write a project on carbon cycle
Answers
Answer:
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Explanation:
Carbon Cycle Steps
Carbon present in the atmosphere is absorbed by plants for photosynthesis.These plants are then consumed by animals and carbon gets bioaccumulated into their bodies.These animals and plants eventually die, and upon decomposing, carbon is released back into the atmosphere.
Answer:
The carbon cycle is the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth. Carbon is the main component of biological compounds as well as a major component of many minerals such as limestone. Along with the nitrogen cycle and the water cycle, the carbon cycle comprises a sequence of events that are key to make Earth capable of sustaining life. It describes the movement of carbon as it is recycled and reused throughout the biosphere, as well as long-term processes of carbon sequestration to and release from carbon sinks. Carbon sinks in the land and the ocean each currently take up about one-quarter of anthropogenic carbon emissions each year.
Humans have disturbed the biological carbon cycle for many centuries by modifying land use, and moreover with the recent industrial-scale mining of fossil carbon (coal, petroleum and gas extraction, and cement manufacture) from the geosphere.[1][2] Carbon dioxide in the atmosphere had increased nearly 52% over pre-industrial levels in 2020, forcing greater atmospheric and Earth surface heating by the Sun.[3][4] The increased carbon dioxide has also increased the acidity of the ocean surface by about 30% due to dissolved carbon dioxide, carbonic acid and other compounds, and is fundamentally altering marine chemistry.[5][6] The majority of fossil carbon has been extracted over just the past half century, and rates continue to rise rapidly, contributing to human-caused climate change.[7][8] The largest consequences to the carbon cycle, and to the biosphere which critically enables human civilization, are still set to unfold due to the vast yet limited inertia of the Earth system.[1][9][10] Restoring balance to this natural system is an international priority, described in the both the Paris Climate Agreement and Sustainable Development Goal 13.
Contents
1 Main components
1.1 Atmosphere
1.2 Terrestrial biosphere
1.3 Ocean
1.4 Geosphere
2 Terrestrial carbon in the water cycle
3 The marine biological pump
4 Fast and slow cycles
5 Deep carbon cycle
5.1 Carbon in the lower mantle
5.2 Carbon in the core
6 Human influence
6.1 Land use changes
6.2 Fossil carbon extraction
6.3 Man-made chemicals
6.3.1 Plastics
6.3.2 Halocarbons
6.4 Climate change feedbacks
7 Gallery
8 See also
9 References
10 Further reading
11 External links
Main components
The carbon cycle was first described by Antoine Lavoisier and Joseph Priestley, and popularised by Humphry Davy.[11] The global carbon cycle is now usually divided into the following major reservoirs of carbon interconnected by pathways of exchange:[12]:5–6
The atmosphere
The terrestrial biosphere
The ocean, including dissolved inorganic carbon and living and non-living marine biota
The sediments, including fossil fuels, freshwater systems, and non-living organic material.
The Earth's interior (mantle and crust). These carbon stores interact with the other components through geological processes.
The carbon exchanges between reservoirs occur as the result of various chemical, physical, geological, and biological processes. The ocean contains the largest active pool of carbon near the surface of the Earth.[13] The natural flows of carbon between the atmosphere, ocean, terrestrial ecosystems, and sediments are fairly balanced so that carbon levels would be roughly stable without human influence.[3][14]
Atmosphere
Main article: Atmospheric carbon cycle
The ocean and land have continued to absorb about half of all carbon dioxide emissions into the atmosphere, even as anthropogenic emissions have risen dramatically in recent decades. It remains unclear if carbon absorption will continue at this rate.[15]
Carbon in the Earth's atmosphere exists in two main forms: carbon dioxide and methane. Both of these gases absorb and retain heat in the atmosphere and are partially responsible for the greenhouse effect.[13] Methane produces a larger greenhouse effect per volume as compared to carbon dioxide, but it exists in much lower concentrations and is more short-lived than carbon dioxide, making carbon dioxide the more important greenhouse gas of the two.[16]
Carbon dioxide is removed from the atmosphere primarily through photosynthesis and enters the terrestrial and oceanic biospheres. Carbon dioxide also dissolves directly from the atmosphere into bodies of water (ocean, lakes, etc.), as well as dissolving in precipitation as raindrops fall through the atmosphere. When dissolved in water, carbon dioxide reacts with water molecules and forms carbonic acid, which contributes to ocean acidity. It can then be absorbed by rocks through weathering. It also can acidify other surfaces it touches or be washed into the ocean.[17]