geochemical cycle वाक्य
उदाहरण वाक्य
मोबाइल
- Ongoing geochemical cycles are one of the main attributes of geologically active worlds.
- The geochemical cycle encompasses the natural separation and concentration of elements and heat-assisted recombination processes.
- Flux in geochemical cycles is the movement of material between the deep Earth and the surface reservoirs.
- Some may use the terms biogeochemical cycle and geochemical cycle interchangeably because both cycles deal with Earth�s reservoirs.
- On terrestrial bodies such as the Earth, chemical cycles involving the lithosphere are known as geochemical cycles.
- Research on metal reduction by " G . fermentans " has contributed to understanding more about the geochemical cycling of metals in the environment.
- Geochemical cycles are concerned with the interactions between deep earth which consists of Earth�s mantle and core, and the lithosphere which consists of the Earth�s crust.
- During this time he published " The Carbonate-Silicate Geochemical Cycle and Its Effect on Atmospheric Carbon Dioxide over the Past 100 Million Years " in 1983.
- He has shown that biology leaves its imprint on global geochemical cycles, and that earth system function cannot be fully understood without considering the impacts of biology.
- Urban environments and outlying areas have been found to exhibit unique local temperatures, precipitation, and other characteristic activity due to a variety of factors such as pollution and altered geochemical cycles.
- However, a biogeochemical cycle refers to the chemical interactions in surface reservoirs such as the atmosphere, hydrosphere, lithosphere, and biosphere whereas a geochemical cycle refers to the chemical interactions that exist in crustal and sub crustal reservoirs such as the deep earth and lithosphere.
- ;Lithoautotroph : An organism ( usually bacteria ) whose sole source of carbon is carbon dioxide and exergonic inorganic oxidation ( chemolithotrophs ) such as " Nitrosomonas europaea "; these organisms are capable of deriving energy from reduced mineral compounds like pyrites, and are active in geochemical cycling and the weathering of parent bedrock to form soil
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