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Bell, A. V. (1975). Some Recent Experiences In Treatment Of Acidic, Metal-Bearing Mine Drainages. CIM Bull., 68(764), 39–46.
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Larsen, H. P. (1973). Chemical Treatment Of Metal-Bearing Mine Drainage. J. Water Poll. Control Fed., 45(8), 1682–1695.
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Lovell, H. L. (1971). Limestone Treatment Of Coal Mine Drainage. Min. Congr. J., 57(10), 28–&.
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Lovell, H. L. (1971). Mine Water Treatment Control. Min. Congr. J., 57(6), 83–&.
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Sasaki, K. (2006). Immobilization of Mn(II) ions by a Mn-oxidizing fungus – Paraconiothyrium sp.-like strain at neutral pHs. Mater. Trans., 47(10), 2457–2461.
Abstract: A Mn-oxidizing fungus was isolated from a constructed wetland of Hokkaido (Japan), which is receiving the Mn-impacted drainage, and genetically and morphologically identified as Paraconiothyrium sp.-like strain. The optimum pHs were 6.45-6.64, where is more acidic than those of previously reported Mn-oxidizing fungi. Too much nutrient inhibited fungal Mn-oxidation, and too little nutrient also delayed Mn oxidation even at optimum pH. In order to achieve the oxidation of high concentrations of Mn like mine drainage containing several hundreds g-m(-3) of Mn, it is important to find the best mix ratio among the initial Mn concentrations, inocolumn size and nutrient concentration. The strain has still Mn-tolerance with more than 380 g-m(-3) of Mn, but high Mn(II) oxidation was limited by pH control and supplied nutrient amounts. The biogenic Mn deposit was poorly crystallized birnessite. The strain is an unique Mn-oxidizing fungus having a high Mn tolerance and weakly acidic tolerance, since there has been no record about the property of the strain. There is a potentiality to apply the strain to the environmental bioremediation.
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