Carbon cycle or carbon circle or organic cycle or organic base of the Earth's biosphere(biosphere), petospiyar (pedosphere), geosphere (geosphere), hydrosphere (hydrosphere) and the atmosphere (atmosphere) measures transactions conducted carbon Postal uyirpuvi chemistry is cyclical. This is one of the most important cycles of the Earth. The fluid permits carbon to recycle all parts of the body and recycle its organisms. The carbon cycle was initially identified by Joseph Priestley and Antoine LavoisierDavy Hump they (Humphry Davy) became popular. [1] It is now commonly considered as five main stagnations of carbon interconnected by transmitters. These stocks are:
- Atmosphere
- Earth biosphere is usually defined as the pure organic water bodies and soil organic matter such as soil carbon.
- Includes dissolved inorganic carbon in the oceans and living and lifeless marine life,
- Fossil fuels include fossils.
- The inner surface of the Earth, carbon from the Earth's turbulence and the volcano and the water source through the volcanoes and geothermal systems from the overlap.
Carbon transactions between carbon's annual movements and stagnations are also caused by various chemical, physical, geological and biological functions. The ocean has a large running carbon tank near the surface of the Earth, but does not perform rapid transit with the deep oceanic atmosphere as part of the group.
The global carbon budget is a balance between transactions between carbon cycles (which are available and lost) between a particular cycle (eg, atmosphere ↔ biosphere) or carbon stagnation in the carbon cycle. An examination of the pump or stagnant carbon content provides information about carbon-dioxide or the flow of stagnant or carbon dioxide.
The carbon cycle is a theory that describes how the most energy of the solar system is available. How so much energy is available for millions of years available for millions of years? American scientist H. A. Beta explained this. There was not enough data to go ahead with the theory of nuclear reactions at high temperatures. Peet explained that the energy of the solar power is obtained through the organic cycle. Four-hydrogen atoms combined with the formation of a leukocytes and the catalyst for the function as a catalyst.
Contents
[ Hide ]Organic cycle [ edit ]
In the organic cycle, a proton (the embryonic embryo) first reacts with a carbon and emits energy. Reaction,
12 C 6 + 1 H 1 - -> 13 N 7 + energy,
This nitrogen is radiant. It evolves into a balsitan in 10.1 minutes and transmits it underneath.
13 N 7 ↔ 13 C 6 + 0 + e +1
Continuous charcoal 13, combined with another proton, emits high energy and acts as shown below.
13 C 6 + 1 H 1 ↔ 14 N 7 + energy.
This is followed by a consistent nitrogen nucleus with another proton (3)
14 N 7 + 1 H 1 ↔ 15 O 8+ energy.
This o becomes an ending positron and will become N again. In conjunction with the N15 Proton,
15 N 7 + 1 H 1 ↔ 12 C 6 + 4 He 2 . On the whole the charcoal did not change. 4 hydrogen nuclei combined with an aluminum nipple and two positrons
And the energy. The explanation illustrates how the potter gives so much energy, the above is the organic system.
The atmosphere [ edit ]
Carbon is the primary carbon dioxide (CO 2 ) gas in the Earth's atmosphere . Although it is a low percentage of the atmosphere ( approximately 0.04% on molar ), it plays a vital role as a partner of life. Methane and chlorofluorocarbon (in which chlorofluorocarbons are fully human growth in time). Are other gases with carbon in the atmosphere. Tree photosynthesis, while addressing carbon dioxide into carbohydrates convert active oxygenPublishes. The process is very prolific in the new forests where the growth of trees is rapid. This process takes place in autumn forests when the leaves come out in spring. It is a key signal of the Keeling curve of the measured CO 2 concentration . The northern hemisphere is superlative in the northern hemisphere, much higher in the latitudes of the latitudes than in the south.
- Forests store over 86% of carbon over the planet's surface and 73% of planetary soil. [2]
- The ocean water on the surface of the oceans on the poles is very cool and contains more carbonic acid and becomes more soluble CO 2 . It works in the thermohaline circulation that carries the dense surface water in the interior of the ocean (see record of soluble load ).
- Organisms above the oceans of high biomass produces less carbon tissues or carbonate hard trim bodies such as tiles and texts. The low rates of currents result in carbon divergence as they are converted into oscillating ( soft tissue ) and reproducible ( carbonate load ) rather than they have produced in the oceans ( see record of biological load ).
- Of silicate rock weathering (see carbonate-silicate cycle ). Carbonate acids work with the environmental degradation rock to produce bicarbonate ions. Manufactured bicarbonateions are transported to the ocean used for marine carbonates. Unlike the dissolved balance or tissue dissolved CO 2 , the atmosphere does not move the carbon into the stagnant, which returns it to the atmosphere.
- The atmospheric carbon dioxide, which was about 320 ppm (ppm) in the moon in 1958, is about 385ppm [3] in 2010 .
- Gaya Identity ( kaya identity ) through the future CO 2 emission computed.
Carbon exits the atmosphere in various ways:
- It is performed through the breathing of planets and spirits . This is a heat emission reaction . It also involves the carbohydrate (or other organic molecules) inside carbon-dioxide and water within the water.
- Animal and plants are performed through the rotting . The carbon compounds of dead animals and plants such as fungus and bacteria degrade and replace carbon dioxide with oxygen, or without methane .
- Carbon dioxide production is produced through the combustion of organic products containing oxidized carbon (and other substances such as steam). The carbon emissions of burning fuel, such as charcoal , petroleum products and natural gas , are released to Earth in thousands of years. Burning acrobures (agrofuel) release carbon dioxide. It is stored for a few years or less.
- Cement production. Component of cement lime (calcium oxide) to form calcite (calcium carbonate) carbon dioxide is released when heated.
- The carbon-dioxide is dissolved in the ocean's surface, and the surface is returned to the atmosphere.
- Volcano eruptions and surface transformation emit gases into the atmosphere. Volcanoes primarily consist of steam , carbon dioxide and sulfur dioxide . Carbon dioxide outlet is roughly balanced to be removed by silicate atmosphere [citation needed]; So the value of these two functions that have alternating chemical changes is estimated to be zero. And does not affect the atmospheric carbon dioxide levels over a period of less than 100,000 years.
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