Authigenic Barite in Tailing Dumps: Mineralogical and Geochemical Data and Results of Physico-Chemical Modeling

Abstract

On the example of the Novo-Ursk tailing dump (Salair Ridge), the typomorphic characteristics of barite are considered. It was found that in the dumps, in addition to residual barite from pyrite-polymetallic ores, there are its authigenic varieties. Ore barite grains are found in the form of fragments of irregular shapes, less often grains of a tabular habit, have a dimension of 50–400 microns, Sr up to 1.41 wt.%. Newly formed barite occurs as single grains or clusters of round and elongated shapes or acicular crystals, ranging in size from 1–2 µm to larger aggregates that form veinlets or clusters in the siliceous matrix in association with jarosite and/or anhydrite. Among the impurities, Pb up to 6.33 wt.% was noted, less often Fe up to 0.73 wt.%, Sr up to 0.94 wt.%. It was shown by using thermodynamic modeling that the concentrations of Ba, SO4, Fe and Ca in solution vary within several orders of magnitude when the mineral composition of the tailings mound zones changes depending on the Eh–pH conditions of their formation. It has been suggested that the formation of barite along with pyrite may occur as a result of the action of a reductive biogeochemical barrier or a sulfate concentration barrier in the deeper parts of the section where supersaturation is achieved.The most informative typomorphic feature proving that barite was formed under tailings conditions is particle morphology, mineral association and chemical composition.