Gold and silver in a system of sulfide tailings. Part 2: Reprecipitation on natural peat

Xehetasun bibliografikoak
Parent link:Journal of Geochemical Exploration
Vol. 165.— 2016.— [P. 8-22]
Erakunde egilea: Национальный исследовательский Томский политехнический университет Институт природных ресурсов Кафедра геоэкологии и геохимии
Beste egile batzuk: Myagkaya I. N. Irina Nikolaevna, Lazareva E. V. Elena Vladimirovna, Gustaytis M. A. Mariya Alekseevna, Zhmodik S. M. Sergey Mikhaylovich
Gaia:Title screen
More than eighty years of mining at the Novo–Ursk Au-bearing sulfide field (Kemerovo region, Russia) have produced a mixed natural–industrial system “wastes–gold-bearing acid mine drainage (AMD) waters–peat”. The behavior of Au, Ag and related elements in the system “wastes–AMD” is described in Part 1 of our study (Myagkaya et al. 2016) where we discuss interaction between the gold-bearing mine drainage waters and peat. This interaction leads to rapid accumulation of Ca, Fe, Mn, Ba, Cu, Zn, Se, Au, Ag, Hg, Pb to concentrations exceeding those in cyanidation wastes (especially, Cu, Zn, Se, Hg, and Pb). The contents of Au (about 5 ppm on average, locally as high as 155 ppm) and Ag (average about 11.2 ppm, locally up to 560 ppm) in peat are above the lowest economic values. These results provide clues to technologies for both generation of secondary gold (silver) deposits at existing or planned tailings and immobilization of toxic elements.
Режим доступа: по договору с организацией-держателем ресурса
Argitaratua: 2016
Gaiak:
Sarrera elektronikoa:http://dx.doi.org/10.1016/j.gexplo.2016.01.016
Formatua: Baliabide elektronikoa Liburu kapitulua
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=648418

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