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Water cycle
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=== Biogeochemical cycling === While the water cycle is itself a [[biogeochemical cycle]], flow of water over and beneath the Earth is a key component of the cycling of other biogeochemicals.<ref>{{cite web |publisher=The Environmental Literacy Council |url=http://www.enviroliteracy.org/subcategory.php/198.html |title=Biogeochemical Cycles |url-status=live |archive-url=https://web.archive.org/web/20150430133927/http://enviroliteracy.org/subcategory.php/198.html |archive-date=2015-04-30 |access-date=2006-10-24}}</ref> Runoff is responsible for almost all of the transport of eroded [[sediment]] and [[phosphorus]] from land to [[waterbody|waterbodies]].<ref>{{Cite web |url=https://enviroliteracy.org/air-climate-weather/biogeochemical-cycles/phosphorus-cycle/ |title=Phosphorus Cycle |work=The Environmental Literacy Council |access-date=2018-01-15 |url-status=live |archive-url=https://web.archive.org/web/20160820012731/http://enviroliteracy.org/air-climate-weather/biogeochemical-cycles/phosphorus-cycle/|archive-date=2016-08-20}}</ref> The [[salinity]] of the oceans is derived from [[erosion]] and transport of dissolved salts from the land. Cultural [[eutrophication]] of lakes is primarily due to phosphorus, applied in excess to [[field (agriculture)|agricultural fields]] in [[fertilizer]]s, and then transported overland and down rivers. Both runoff and groundwater flow play significant roles in transporting nitrogen from the land to waterbodies.<ref>{{cite web |publisher=Ohio State University |website=Extension Fact Sheet |url=http://ohioline.osu.edu/aex-fact/0463.html |title=Nitrogen and the Hydrologic Cycle |url-status=dead |archive-url=https://web.archive.org/web/20060901071850/http://ohioline.osu.edu/aex-fact/0463.html |archive-date=2006-09-01 |access-date=2006-10-24}}</ref> The [[dead zone (ecology)|dead zone]] at the outlet of the [[Mississippi River]] is a consequence of [[nitrate]]s from fertilizer being carried off agricultural fields and funnelled down the [[river system]] to the [[Gulf of Mexico]]. Runoff also plays a part in the [[carbon cycle]], again through the transport of eroded rock and soil.<ref>{{cite web |publisher=NASA |website=Earth Observatory |title=The Carbon Cycle |url=http://earthobservatory.nasa.gov/Library/CarbonCycle/ |url-status=dead |archive-url=https://web.archive.org/web/20060928223836/http://earthobservatory.nasa.gov/Library/CarbonCycle/ |archive-date=2006-09-28 |access-date=2006-10-24|date=2011-06-16 }}</ref>
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