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The carbon cycle is the process by which carbon is exchanged between the atmosphere, oceans, biosphere, and geosphere. It includes processes such as photosynthesis, respiration, and decomposition. Carbon moves through these different reservoirs in a balanced and interconnected way, influencing Earth's climate and supporting life.
Phosphorus generally does not exist as gas
Huge deposits of carbon were stored over millions of years through processes like sedimentation and burial of organic matter, leading to the formation of coal, oil, and natural gas. These fossil fuels contain large amounts of carbon that were extracted from the atmosphere by plants and other organisms during their growth and then preserved underground.
A carbon sink is a natural or artificial reservoir that absorbs and stores atmospheric carbon dioxide, such as forests or oceans. Carbon sequestering refers to the process of capturing and storing carbon dioxide from the atmosphere, which can be achieved through activities like reforestation, soil carbon enhancement, or carbon capture and storage technologies. In essence, carbon sequestering is the action while a carbon sink is the result or location where carbon is stored.
The correct way to write the chemical name of carbon dioxide is "carbon dioxide" or "CO2".
Plants in the biosphere interact with the atmosphere through photosynthesis, where they take in carbon dioxide from the air and release oxygen.
The carbon cycle is the process by which carbon is exchanged between the atmosphere, oceans, biosphere, and geosphere. It includes processes such as photosynthesis, respiration, and decomposition. Carbon moves through these different reservoirs in a balanced and interconnected way, influencing Earth's climate and supporting life.
Energy in the biosphere flows through a one-way system, entering as sunlight and being converted into chemical energy through photosynthesis. This energy is then transferred through the food chain as organisms consume each other. In contrast, matter in the biosphere cycles through biogeochemical processes, such as the carbon and nitrogen cycles, where elements are taken up by organisms, recycled, and reused in the ecosystem.
One way oxygen moves between the biosphere and the atmosphere is through the process of photosynthesis. During this process, plants and other photosynthetic organisms take in carbon dioxide from the atmosphere and release oxygen as a byproduct, thus increasing the oxygen levels in the atmosphere.
Ecological
Phosphorus generally does not exist as gas
Humans affect the biosphere in numerous ways. One of the most common ways in which humans impact the biosphere is by their extraction of Natural Resources. Growth and expansion is another way in which humans affect the biosphere.
To most people it is true that in the biosphere there is a one way flow of energy. This is thought of in terms of the food chain.
Photosynthesis is considered the most important process in the biosphere because it is the primary way that energy enters the ecosystem. It converts sunlight into chemical energy stored in glucose, which is used by plants and other organisms for growth and survival. Additionally, photosynthesis releases oxygen into the atmosphere, which is essential for the respiration of most living organisms.
The energy stored in mineral oil is in the form of carbon that produces energy when it forms atomic bonds with oxygen to form carbon dioxide in the burning process. That energy was originally stored when plants used to Sun's energy to separate carbon and oxygen from atmospheric carbon dioxide millions of years ago, by photosynthesis. Plants used the carbon to form tissues made from long chains of carbon atoms. In that way, burning oil, coal and natural gas releases the Sun's energy, stored millions of years ago. 1 kg of fossil fuel burns with approximately 2.5 kg of oxygen to produce 3.5 kg of carbon dioxide.
Are complex sugars that are stored. Glycogen is the way that sugar is stored in animals, starch is the way that sugar is stored in plants.
Huge deposits of carbon were stored over millions of years through processes like sedimentation and burial of organic matter, leading to the formation of coal, oil, and natural gas. These fossil fuels contain large amounts of carbon that were extracted from the atmosphere by plants and other organisms during their growth and then preserved underground.