Difference between revisions of "AY Honors/Ecology - Advanced/Answer Key"

Revision as of 06:41, 29 June 2006

In ecology, a biogeochemical cycle is a circuit or pathway by which a chemical element or molecule 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 chemicals are sometimes held for long periods of time in one place. This place is called a reservoir, which, for example, includes such things as coal deposits that are storing carbon for a long period of time. When chemicals are held for only short periods of time, they are being held in exchange pools. Generally, reservoirs are abiotic factors while exchange pools are biotic factors. Examples of exchange pools include plants and animals, which temporarily use carbon in their systems and release it back into the air or wherever. Carbon is held for a relatively short time in plants and animals when compared to coal deposits. The amount of time that a chemical is held in one place is called its residence.

The most well-known and important biogeochemical cycles, for example, include the carbon cycle, the nitrogen cycle, the oxygen cycle, the phosphorus cycle, and the water cycle.

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.

@@ Line 1: / Line 1: @@
 In [[ecology]], a '''biogeochemical cycle''' is a circuit or pathway by which a [[chemical element]] or [[molecule]] 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 Earth does not constantly receive more chemicals as it receives light. The Earth only has those chemicals that were formed in the creation of the Earth, and the only way to obtain more chemicals or nutrients is from occasional meteorites from outer space that contain those elements. Because chemicals operate on a closed system and cannot be lost and replenished like energy can, these chemicals must be recycled throughout all of Earth’s processes that use those chemicals or elements. These cycles include both the living biosphere, and the nonliving lithosphere, atmosphere, and hydrosphere. The term "biogeochemical" takes its prefixes from these cycles: Bio refers to the biosphere. Geo refers collectively to the lithosphere, atmosphere, and hydrosphere. Chemical, of course, refers to the chemicals that go through the cycle.
+The chemicals are sometimes held for long periods of time in one place. This place is called a '''reservoir''', which, for example, includes such things as [[coal]] deposits that are storing carbon for a long period of time. When chemicals are held for only short periods of time, they are being held in '''exchange pools'''. Generally, reservoirs are abiotic factors while exchange pools are biotic factors. Examples of exchange pools include plants and animals, which temporarily use carbon in their systems and release it back into the air or wherever. Carbon is held for a relatively short time in plants and animals when compared to coal deposits. The amount of time that a chemical is held in one place is called its '''residence'''.
 The most well-known and important biogeochemical cycles, for example, include the [[carbon cycle]], the [[nitrogen cycle]], the [[oxygen cycle]], the [[phosphorus cycle]], and the [[water cycle]].
 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.