Jarosites and Their Application in Hydrometallurgy
2000; Mineralogical Society of America; Volume: 40; Issue: 1 Linguagem: Inglês
10.2138/rmg.2000.40.8
ISSN1943-2666
Autores Tópico(s)Metal Extraction and Bioleaching
ResumoResearch Article| January 01, 2000 Jarosites and Their Application in Hydrometallurgy John E. Dutrizac; John E. Dutrizac Mining and Mineral Science Laboratories, CANMET, Natural Resources Canada, 555 Booth Street, Ottawa, Ontario, Canada K1A OG1 Search for other works by this author on: GSW Google Scholar John L. Jambor John L. Jambor Leslie Research and Consulting, 316 Rosehill Wynd, Tsawwassen, British Columbia, Canada V6T 1Z4 Search for other works by this author on: GSW Google Scholar Author and Article Information John E. Dutrizac Mining and Mineral Science Laboratories, CANMET, Natural Resources Canada, 555 Booth Street, Ottawa, Ontario, Canada K1A OG1 John L. Jambor Leslie Research and Consulting, 316 Rosehill Wynd, Tsawwassen, British Columbia, Canada V6T 1Z4 Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2000) 40 (1): 405–452. https://doi.org/10.2138/rmg.2000.40.8 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation John E. Dutrizac, John L. Jambor; Jarosites and Their Application in Hydrometallurgy. Reviews in Mineralogy and Geochemistry 2000;; 40 (1): 405–452. doi: https://doi.org/10.2138/rmg.2000.40.8 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search The alunite supergroup consists of more than 40 minerals with the general formula DG3(TO4)2(OH,H2O)6, wherein D represents cations with a coordination number greater or equal to 9, and G and T represent sites with octahedral and tetrahedral coordination, respectively (Smith et al. 1998). The supergroup is commonly subdivided into various groups, but the simplest primary subdivision is on the basis of the G cations. For all of the minerals in the supergroup, the dominant G cation is trivalent; most of the minerals have G represented by... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Referência(s)