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Geochemistry of Trace Metals and Rare Earth Elements in Stream Water, Stream Sediments and Acid Mine Drainage from Darrehzar Copper Mine, Kerman, Iran

机译:来自伊朗克尔曼达雷赫扎尔铜矿的溪流水,溪流沉积物和酸性矿山中的微量金属和稀土元素的地球化学

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Darrehzar porphyry copper mine is located 10km south of the famous Sarcheshmeh porphyry copper mine in Kerman province, Iran. Water and sediment samples in the Darrehzar porphyry copper mine were collected and analyzed in order to characterize the environmental effects of regional geology and mining activity. Stream affected by acid mine drainage (AMD) are Ca-SO_4~(2-) in type, while unaffected streams are Ca-HCO_3~- type. Acid drainage, with pH values as low as 2.5, is quite rich in dissolved copper (mean 306.53 mg/L) > iron (77.83 mg/L) > aluminium (48.62 mg/L) > manganese (6.90 mg/L) > zinc (2810.42 μg/L) > cobalt (831.55 μg/L) > nickel (298.47 μg/L). The high sulfate concentration makes sulfate the major controlling factor of electrical conductivity. The strong correlation among the majority of the elements indicates either similar geochemical behavior or a common origin, (mostly sulfides). Calculation of Acid Mine Drainage Index (AMDI) indicates that Darrehzar mine is classified as dangerous in view of AMD hazards. In Darrehzar porphyry copper mine, total rare earth element content (∑REE) in AMD (5.54-417.76 μg L~(-1)) is higher than natural water (REE in upstream and downstream water is 0.87-1.40 and 0.83- 1.71 μg L~(-1) respectively). The North American Shale Composite (NASC) normalized REE patterns of AMDs revealed strong enrichment of middle REE (MREE), and heavy REE (HREE) compared with light REE (LREE). Speciation modeling indicates the predominance of aqueous species i.e., LnSO_4~+, Ln(SO_4)_2~-, Ln~(3+), LnCO_3~+, LnHCO_3~(2+) and Ln(CO_3)_2~- (Ln refers to any lanthanide element). In upstream, where pH is 7.2 ≤ pH, REEs primarily exist as LnCO_3~+, and HREE bicarbonate complexes (Ln (CO_3)_2~-) exceed those of LREEs. Based on mean geoaccumulation indices (I_(geo)), Darrehzar river sediments at mine site display the following trend:Cu > Mo > Pb > Sb > Cd. Calculated potential ecological risk index (RI) indicates higher risk at mine site. The mean potential ecological risk factors (E_i) for sediment metals display the following trend:Mo > Cd > Cu > As > hbox Pb > Ni > Cr > Zn.
机译:Darrehzar斑岩铜矿位于伊朗克尔曼省著名的Sarcheshmeh斑岩铜矿以南10公里处。收集并分析了Darrehzar斑岩铜矿中的水和沉积物样本,以表征区域地质和采矿活动的环境影响。受酸性矿山排水(AMD)影响的流为Ca-SO_4〜(2-)型,未受影响的流为Ca-HCO_3〜-型。 pH值低至2.5的酸排泄中含有丰富的溶解铜(平均306.53 mg / L)>铁(77.83 mg / L)>铝(48.62 mg / L)>锰(6.90 mg / L)>锌(2810.42μg/ L)>钴(831.55μg/ L)>镍(298.47μg/ L)。高硫酸盐浓度使硫酸盐成为电导率的主要控制因素。大多数元素之间的强相关性表明相似的地球化学行为或共同的起源(主要是硫化物)。酸性矿山排水指数(AMDI)的计算表明,考虑到AMD危害,Darrehzar矿山被归类为危险矿山。在Darrehzar斑岩铜矿中,AMD中的总稀土元素含量(∑REE)(5.54-417.76μgL〜(-1))高于天然水(上,下游水的REE为0.87-1.40和0.83- 1.71μg L〜(-1))。与轻质稀土(LREE)相比,北美页岩复合材料(NASC)规范化的稀土元素稀土模式显示出中稀土(MREE)和重稀土(HREE)的富集。形态建模表明水相物种占优势,即LnSO_4〜+,Ln(SO_4)_2〜-,Ln〜(3 +),LnCO_3〜+,LnHCO_3〜(2+)和Ln(CO_3)_2〜-(Ln指到任何镧系元素)。在上游,pH为7.2≤pH时,REE主要以LnCO_3〜+的形式存在,而HREE碳酸氢盐配合物(Ln(CO_3)_2〜-)超过了LREE。根据平均地质累积指数(I_(geo)),矿区的达勒赫萨尔河沉积物显示出以下趋势:Cu> Mo> Pb> Sb> Cd。计算出的潜在生态风险指数(RI)表示矿场风险较高。沉积物金属的平均潜在生态风险因子(E_i)呈现以下趋势:Mo> Cd> Cu> As> hbox Pb> Ni> Cr> Zn。

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