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In the long-term carbon cycle, carbon is stored in geological reservoirs such as sedimentary rocks, fossil fuels, and the ocean. Over millions of years, processes like weathering, volcanic activity, and tectonic movements facilitate the release and sequestration of carbon. Carbon dioxide from the atmosphere is absorbed by oceans and photosynthetic organisms, while geological processes can return it to the atmosphere through volcanic eruptions. This cycle plays a crucial role in regulating Earth's climate and maintaining the balance of carbon in the environment.
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What happens to carbon in the short term carbon cycle?
In the short-term cycle, plants convert carbon dioxide into carbohydrates. Organisms eat the plants and obtain carbon, and then release it back into the air as carbon dioxide. Carbon is also released through wastes and decay of their remains.
What in the global carbon cycle is not a long term sink?
In the global carbon cycle, the atmosphere and surface ocean are not considered long-term sinks for carbon. While they do temporarily store carbon dioxide, they are in constant exchange with the biosphere and lithosphere, making their carbon content subject to rapid fluctuations. Unlike long-term sinks such as fossil fuels and sedimentary rocks, which sequester carbon for millions of years, these components are more dynamic and can release carbon back into the atmosphere relatively quickly.
Where is the carbon cycle naturally slowest?
The carbon cycle is naturally slowest in deep ocean waters, where carbon can remain sequestered for hundreds to thousands of years before resurfacing. In these regions, carbon can be stored in deep-sea sediments, forming long-term repositories of carbon that contribute to the slow turnover of carbon in the cycle.
Is the atmosphere a carbon store?
Yes, the atmosphere acts as a carbon store by holding carbon dioxide and other greenhouse gases. However, excessive amounts of carbon emissions can lead to an imbalance in the carbon cycle and contribute to climate change.
How and in what form does carbon center an leave the cycle?
Carbon enters the carbon cycle primarily through photosynthesis, where plants absorb carbon dioxide (CO2) from the atmosphere and convert it into organic matter. It is then transferred through various processes, including respiration, decomposition, and combustion. Carbon exits the cycle when it is released back into the atmosphere as CO2 through respiration, decay, or human activities like burning fossil fuels. Additionally, carbon can be stored long-term in geological formations or ocean sediments, effectively removing it from the active cycle.
What is the carbon sequenstriation?
well.......the carbon cylcle goes through two processes. one is i short term cycle. the other is a long term cycle
What happens to carbon in the short term carbon cycle?
In the short-term cycle, plants convert carbon dioxide into carbohydrates. Organisms eat the plants and obtain carbon, and then release it back into the air as carbon dioxide. Carbon is also released through wastes and decay of their remains.
What in the global carbon cycle is not a long term sink?
In the global carbon cycle, the atmosphere and surface ocean are not considered long-term sinks for carbon. While they do temporarily store carbon dioxide, they are in constant exchange with the biosphere and lithosphere, making their carbon content subject to rapid fluctuations. Unlike long-term sinks such as fossil fuels and sedimentary rocks, which sequester carbon for millions of years, these components are more dynamic and can release carbon back into the atmosphere relatively quickly.
What is the difference between the short term and long term carbon cycle?
The short-term carbon cycle involves the rapid exchange of carbon among the atmosphere, oceans, and living organisms, primarily through processes like photosynthesis, respiration, and decomposition. This cycle typically operates on timescales of days to years. In contrast, the long-term carbon cycle involves the geological processes that sequester carbon over millions of years, including the formation of fossil fuels, sedimentation, and the weathering of rocks. This cycle regulates Earth's climate over much longer periods and plays a crucial role in carbon storage in geological formations.
Where is the carbon cycle naturally slowest?
The carbon cycle is naturally slowest in deep ocean waters, where carbon can remain sequestered for hundreds to thousands of years before resurfacing. In these regions, carbon can be stored in deep-sea sediments, forming long-term repositories of carbon that contribute to the slow turnover of carbon in the cycle.
The formation of fossil fuels in the carbon cycle serves to?
The formation of fossil fuels in the carbon cycle stores carbon that was once in the atmosphere. This process helps regulate the Earth's climate by removing carbon dioxide from the atmosphere and storing it long-term underground. Burning fossil fuels releases this stored carbon, contributing to the greenhouse effect and climate change.
What is a carbon store?
A carbon store is a natural or artificial reservoir that contains carbon, either in the form of organic matter or carbon dioxide. Examples include forests, soils, oceans, and fossil fuel deposits. These stores play a crucial role in the global carbon cycle and can help regulate the Earth's climate by absorbing and storing carbon dioxide from the atmosphere.
Is the atmosphere a carbon store?
Yes, the atmosphere acts as a carbon store by holding carbon dioxide and other greenhouse gases. However, excessive amounts of carbon emissions can lead to an imbalance in the carbon cycle and contribute to climate change.
Which one doesn't have a shortterm biogeochemical cycle carbon nitrogen oxygen phosphorus?
Carbon has both short-term and long-term biogeochemical cycles, while nitrogen, oxygen, and phosphorus have primarily long-term biogeochemical cycles. These elements are cycled through various reservoirs in the environment, but the rates at which they move through these cycles differ.
How and in what form does carbon center an leave the cycle?
Carbon enters the carbon cycle primarily through photosynthesis, where plants absorb carbon dioxide (CO2) from the atmosphere and convert it into organic matter. It is then transferred through various processes, including respiration, decomposition, and combustion. Carbon exits the cycle when it is released back into the atmosphere as CO2 through respiration, decay, or human activities like burning fossil fuels. Additionally, carbon can be stored long-term in geological formations or ocean sediments, effectively removing it from the active cycle.
What is carbon storing?
either a long-term or a short term store, it's a place where carbon is accumalated and stored. Examples of long term stores is the atmosphere and short-term could be living organisms.
What best describes matter in the continual cycle of growth reproduction death and decay of organisms?
One term for the process is the carbon cycle, or at least the biologic part of that cycle.
