Abstract
The alunite–jarosite minerals are defined as having the general formula AB 3( X O4)2(OH)6, where A is a large ion in 12-fold coordination ( e.g. , K, Na, Ca, Pb, REE ), B is usually Fe or Al, and the X O4 anions are usually SO4, PO4 or AsO4. Because of the potential for a large number of complex
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