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File:Fluorine cycle draft2.pngFluorine cycle: F fluxes[1] are in Tg/yr and reservoir data[2] is in mg/kg. The major mechanisms that mobilize fluorine are chemical and mechanical weathering of rocks. Major anthropogenic sources also include industrial chemicals and fertilizers, brick manufacturing, and groundwater extraction. Fluorine is primarily carried by rivers to the oceans, where it can have a residence time of about 500,000 years. Fluorine can be removed from the ocean by deposition of terrigenous or authigenic sediments, or subduction of the oceanic lithosphere.
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- ^ Schlesinger, William H.; Klein, Emily M.; Vengosh, Avner (2020). "Global Biogeochemical Cycle of Fluorine". Global Biogeochemical Cycles. 34 (12). doi:10.1029/2020gb006722. ISSN 0886-6236.
- ^ Rudnick, R.L.; Gao, S. (2003), "Composition of the Continental Crust", Treatise on Geochemistry, Elsevier, pp. 1–64, doi:10.1016/b0-08-043751-6/03016-4, ISBN 978-0-08-043751-4
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 01:01, 3 April 2021 | | 1,440 × 900 (190 KB) | Jmckaig (talk | contribs) | [[File:Fluorine cycle draft2.png|thumb|Fluorine cycle: F fluxes<ref name=":0">{{Cite journal|last=Schlesinger|first=William H.|last2=Klein|first2=Emily M.|last3=Vengosh|first3=Avner|date=2020|title=Global Biogeochemical Cycle of Fluorine|url=http://dx.doi.org/10.1029/2020gb006722|journal=Global Biogeochemical Cycles|volume=34|issue=12|doi=10.1029/2020gb006722|issn=0886-6236}}</ref> are in Tg/yr and reservoir data<ref>{{Citation|last=Rudnick|first=R.L.|title=Composition of the Continental Crus... |
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