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Oceans are the major sources for water evaporation.
The abundance of plants and the fact that they take in so much Carbon Dioxide for photosynthesis makes plants a major reservoir for carbon. Sedimentary rock comprises the largest single reservoir in the carbon cycle. The world's oceans are the second-largest reservoir in the carbon cycle.
atmosphere
Gaseous cylces Is a process by which elements like oxygen,carbon, nitrogen & water move through atmosphere in a gaseous phase . The reservoir pool is atmosphere or water .
the Water Cycle.
Oceans are the larger reservoir of water.
The oceans. 97% of earth's water is in the oceans.
Oceans are the major sources for water evaporation.
Oceans are the major sources for water evaporation.
The abundance of plants and the fact that they take in so much Carbon Dioxide for photosynthesis makes plants a major reservoir for carbon. Sedimentary rock comprises the largest single reservoir in the carbon cycle. The world's oceans are the second-largest reservoir in the carbon cycle.
The carbon cycle is the cycle which includes an underground reservoir in the from of fossil fuels.
Cycle King was established back in 1968 and is now the largest family owned cycle retailer in the United Kingdom. The headquarters is located in Oxford.
atmosphere
Gaseous cylces Is a process by which elements like oxygen,carbon, nitrogen & water move through atmosphere in a gaseous phase . The reservoir pool is atmosphere or water .
Biogeochemical cycles are basically of two types: a) Gaseous cycles like carbon (as carbon dioxide), oxygen, nitrogen, etc. b) Sedimentary cycles like sulphur, phosphorus, etc. In gaseous cycles, the elements have a main reservoir in the gaseous phase, and the reservoir pool is the atmosphere or water. The biogenetic materials involved in circulation pass through a gaseous phase before completing the cycle. In sedimentary cycles, the elements main reservoir pool is lithosphere and the biogenetic materials involved in circulation are non-gaseous. The sedimentary cycles are usually very slow as the elements may get locked up in rocks and go out of circulation for long periods.
Biogeochemical cycles are basically of two types: a) Gaseous cycles like carbon (as carbon dioxide), oxygen, nitrogen, etc. b) Sedimentary cycles like sulphur, phosphorus, etc. In gaseous cycles, the elements have a main reservoir in the gaseous phase, and the reservoir pool is the atmosphere or water. The biogenetic materials involved in circulation pass through a gaseous phase before completing the cycle. In sedimentary cycles, the elements main reservoir pool is lithosphere and the biogenetic materials involved in circulation are non-gaseous. The sedimentary cycles are usually very slow as the elements may get locked up in rocks and go out of circulation for long periods.
the Water Cycle.