the atmosphere. Decomposers respire as well. Green plants can be used to make fuels, which combust to return carbon dioxide to the air.
Decomposition of dead organisms releases carbon back into the atmosphere and soil. Burning of fossil fuels releases stored carbon back into the atmosphere as carbon dioxide. Weathering of rocks can release carbon into the soil and ocean, where it can be stored for extended periods.
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Mars Atmosphere is made of 95% Carbon Dioxide (co2) and 3% nitrogen (n2)
the Martian atmosphere is made up of 95% Carbon Dioxide, 3% nitrogen, 1.6% argon, and 0.4% oxygen.
No. The sun radiates heat in all directions on 3 axes. The spherical arc of that which reaches the Earth's Atmosphere is very small in comparison.
Carbon dioxide is added to the atmosphere primarily through the burning of fossil fuels, such as coal, oil, and natural gas, for energy and transportation. Deforestation also contributes significantly, as trees that absorb CO2 are removed, releasing stored carbon. Additionally, industrial processes, including cement production and various manufacturing operations, release CO2 as a byproduct.
1) carbon dioxide 2) nitrogen 3) oxygen
The atmosphere on Mars consists of 95% carbon dioxide, 3% nitrogen, 1.6% argon, and contains traces of oxygen and water.[
Nature produces the vast bulk of carbon dioxide in the atmosphere. Rotting trees, and dead matter produce over 90% of the current levels of carbon dioxide. Man produces between 3 and 6 percent of all CO2 annually.
Most of carbon in the atmosphere is in the form of CO2. At nearly 400 ppm, that pencils out to 3 trillion tonnes (metric tons). To single out how much of that is carbon we need to multiply by 12 (molecular weight of carbon) and divide by 32 (molecular weight of O2). That works out to 1.1 trillion tonnes. There is additional carbon in the atmosphere in the form of methane (CH4), carbon monoxide (CO), chlorofluorocarbons (CFC), and a few other carbon compounds. If you count pollen, wind born leaves, birds, and other things occasionally swept aloft, the atmosphere temporarily suspends much more carbon yet.
Some non-human activities that release carbon into the atmosphere as CO2 during the carbon cycle include volcanic eruptions, wildfires, and the decomposition of organic matter in soils. These processes release carbon that has been stored in rocks, vegetation, or soil back into the atmosphere.