
The flow of materials from non living components to living components and back to the non living components in a more or less cyclic manner is called as
A)Gaseous cycle
B)Sedimentary cycle
C)Biogeochemical cycle
D)Hydrologic cycle
Answer
563.4k+ views
Hint: Non-living factors decide what living organisms will be sustained within the environment. The living species within the habitat have a sway on the non-living elements within the group. For instance, plants may affect soil chemistry, or some algae may affect water chemistry.
Complete answer:
The term gaseous cycle refers to the movement and transformation of gasses between different biogeochemical reservoirs, the lithosphere, the hydrosphere, the atmosphere and therefore the biosphere. Comprehension of the interactions between reservoirs is vital for any evaluation of gaseous biogeochemical cycles.
Sedimentary could be a cycle that has the weathering of existing rock, among the erosion of minerals, their transport and deposition, then burial. First-cycle sediments are distinguished by the presence of less resistant minerals and fragments of rock.
The hydrological cycle explains the exchange of water between the oceans, the atmosphere, the land surface, the biosphere, the soil, the groundwater and therefore the solid earth. The Hydrology Overview Article considers aspects of the worldwide water cycle and therefore the volume of water contained in these various reservoirs.
A biogeochemical or inorganic-organic cycle could be a circulating or repeatable pathway through which either an element or a molecule moves.
Hence, the correct answer is option (D)
Note: Some of the most biogeochemical cycles are as follows: (1) Water cycle or Hydrologic cycle (2) Carbon cycle (3) organic process (4) Oxygen cycle. Ecosystem producers take a spread of essential inorganic nutrients from their non-living environment.
Complete answer:
The term gaseous cycle refers to the movement and transformation of gasses between different biogeochemical reservoirs, the lithosphere, the hydrosphere, the atmosphere and therefore the biosphere. Comprehension of the interactions between reservoirs is vital for any evaluation of gaseous biogeochemical cycles.
Sedimentary could be a cycle that has the weathering of existing rock, among the erosion of minerals, their transport and deposition, then burial. First-cycle sediments are distinguished by the presence of less resistant minerals and fragments of rock.
The hydrological cycle explains the exchange of water between the oceans, the atmosphere, the land surface, the biosphere, the soil, the groundwater and therefore the solid earth. The Hydrology Overview Article considers aspects of the worldwide water cycle and therefore the volume of water contained in these various reservoirs.
A biogeochemical or inorganic-organic cycle could be a circulating or repeatable pathway through which either an element or a molecule moves.
Hence, the correct answer is option (D)
Note: Some of the most biogeochemical cycles are as follows: (1) Water cycle or Hydrologic cycle (2) Carbon cycle (3) organic process (4) Oxygen cycle. Ecosystem producers take a spread of essential inorganic nutrients from their non-living environment.
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