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Publikováno v:
International Geology Review. 19:766-774
Ferrihydrite (2.5 Fe2O2-4.5 H2O) is an unstable colloidal mineral. It dissolves in highly alkaline solutions and is precipitated from them in the form of goethite. Jarosite is stable at very low pH but is decomposed at higher values of pH with separa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1c29077ced99a627f60a6f5acdbaabd
https://doi.org/10.1080/00206817709471076
https://doi.org/10.1080/00206817709471076
