首页> 外文会议>International conference on tailings and mine waste >The effect of weathering on the acid-producing potential of the Goathill North Rock Pile, Questa mine, NM
【24h】

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

机译:风化对Goathill北岩桩,Questa Mine,NM的产生潜力的影响

获取原文

摘要

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)摇滚桩于1964 - 74年建造,并于2004 - 05年重新评估。对GHN样品进行静态,岩体和化学试验,以表征酸度和未来酸产生潜力(AP)。具有较高浓度的黄铁矿的样品更可能具有更高的AP。静态试验表明,尽管岩石桩材料含有酸性消耗矿物质,但也发生了酸产生。具有菱形岩石碎片的样品具有较低的NP(中和电位),然后用安德烈岩石碎片样品。具有细流石岩石片段的样品经历了水热石英 - 丝晶醇 - 黄铁矿(QSP)改变,而使用安塞氏岩碎片的样品是旋涡性的改变;这些水热改变发生在钼矿化后发生,但在采矿前。没有单一组件控制ABA(酸基核算)和NAG(净酸生成)测试。 ABA和NAG测试,矿物学​​和化学之间缺乏相关性是1)土壤基质中的风化反应,产生围绕岩石片段的涂层沉淀并防止岩石片段的进一步风化,尤其是硫铁矿晶体,2)在25-40岁以来,由于GHN岩石桩的形成,3)由于异质空气流动,岩石桩内的岩石内的黄铁矿风化,而且,缺乏可用的水。岩石碎片。此外,岩石桩的AP容量由K-Feldspar,方解石,蒙脱石,伊尔氏岩和硫铁矿的组合决定,该岩石和硫铁矿由岩性,预先开采的水热改变和后开采耐候控制。预先采矿水热改变和开采后矿床的影响影响静态测试,强调需要进行详细的岩手和矿物学调查以及确定任何矿井废料的AP的静态试验。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号