首页> 外文期刊>Geology of Ore Deposits: A Journal of Theoretical and Applied Papers on All Aspects of Ore Genesis >Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores: Part VII. Solubility of Synthetic Analogs of Erythrite and Annabergite at 25°C
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Thermodynamics of Arsenates, Selenites, and Sulfates in the Oxidation Zone of Sulfide Ores: Part VII. Solubility of Synthetic Analogs of Erythrite and Annabergite at 25°C

机译:硫化矿石氧化区中砷酸盐,亚硒酸盐和硫酸盐的热力学:第七部分。赤铁矿和黄铁矿的合成类似物在25°C的溶解度

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Understanding the mechanisms of arsenic's behavior under near-surface conditions is one of the actual problems of contemporary mineralogy and geochemistry and is important for solving environmental problems. The aim of this study is to synthesize analogs of erythrite and annabergite and to investigate their solubility in water. These phases have been synthesized by the boiling-dry of aqueous solutions of cobalt and nickel nitrates mixed with sodium hydroarsenate alkalized with NaOH. The samples obtained have been identified with electron microprobe, X-ray diffraction, and IR spectroscopy. Solubility has been determined by the isothermal saturation method in ampoules at 25°C. The solubility has been calculated using the Geochemist's Workbench (GMB 7.0) software package. The measured solubilities of erythrite and annabergite are 10~(-35.76) and 10~(36.43), respectively. Eh—pH diagrams were calculated and plotted using the GMB 7.0 software package. The database comprises the thermodynamic parameters of 46 elements, 47 main particles, 48 redox pairs, 552 particles in solution, 624 solid phases, and 10 gases. The Eh—pH diagrams of the Ni—As— H2O and Co—As—H2O systems were plotted for the average contents of these elements in the acidic waters in the oxidation zones of sulfide deposits. The formation of erythrite and annabergite under near-surface conditions is discussed.
机译:了解砷在近地表条件下的行为机理是当代矿物学和地球化学的实际问题之一,对解决环境问题具有重要意义。这项研究的目的是合成赤铁矿和菱锰矿的类似物,并研究它们在水中的溶解度。这些相是通过将钴和硝酸镍水溶液与用NaOH碱化的氢砷酸钠混合的溶液进行沸腾干燥而合成的。获得的样品已通过电子探针,X射线衍射和IR光谱进行了鉴定。溶解度已通过等温饱和法在25°C的安瓿瓶中测定。溶解度已使用Geochemist的Workbench(GMB 7.0)软件包进行了计算。测得的赤铁矿和菱锰矿的溶解度分别为10〜(-35.76)和10〜(36.43)。使用GMB 7.0软件包计算并绘制Eh-pH图。该数据库包含46个元素,47个主要粒子,48个氧化还原对,溶液中的552个粒子,624个固相和10种气体的热力学参数。绘制了Ni-As-H2O和Co-As-H2O系统的Eh-pH图,以了解这些元素在硫化物沉积氧化区中酸性水中的平均含量。讨论了近地表条件下赤铁矿和菱锰矿的形成。

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