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1.
Mehdi Khorasanipour Majid H. Tangestani Reza Naseh Hamid Hajmohammadi 《Mine Water and the Environment》2012,31(3):199-213
This paper presents chemical fractionation and contamination intensities of trace elements in stream sediments at the Sarcheshmeh mine, southeastern Iran, which is one of the world’s largest Oligo-Miocene porphyry copper deposits. Evaluation of environmental pollution indices and maximum probable background concentrations revealed that As, Cu, Cd, Mo, Pb, Sb, Se, S, and Zn are highly concentrated in the contaminated sediments, while Cr, Co, Ni, Fe, and Mn show lower enrichment values. Discharges of industrial effluents (especially those contaminated by tailings), reject waste from the semi-autogenous mill, and rock waste drainages are the main anthropogenic contaminant sources. High values of As, Cu, Fe, Mo, Pb, and Zn were associated with the oxidizable, primary sulfide, and residual sediment fractions. Relatively high percentages of Co (>92?%), Cr (>58?%), Cu (>79?%), Fe (>40?%), Mn (>97?%), Ni (>87?%), and Zn (>83?%) in the sediments associated with the rock waste drainages were readily released during the extraction of water-soluble, exchangeable, and carbonate fractions. Sediments that received reject waste drainages were also polluted by As (>351.7?mg?kg?1), Cu (>1.58?%), Mo (>91.8?mg?kg?1), Pb (>291.8?mg?kg?1), and Zn (>762.4?mg?kg?1). A large percentage of these contaminants were found to be adsorbed and co-precipitated with amorphous Fe-oxides and carbonate phases. The chemical fractionation pattern of the potentially hazardous trace elements corresponded well with the mineralogical composition of the contaminated sediments. 相似文献
2.
Shafaei Foojan Doulati Ardejani Faramarz Bahroudi Abbas Yavarzade Mohamad Amini Aliasghar 《Mine Water and the Environment》2021,40(4):847-863
Mine Water and the Environment - The effect of the electrokinetic process on the extraction of trapped water was evaluated in the Miduk copper mine’s tailings slurry. The effect of the... 相似文献
3.
Laboratory and field treatment tests were performed to evaluate the effectiveness of lime treatment for mitigation of environmental
effects of acid mine drainage (AMD) at the Sarcheshmeh porphyry copper mine. AMD associated with the rock waste dumps is contaminated
with Al (>36,215 μg/L), Cd (>105 μg/L), Co (>522 μg/L), Cu (>53,250 μg/L), Mn (>42,365 μg/L), Ni (>629 μg/L), and Zn (>12,470 μg/L).
The concentrations of other metals (Fe, Mo, Pb, and Se) are low or below detection limits (As, Cr, and Sb). Due to the very
high Al and Mn content and the low concentration of Fe, a two-stage lime treatment method was chosen for the laboratory tests.
In the first stage, the AMD was treated at four pH set points: 7.5, 8.9, 9, and 10. In the second stage, after removing the
sludge at pH 9, treatment was continued at pH 10 and 11. The results indicated that a two-stage treatment method was not necessary
because elements such as Al, Cu, Co, and Zn were easily treated at pH 7.5, while complete removal of Cd, Mn, and Ni only required
a pH of 10. Increasing pH during the treatment process only caused a slight increase in Al. Field treatment tests support
the laboratory results. Lime treatment of highly contaminated AMD from dump 11, using simple low density sludge pilot scale
equipment, show that contaminant metals are treatable using this method. The mean treatment efficiency for contaminant metals
was 99.4% for Al, % for Cd, 99.6% for Co, 99.7% for Cu, 98.5% for Mn, 99.7% for Ni, 99% for U, and 99.5% for Zn. The optimum
pH for AMD treatment by lime was in the range of 9–10. The produced sludge in the treatment process was highly enriched in
the contaminant metals, especially Cu (>7.34%), Al (>4.76%), Mn (>2.94%), and Zn (>1.25%). A correlation coefficient matrix
indicates that the distribution pattern of the contaminant metals between soluble and precipitated phases is consistent with
the hydrochemical behavior of the metals during the lime treatment process. 相似文献
4.
