4.5 Article

Geochemistry of arsenic and metals in stored tailings of a Co-Ni arsenide-ore, Khovu-Aksy area, Russia

Journal

APPLIED GEOCHEMISTRY
Volume 27, Issue 11, Pages 2238-2250

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.apgeochem.2012.02.033

Keywords

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Funding

  1. RFBR [08-05-00688, 10-05-00518, 11-05-00742]

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Interest in the redistribution of As-bearing species during long-term storage of hydrometallurgical tailings is motivated partly by the need to prevent As from being released into the environment. The speciation of As in mine wastes from the Tuva Cobalt Plant (Khovu-Aksy mine site, Tuva Republic, Russia) has been studied using mineralogical techniques, and chemical analyses of solids (tailings, soils, vegetation) and solutions (recovered pore waters, leach solutions). Ore at the plant was processed by hot autoclave leaching with an ammoniacal carbonate solution followed by treatment with CO2(gas) and caustic magnesite, MgO. Pronounced differences in element concentrations were measured in the five separate tailings ponds and one trench that were filled sequentially during operation of the plant. The concentration of each element was relatively uniform within each pond but the correlations among solid-phase Co, Ni, Zn and Cu gradually decrease from the most recent to oldest ponds as does the correlation between solid-phase As, Ag, Cd and Pb. In the oldest ponds, significant correlations are present between solid-phase Fe-As, Fe-Sb and Fe-Zn. High carbonate content in the ores and leaching reagents control the pH of the pore waters (pH = 7.27-9.10) where the major cation is Ca2+, followed by NH4+ and Mg2+. Concentrations of As in pore solutions reach up to 140 mg L-1, and average 15 mg L-1. The high pore-water As concentrations are a consequence of instability of the processing residues, which include Mg(NH4)AsO4 center dot nH(2)O and Mg-3(AsO4)(2)center dot nH(2)O. The concentrations of Zn, Cu and As in pore waters increase from the youngest pond to the oldest storage impoundment (trench), which is evidence of the increase in element mobility with time. In contrast to the metals, As is preferentially sorbed to Fe oxides formed in the tailings. Aerosol transport of dust from the dry ponds has produced anomalies of As and metals in the surrounding area with As in the most polluted soils reaching up to 540 ppm. Moreover, vegetation growing on the surface of the disposal ponds absorbs solutes from the soil. (C) 2012 Elsevier Ltd. All rights reserved.

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