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The effect of weathering on the acid-producing potential of the Goathill North Rock Pile, Questa mine, NM

机译:风化对新墨西哥州Questa矿山Goathill North Rock桩产酸潜力的影响

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The Goathill North (GHN) rock pile was constructed in 1964-74 and re-graded in 2004-05. GHN samples were subjected to static, petrographic, and chemical tests to characterize acidity and future acid-producing potential (AP). Samples that have higher concentrations of pyrite are more likely to have a higher AP. Static tests indicated that, although the rock-pile material contains acid consuming minerals, acid generation has occurred. Samples with rhyolite rock fragments have lower NP (neutralization potential) then samples with andesite rock fragments. Samples with rhyolite rock fragments had undergone hydrothermal quartz-sericite-pyrite (QSP) alteration, whereas samples with andesite rock fragments were propylitically altered; these hydrothermal alterations occurred after the molybdenum mineralization, but prior to mining. No single component controls the ABA (acid-base accounting) and NAG (net acid generation) tests. This lack of correlation between ABA and NAG tests, mineralogy, and chemistry is a result of 1) weathering reactions in the soil matrix producing precipitation of coatings surrounding the rock fragments and preventing further weathering of the rock fragments, especially around pyrite crystals, 2) a lack of the water available that is required for weathering in the 25-40 years since the formation of GHN rock pile, 3) non-uniform weathering of pyrite within the rock pile due to heterogeneous air flow, and 4) little or no weathering of the rock fragments. Also, the AP capacity of the rock-pile is determined by the combination of K-feldspar, calcite, smectite, illite, and pyrite, which are controlled in part by the lithology, pre-mining hydrothermal alteration, and post-mining weathering. The effects of pre-mining hydrothermal alteration and post-mining weathering both affect the static tests, emphasizing the need to perform detailed petrographic and mineralogic investigations along with the static tests to determine the AP of any mine waste material.
机译:Goathill North(GHN)岩石桩建于1964-74年,并于2004-05年进行了重新分级。 GHN样品经过了静态,岩石学和化学测试,以表征酸度和未来的产酸潜力(AP)。黄铁矿浓度较高的样品更有可能具有较高的AP。静态测试表明,尽管岩石堆材料中含有消耗酸的矿物,但仍发生了酸的产生。带流纹岩碎块的样品比具有安山岩碎块的样品具有更低的NP(中和潜力)。流纹岩碎石样品经历了热液石英-绢云母-黄铁矿(QSP)蚀变,而安山岩碎石样品发生了丙基化变化。这些热液蚀变发生在钼矿化之后,但在开采之前。没有哪个组件可以控制ABA(酸碱会计)和NAG(净酸生成)测试。 ABA和NAG测试,矿物学​​和化学性质之间缺乏相关性是由于以下原因造成的:1)土壤基质中的风化反应在岩石碎片周围产生了涂层沉淀,并阻止了岩石碎片的进一步风化,特别是在黄铁矿晶体周围,2)自GHN岩堆形成以来,在25-40年内缺乏风化所需的可用水; 3)由于异质气流,导致岩堆内黄铁矿的风化不均匀;以及4)很少或没有风化的岩石碎片。同样,岩石桩的抗压强度由钾长石,方解石,蒙脱石,伊利石和黄铁矿的组合确定,这些组合部分受岩性,开采前热液蚀变和开采后风化的控制。开采前热液蚀变和开采后风化的影响均会影响静态测试,强调需要进行详细的岩石学和矿物学研究以及静态测试以确定任何矿山废料的AP。

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