Precipitation, surface, and groundwater samples were collected during 2009–2010 in the Sarcheshmeh copper mine drainage basin, Kerman Province, Iran. Groundwater samples were collected from both shallow and deep aquifers. All of the samples were analyzed for stable isotopes, deuterium (2H), and oxygen-18 (18O), and some were analyzed for tritium (3H). The results show a more restricted range of isotopic composition in groundwater samples than in precipitation samples based on the isotopic composition of the precipitation. The isotopic composition of surface and groundwater samples plot to the right of the local meteoric water line of the Sarcheshmeh area and around the evaporation line, indicating that the groundwater within the study area originates from meteoric water that has undergone secondary evaporation before or during recharge. Tritium was below the detection limit in the deep groundwater samples while shallow groundwater samples had tritium concentrations between 1.2 and 1.7 TU, which indicates a longer residence time for deep groundwater. 相似文献
5.
A laboratory study was undertaken using mine tailings and soil columns to evaluate some of the natural processes that can
control the mobility of metals at Pb–Ag mine tailings impoundments. The effects of buffering, pH, and salinity were examined
with tailings from the El Arteal deposit. Al, Ba, Cd, Cu, Fe, Mn, Ni, Pb, Sr, and Zn were mobilized when the tailings were
leached. However, when the mine tailings were placed above alluvial soils, Al, Ba, Cd, Cu, Mn, Pb, and Zn were retained, although
Fe and Sr clearly remained mobile. Most of the metal retention appears to be associated with the increase in pH caused by
calcite dissolution. The sorption of some metals (Cu, Pb, and Zn) onto oxyhydroxides of Fe and Mn, sulphates, clay materials,
and organic matter may also explain the removal of these metals from the leachate. 相似文献
6.
Abhishek RoyChowdhury Dibyendu Sarkar Yang Deng Rupali Datta 《Mine Water and the Environment》2017,36(2):248-254
In 1996, the Tab-Simco site, an abandoned coal mine 10 km southeast of Carbondale, Illinois, was listed as one of the most highly contaminated AMD sites in the mid-continent region. A suite of impacted soil and water samples were collected from various locations to characterize the current extent of AMD pollution, following standard U.S. EPA protocols. The mean pH of soil and water samples were found to be 2.69 and 2.07, respectively. The mean sulfur content of the soil samples was 0.5 %. The AMD-impacted soils contained high concentrations of Fe, Zn, Ni, Cr, Cu, Pb, and As. The AMD also contained high concentrations of Fe, As, Zn, Pb, Cr, Al, Cd, Cu, and Ni, as well as \({\text{SO}}_{4}^{2 - }\), all of which were significantly above their U.S. EPA permissible limits for surface water. 相似文献
7.
This study focused on acid neutralization reactions and the effects of water composition on the release and mobility of metals from mine tailings. The aims of this study were to: investigate leaching of metals from neutral mine tailings, determine the factors responsible for metal leaching, and investigate potential metal filtering by the soil. Tailings and soil samples were collected from an iron mine and analyzed. Equilibrium thermodynamic data and metal fractionation were then used to predict precipitation/dissolution of minerals and ion adsorption/desorption. Three column experiments were designed. The first column was filled with tailings, while the second column contained tailings above a layer of soil; both were leached with distilled water as rainfall. The third column was packed with soil and percolated with synthetic groundwater. The results indicated that iron (Fe) and zinc (Zn) mobility are mainly controlled by precipitation–dissolution mechanisms, while sorption onto oxides and carbonates limit the mobility of copper (Cu) and nickel (Ni). Cadmium (Cd) and manganese (Mn) mobility are affected by both mechanisms. Water discharging from column 3 (soil washed with groundwater) contained high concentrations of dissolved metals, indicating that water composition played an important role in metal mobility. Buffering minerals like carbonates and hornblende, chlorite, and albite decreased acid generation. 相似文献
8.
金属矿山的尾矿库、排土场由于含有大量的重金属,在长期的风化、淋溶作用下缓慢释放,从而污染土壤与地下水。本文对江西某铜矿排土场、尾矿库、疏干井排水口淤泥进行了取样测试。浸出毒性判别结果表明排土场土壤、尾矿砂及淤泥为不具有浸出毒性的危险废物,但浸出液浓度超过《地下水质量标准》中III类水标准,尤其是铜、铅、镉元素超标严重,对地下水环境构成威胁。重金属释放实验显示,随时间增加重金属释放量也增加,酸性降水条件下重金属释放量明显高于中性条件。因此,为避免土壤及地下水受到污染,应采取控制与修复措施。 相似文献
9.
