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Al-Abed, S., Allen, D., Bates, E., & Reisman, D. (2002). Lime treatment lagoons technology for treating acid mine drainage from two mining sites.
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(2002). The BioSulphide Process to treat acid mine drainage and Anaconda tailings at Caribou Mine, New Brunswick (Vol. 2002-3).
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Stoica, L., & Dima, G. (2000). Pb(II) removal from aqueous systems by biosorption-flotation on mycelial residues of Penicillium chrysogenum. In A. Rozkowski (Ed.), 7th international Mine Water Association congress; Mine water and the environment (pp. 472–481). Sosnowiec: Uniwersytet Slaski.
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Magdziorz, A., & Sewerynski, J. (2000). The use of membrane technique in mineralised water treatment for drinking and domestic purposes at “Pokoj” coal mine district under liquidation. In A. Rozkowski (Ed.), 7th international Mine Water Association congress; Mine water and the environment (pp. 430–442). Sosnowiec: Uniwersytet Slaski.
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Turek, M. (2000). Recovery of NaCl from saline mine water in the ED-MSF system. 8th World Salt Symposium, Vols 1 and 2, , 471–475.
Abstract: A considerable part of water obtained by drainage of Polish coal-mines is saline which creates substantial ecological problems. The load of salt (mainly sodium chloride) amounts to 5 min t/year. Despite the utilisation of saline coalmine waters is considered to be the most adequate method of solving ecological problems caused by this kind of water in Poland there are only two installations utilising coal-mine waters and producing 100,000 t salt per year. In the case of the most concentrated waters, the so-called coal-mine brines, the method of concentrating by evaporation in twelve-stage expansion installation or vapour compression is applied, after which sodium chloride is manufactured. In the case of low salinity waters they are preconcentrated first by RO method. High energy consumption in above-mentioned methods of evaporation is a considerable restriction in the utilisation of coal-mine brines. An obstacle in the application of low energy evaporation processes, e.g. multi-stage flash, is the high concentration of calcium and sulphate ions in the coal-mine waters.
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