THE REDUCTION OF AQUEOUS AU3+ BY SULFIDE MINERALS AND GREEN RUST PHASES

dc.contributor.author	Heasman D.M.
dc.contributor.author	Sherman D.M.
dc.contributor.author	Ragnarsdottir K.V.
dc.date.accessioned	2021-11-28T04:25:36Z
dc.date.available	2021-11-28T04:25:36Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=14206070
dc.identifier.citation	American Mineralogist, 2003, 88, 5, 725-738
dc.identifier.issn	0003-004X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/32552
dc.description.abstract	The reactions of Au3+ with green rust, stibnite, pyrite, and chalcopyrite were investigated in the laboratory and the size of the gold clusters formed was measured using extended X-ray absorption fine structure (EXAFS) spectroscopy, scanning electron microscopy (SEM), and transmission electron microscopy (TEM). The individual clusters produced were between approximately 29 Å and 77 Å in diameter and may occur individually or as composite clusters from hundreds to thousands of angstroms in size. This work shows that it is possible to form "invisible" gold through reduction of Au3+ by green rust phases and the surfaces of sulfide minerals.
dc.title	THE REDUCTION OF AQUEOUS AU3+ BY SULFIDE MINERALS AND GREEN RUST PHASES
dc.type	Статья

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