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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Hydrochemistry, mineralogy and chemical fractionation of mine and processing wastes associated with porphyry copper mines: A case study from the Sarcheshmeh mine, SE Iran
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Hydrochemistry, mineralogy and chemical fractionation of mine and processing wastes associated with porphyry copper mines: A case study from the Sarcheshmeh mine, SE Iran

机译:与斑岩铜矿有关的矿山和加工废料的水化学,矿物学和化学分馏:以伊朗东南部Sarcheshmeh矿为例

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摘要

The Sarcheshmeh is one of the largest Oligo-Miocene porphyry Cu deposits in the world. Comparative hydrochemical, mineralogical and chemical fractionation associated with mining efflorescence salts and processing wastes of this mine are discussed. Hydrochemical results showed that rock waste dumps, reject wastes and old impoundments of tailings are the main sources of acid mine drainage waters (AMD) that contain potentially toxic metals such as Cd, Co, Cu, Mn, Ni and Zn as well as Al. Episodic fluxes of highly contaminated acidic waters were produced in a tailings dam over a short period of time. Secondary soluble minerals provide important controls on the quality of AMD produced, especially in old, dry tailings impoundments. Secondary sulfate minerals such as gypsum, magnesiocopiapite, hydronium jarosite, kornelite and coquimbite were found in rock waste drainages and in old weathered reject wastes. Highly soluble secondary minerals such as gypsum, eriochalcite, and bonattite are also observed in an evaporative layer on old tailings impoundments. Chemical fractionation patterns of potentially toxic elements showed that the geochemical behavior of metals is primarily controlled by the mineralogical composition of waste samples. Elements such as Co, Cr, Cu, Mn, Ni and Zn are readily released into the water soluble fraction from efflorescence salts associated with rock waste drainages, as well as from the evaporative layer of old tailings. Potentially toxic elements, such as As, Mo and Pb, are principally adsorbed or co-precipitated with amorphous and crystalline Fe oxides, but they may also be associated with oxidizing, primary sulfides and residual fractions. Following the development of the dammed tailings pond, the secondary minerals were dissolved, producing acidic waters contaminated by Al (154mgL~(-1)), Cu (150mgL~(-1)), Cd (0.31mgL~(-1)), Co (2.13mgL~(-1)), Mn (73.7mgL~(-1)), Ni (1.74mgL~(-1)), Zn (20.3mgL~(-1)) and Cl (1690mgL~(-1)). Therefore, the potential use of recycled water from the Sarcheshmenh dammed tailings pond is diminished by the presence of corrosive ions like Cl- in highly acidic fluids that promote corrosion of pipes and pumps in the water recycling system.
机译:Sarcheshmeh是世界上最大的中新世斑岩型铜矿床之一。讨论了与开采风化盐和该矿山的加工废料有关的比较水化学,矿物学和化学分馏。水化学结果表明,岩石废料堆,废品废物和尾矿的旧堆积物是酸性矿山排水(AMD)的主要来源,这些酸性矿山排水含有潜在的有毒金属,例如Cd,Co,Cu,Mn,Ni和Zn以及Al。短时间内在尾矿坝中产生了高污染酸性水的偶发通量。次生可溶性矿物质对产生的AMD的质量提供了重要的控制,特别是在老的干尾矿库中。在岩石废物排水系统和老风化的废物废物中发现了次生硫酸盐矿物,例如石膏,菱镁矿,水合黄钾铁矾,钾锰矿和白云石。在老尾矿库房的蒸发层中也观察到了高溶解度的次生矿物,例如石膏,硅铝石和方钠石。潜在有毒元素的化学分馏模式表明,金属的地球化学行为主要受废物样品的矿物组成控制。诸如Co,Cr,Cu,Mn,Ni和Zn等元素很容易从与废石料排放相关的风化盐以及旧尾矿的蒸发层中释放到水溶性馏分中。潜在的有毒元素(例如As,Mo和Pb)主要与非晶和结晶的Fe氧化物吸附或共沉淀,但它们也可能与氧化,初级硫化物和残留部分有关。随着坝尾矿池的发展,次生矿物质被溶解,产生了被Al(154mgL〜(-1)),Cu(150mgL〜(-1)),Cd(0.31mgL〜(-1))污染的酸性水。 ,Co(2.13mgL〜(-1)),Mn(73.7mgL〜(-1)),Ni(1.74mgL〜(-1)),Zn(20.3mgL〜(-1))和Cl(1690mgL〜( -1))。因此,由于在高酸性流体中存在诸如Cl-之类的腐蚀性离子,从而削弱了Sarcheshmenh筑坝的尾矿池中循环水的潜在用途,从而促进了水循环系统中管道和泵的腐蚀。

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