Tracing the Origin and Evolution of Geochemical Characteristics of Waters from the Candiota Coal Mine Area (Southern Brazil): Part I

This work correlates surface and ground water composition to the substrata, and traces how water chemistry evolves at Brazil’s largest coal mine, the Candiota Mine. The water is dominated by SO 4 , Fe, Ca, and Mg. A pH range of 2.7–3 in the pit lakes is attributed through chemical models to concomit...

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Veröffentlicht in:Mine water and the environment 2016-03, Vol.35 (1), p.29-43
Hauptverfasser: Roisenberg, C., Loubet, M., Formoso, M. L., Berger, G., Munoz, M., Dani, N.
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Sprache:eng
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