Carbon is a naturally occurring element on Earth and is an integral part of all human, animal, and plant life. It is also one of the most frequently used occurring elements in biology. This is the starting point of many elements and builds a long relationship. This element has great strength and bonds last a long time. Because of this, carbon is an important and often-used source of fuel for living things.
What is the Carbon Cycle?
Carbon is one of the most easily found elements in the Earth’s crust. Natural and synthetic, that cause carbon to be exchanged from one sphere to another. The compounds that form during that exchange are called the carbon cycle. Carbon can be found in many different forms. The lithosphere, or rock and earth aspect of the Earth, holds a large amount of carbon. Carbon also exists in the atmosphere as carbon dioxide, an organic compound composed of both carbon and oxygen, and the hydrosphere also contains carbon in carbon dioxide form,
The carbon on Earth, and in the earthly spheres, is constantly in motion. Sometimes the carbon moves quickly within the Earth’s systems, and other times it can be retained in one place for many years. This is called the Fast cycle and the slow cycle due to the change and retention of compounds between the carbon. The carbon exchange between living things and the exchange of carbon between living things and the atmosphere is a fast cycle. The fast cycle encompasses those aspects of the carbon exchange which happen more quickly. Lifespan is used to measure the fast cycle. The exchange of carbon between the Earth’s surface and the atmosphere for millions of years is a slow cycle.
What is the Photosynthesis?
Photosynthesis is the absorption of carbon from the atmosphere by plants in the form of carbon dioxide(CO2). Plantlife uses carbon dioxide, along with sunlight and water, and transforms them into sugars, in a process called photosynthesis. In this process, the leaves of the plant get the carbon needed for photosynthesis from the air. This then interacts with sunlight and water to provide the energy a plant needs to grow and the product produces sugar and oxygen. Plants are an important factor in human life because this process cannot exist without carbon.
The contribution of organisms to the carbon cycle.
Carbon is transferred to animals by ingesting the dietary components of the plant. The transfer of its stored energy reserves and carbon atoms to animals is the second part of the fast cycle. Also, carbon is spread by small predators being eaten by high predators in the food chain. The carbon remains within the food chain until it is released through decomposition following the death of a plant or animal, or through respiration.
Oxygen produced by plants binds to carbon by inhalation by animals, including humans. O2 binds to the carbon to produce the oxygen needed for this respiratory process. We normally produce CO2 as a by-product of getting enough oxygen to the blood and body during the breathing process. That releases carbon dioxide into the atmosphere. And then, carbon moves easily from the atmosphere to a plant, from plants to animals, and then back to the air. Therefore, carbon is constantly moving in the carbon cycle and produces a large amount per year.
A dead body releases CO2 through decomposition. Once it is deceased, the bacteria activate on the dead body and break the bonds between the carbon compounds. That process releases CO2 back into the atmosphere. And then, carbon moves easily from the atmosphere to a plant, from plants to animals, and then back to the air.
Acid rain formation.
The transfer of carbon from the atmosphere to the Earth’s surface occurs naturally. One of these ways is through rainwater. CO2 accumulates in the air and saturates rainwater to form a mild type of acid rain. This rainwater is deposited between the rocks and evaporates over time. This evaporation releases inorganic carbon into the atmosphere. Carbon compounds are also produced when these acids flow into the ocean. The bicarbonate ions produced by the dissolution of acid binds with calcium to form shells and calcium bicarbonate. Also, shells are produced when oysters die.
Carbon is also added to the atmosphere during combustion. Also, decomposition also acts as part of the carbon cycle. Fossil fuels are formed as a result of the long-term deposition of carbon on this decomposing material, a compound that is produced. The resulting fossil fuels are stored for a long time. These long-deposited fossil fuels are released into the atmosphere by an earthquake or excavation. In this way, it contributes to the carbon cycle by releasing it from the atmosphere to the earth and back into the atmosphere. In this way, the carbon goes through a much slower cycle.