The role of sulfur in palladium transport and fractionation from platinum by hydrothermal fluids

IF 5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
C. Laskar , E.F. Bazarkina , G.S. Pokrovski
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引用次数: 0

Abstract

The solubility of palladium sulfide (PdS(s)) has been measured in H2S/HS aqueous solutions across wide ranges of sulfur concentrations (0.5–1.2 molal) and pH (5–8) at temperatures from 50 to 300 °C and pressures from 90 to 600 bar, using a hydrothermal flexible-cell reactor allowing controlled fluid injection and sampling. Combined with thermodynamic modeling and analysis of available literature data, our results demonstrate that palladium tetrahydrosulfide, PdII(HS)42–, is the dominant complex in sulfide-rich moderate-temperature hydrothermal fluids. The equilibrium constants of PdS(s) dissolution reaction, PdS(s) + 3 H2S0(aq) = Pd(HS)42– + 2H+ (Ks4,Pd), generated in this study can be described by the function log10Ks4,Pd = (196.4 ± 60.0) – (11384 ± 3567)/T(K) – (71.24 ± 19.52) × log10T(K), valid over the temperature range 25–300 °C and from saturated vapor pressure to 600 bar. Our results, combined with recent analogous PtS(s) solubility data, enabled the derivation of a self-consistent set of thermodynamic properties of Pd(HS)42– and Pt(HS)42– in the framework of the HKF model. Solubility predictions of PdS(s) using these properties yield maximum solubility values of 1 ppb Pd, as the tetrahydrosulfide complex, in H2S-bearing hydrothermal fluids (>0.01 m S) at moderate temperatures (50–350 °C) and near-neutral pH (6–7), whereas chloride complexes are predominant at acidic pH (<4). The Pd/Pt atomic ratio in typical H2S-bearing hydrothermal fluids at 300 °C in equilibrium with PdS(s) and PtS(s) varies from > 104 at pH < 2 to 10–2 at pH > 3, corresponding to the change from chloride- to sulfide-dominated speciation for both metals. However, the absolute solubilities of both chloride and sulfide complexes are too small over the whole pH range to significantly contribute to Pd vs. Pt fractionations observed in hydrothermal environments. Among different factors that may lead to such fractionations, the role of polysulfide sulfur species, including trisulfur radical ions, should be considered in future studies.
硫在热液中钯输运和铂分馏中的作用
在硫浓度(0.5-1.2摩尔)和pH值(5-8)范围内的H2S/HS水溶液中,使用热液柔性电池反应器,在温度为50至300℃,压力为90至600 bar的条件下,测量了硫化钯(PdS(s))的溶解度。结合热力学模型和现有文献数据分析,我们的研究结果表明,四氢硫化钯PdII(HS)42 -是富硫化物的中温热液中的主导配合物。本研究生成的PdS(s)溶解反应的平衡常数PdS(s) + 3 H2S0(aq) = Pd(HS)42 - + 2H+ (Ks4,Pd)可以用函数log10Ks4表示,Pd =(196.4±60.0)-(11384±3567)/T(K) -(71.24±19.52)× log10T(K),其有效温度范围为25 ~ 300℃,饱和蒸汽压至600 bar。我们的研究结果,结合最近类似的Pt(s)溶解度数据,使Pd(HS)42 -和Pt(HS)42 -在HKF模型的框架内推导出一组自一致的热力学性质。利用这些性质对PdS进行溶解度预测,在含h2s的热液(0.01 m s)中,在中等温度(50-350°C)和接近中性的pH值(6-7)下,四氢硫化物络合物的最大溶解度值为1 ppb Pd,而氯化物络合物在酸性pH值(<4)下占主导地位。300℃时,典型含硫化氢热液中Pd/Pt原子比在PdS(s)和PtS(s)平衡时的变化范围为>;pH <时104;2至10-2在pH >;3、对应于两种金属从氯化物为主到硫化物为主的形态变化。然而,在整个pH范围内,氯化物和硫化物配合物的绝对溶解度都太小,无法显著影响在热液环境中观察到的Pd和Pt分馏。在可能导致这种分馏的不同因素中,包括三硫自由基离子在内的多硫硫物种的作用应在未来的研究中加以考虑。
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来源期刊
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta 地学-地球化学与地球物理
CiteScore
9.60
自引率
14.00%
发文量
437
审稿时长
6 months
期刊介绍: Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes: 1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids 2). Igneous and metamorphic petrology 3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth 4). Organic geochemistry 5). Isotope geochemistry 6). Meteoritics and meteorite impacts 7). Lunar science; and 8). Planetary geochemistry.
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