菲律宾某尾矿中金的赋存状态 总被引:2,自引:0,他引:2
菲律宾某尾矿库中矿样是金矿全泥氰化的浸渣,古Au0.88g/t,含Ag4.94g/t.在传统显镜观察及化学物相分析等研究办法基础上,结合矿物自动分析仪MLA查明尾矿库中金的赋存状态.矿样中82.95%的金以自然金、银金矿形式存在,17.05%以碲金矿、碲金银矿形式存在.自然金、银金矿产出粒度一般小于0.125mm,碲金矿、碲金银矿产出粒度均小于0.020mm,金矿物产出特征复杂,主要以硫化矿物包裹体、褐铁矿包裹体、石英及方解石等脉石矿物包裹体形式存在. 相似文献
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11.
The Hydrogeochemistry of Arsenic in
the Clara Mine,Germany 总被引:1,自引:1,他引:0
Abstract.
The oxidative dissolution of primary arsenic-bearing
sulfide minerals in barite-fluorite veins is a potential source
of arsenic in the Clara Mine. Geological structures, especially
the mineral veins, provide potential pathways for the water. The
highest arsenic concentrations are found in ground water within
the eastern part of the mine. Arsenic and major ions are
positively correlated and provide evidence that arsenic is
likely derived locally from the water-vein/water-rock
interaction. Geochemical modeling with PHREEQC shows all the
arsenate mineral phases to be significantly undersaturated,
although secondary arsenate minerals are common in the oxidized
part of the deposit. The mine waters plot near the boundary of
Fe(OH)3 and
Fe2+ in the pH-Eh diagram for the
As-Fe-S-H2O-system. Arsenic occurs as the
5-valent species
and
. Statistical analysis
illustrates a strong association between As, Fe, pH, and
HCO3. Oxidation of the primary As-bearing
minerals, such as pyrite and arsenopyrite, and the subsequent
behavior of the oxyanion, arsenate, generally controls the
distribution and speciation of arsenic. The low concentrations
of dissolved As is due to co-precipitation and adsorption of
arsenate by Fe, Al, and Mn (oxy)hydroxides. 相似文献
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13.
贵州某金矿尾矿综合利用研究 总被引:2,自引:0,他引:2
为给贵州某金矿综合利用其尾矿资源提供初步的技术基础,进行了试验研究,试验采用浮选的方法先将金富集在金精矿中,然后对这种金精矿采用焙烧-氰化浸出的方法进行处理。试验取得了较好的效果:金精矿品位达到43.4g/t,回收率达到90.56%,尾矿品位为0.21 g/t;焙烧后金精矿的浸出率可达80.94%。因此,在该金矿进行尾矿的综合利用是完全可行的。 相似文献
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从国内外几个典型尾矿坝事故分析入手,就导致尾矿坝失事的原因进行论述,认为管理、洪水、渗透及液化等是导致尾矿坝失事的主要原因,从而阐述应吸取的教训。 相似文献
17.
某金矿尾矿含金0.68 g/t,含银4.50 g/t,具有较高的综合利用价值,为进一步回收有用元素,对某金矿尾矿进行了工艺矿物学和选别工艺流程研究。原矿物相分析结果表明,金以自然金和包裹金的形式存在,其中自然金占56.50%。浮选试验结果表明:在-0.074 mm 80%的条件下,采用1粗1扫3精的浮选工艺流程,可获得金品位27.68 g/t、银品位107.311 g/t、金回收率72.18%、银回收率42.77%的金精矿,综合回收效果较好。 相似文献
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Mu Wenping Wu Xiong Ding Hanghang Geng Fuqiang Yu Shuai Zhang Xiao 《Mine Water and the Environment》2022,41(4):906-920
Mine Water and the Environment - Comprehensive analysis of hydrogeological conditions at a typical coal mine in northwestern China allowed us to establish a groundwater numerical model, which we... 相似文献