Hydrogeochemische Untersuchungen an Erzgebirgischen Gruben- und Oberflächenwässern

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The chemical composition of mine-waters from different ore-districts in the Erzgebirge was studied over a period of several months. The composition changes were due to climatic factors but nearly all ore formations give rather characteristic trace-element-associations in the mine waters. For some districts, the quantity of metals transported as ionic or colloidal solutions over a year are calculated. Further, the writers give the results of a hydrogeochemical investigation over the whole course of the Mulde--a little river, whose source lies at about 800 m altitude in a crystalline region and receives as affluents, waters from most of the oredistricts of Saxony. The second half of the Mulde lies in the diluvial plains, and after a course of 115 km it flows into the Elbe. Solution, transport, sorption and precipitation of mobilized matter were investigated and quantitative data for several metals are given.

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