The iodine cycle is a biogeochemical cycle that primarily consists of natural[1] and biological processes[3] that exchange iodine through the lithosphere, hydrosphere, and atmosphere.[3][2] Iodine exists in many forms, but in the environment, it generally has an oxidation state of -1, 0, or +5.[1]
^ abcdefghijFuge, Ronald; Johnson, Christopher C. (1986). "The geochemistry of iodine — a review". Environmental Geochemistry and Health. 8 (2): 31–54. doi:10.1007/BF02311063. ISSN 1573-2983. PMID 24213950. S2CID 45457666.
^ abcWhitehead, D. C. (1984). "The distribution and transformations of iodine in the environment". Environment International. 10 (4): 321–339. doi:10.1016/0160-4120(84)90139-9. ISSN 0160-4120.
^ abcdAmachi, Seigo (2008). "Microbial Contribution to Global Iodine Cycling: Volatilization, Accumulation, Reduction, Oxidation, and Sorption of Iodine". Microbes and Environments. 23 (4): 269–276. doi:10.1264/jsme2.ME08548. ISSN 1342-6311. PMID 21558718.
^ abcMuramatsu, Yasuyuki; Yoshida, Satoshi; Fehn, Udo; Amachi, Seigo; Ohmomo, Yoichiro (2004). "Studies with natural and anthropogenic iodine isotopes: iodine distribution and cycling in the global environment". Journal of Environmental Radioactivity. Papers from the International Conference on Radioactivity in the Environment, Monaco, 1-5 September 2002. 74 (1): 221–232. doi:10.1016/j.jenvrad.2004.01.011. ISSN 0265-931X. PMID 15063550.
The iodinecycle is a biogeochemical cycle that primarily consists of natural and biological processes that exchange iodine through the lithosphere, hydrosphere...
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