Science Fair Project Encyclopedia
Biogeochemical cycle
In ecology, a biogeochemical cycle is a circuit or pathway by which a chemical element moves through both biotic ("bio-") and abiotic ("geo-") compartments of an ecosystem. In effect, the element is recycled, although in some such cycles there may be places (called "sinks") where the element is accumulated or held for a long period of time. The water cycle involves not a chemical element, but a molecule of great significance to life.
Biogeochemical cycles always involve equilibrium states: a balance in the cycling of the element between compartments. However, overall balance may involve compartments distributed on a global scale.
Biogeochemical cycles of particular interest in ecology are:
- nitrogen cycle
- oxygen cycle
- carbon cycle
- phosphorus cycle
- sulfur cycle
- water cycle
- hydrogen cycle
03-10-2013 05:06:04
The contents of this article is licensed from www.wikipedia.org under the GNU Free Documentation License. Click here to see the transparent copy and copyright details
The contents of this article is licensed from www.wikipedia.org under the GNU Free Documentation License. Click here to see the transparent copy and copyright details


