Geochemistry: Difference between revisions

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Latest revision as of 01:24, 18 February 2025

Geochemistry is the science that uses the principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans.<ref>https://www.wikimd.com/wiki/Geochemistry</ref>

The field can be divided into various sub-disciplines including, but not limited to, Biogeochemistry, Organic Geochemistry, Isotope Geochemistry, and Environmental Geochemistry.

Biogeochemistry[edit]

Biogeochemistry is the study of the chemical, physical, geological, and biological processes and reactions that govern the composition of the natural environment and its energy flows.

Organic Geochemistry[edit]

Organic Geochemistry involves the study of the impacts and processes that organisms have had on Earth.

Isotope Geochemistry[edit]

Isotope Geochemistry is the study of the relative and absolute concentrations of the elements and their isotopes using chemistry and geology.

Environmental Geochemistry[edit]

Environmental Geochemistry focuses on the study of the chemical processes and reactions which occur in the environment and the effects of human activity on these.

See Also[edit]

References[edit]

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