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Static tests are the most widely used method to assess the net acid-generating potential of rocks at prospective mine sites. The results influence mine plans in which the safe disposal of wastes, such as tailings and waste rocks, is an environmental requirement in most jurisdictions. Static tests are chemical tests that are intended to provide predictions of the extent to which the minerals in representative samples will react to produce acidity, or neutralize acidity, during weathering in potential ARD (acid rock drainage) scenarios. Weathering, however, is not an instantaneous process that affects all minerals equally. Consequently, if static tests are to be interpreted meaningfully, the rates of weathering of the common gangue minerals need to be taken into account. Although the amount of neutralization contributed by an individual mineral during the vigorous reactions in most laboratory static tests is an important measure, it is commonly assumed that this amount of neutralization is directly correlative with that accessible during natural weathering. Static tests by definition exclude mineral-dissolution kinetics, but these vectors are intrinsic to the interpretation and application of the results of static tests. Experimental dissolution rates of silicate and aluminosilicate minerals are rapid relative to normal weathering rates, but most of these minerals react slowly relative to the rapidity at which acid is generated by the oxidation of iron sulphides. Most silicates or aluminosilicates therefore contribute to the attenuation of acidity only after ARD has already been established. For environmental assessments, it is suggested that carbonate contents (calcite and dolomite, but with siderite excluded) provide a more realistic assessment of whether rocks have neutralization potential adequate for the prevention of ARD

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