The non-participation of organic sulphur in acid mine drainage generation
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Abstract
Acid mine drainage is commonly associated with land disturbances that encounter and expose iron sulphides to oxidising atmospheric conditions. The attendant acidic conditions solubilise a host of trace metals. Within this flow regime the potential exists to contaminate surface drinking water supplies with a variety of trace materials. Accordingly, in evaluating the applications for mines located in the headwaters of water sheds, the pre-mining prediction of the occurrence of acid mine drainage is of paramount importance. There is general agreement among investigators that coal organic sulphur is a nonparticipant in acid mine drainage generation; however, there is no scientific documentation to support this consensus. Using simulated weathering, kinetic, mass balance, petrographic analysis and a peroxide oxidation procedure, coal organic sulphur is shown to be a nonparticipant in acid mine drainage generation. Calculations for assessing the acid-generating potential of a sedimentary rock should not include organic sulphur content.
Publication type | Article |
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Publication Subtype | Journal Article |
Title | The non-participation of organic sulphur in acid mine drainage generation |
Series title | Environmental Geochemistry and Health |
DOI | 10.1007/BF01758669 |
Volume | 11 |
Issue | 3-4 |
Year Published | 1989 |
Language | English |
Publisher location | Kluwer Academic Publishers |
Description | 6 p. |
First page | 187 |
Last page | 192 |
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