Coupled Solubility of Cu and Ag in Chloride-Bearing Hydrothermal Fluids (350-650°C, 1000-1500 bar)

被引:2
作者
Rubtsova, E. A. [1 ]
Tagirov, B. R. [1 ]
Akinfiev, N. N. [1 ]
Reukov, V. L. [1 ]
Koroleva, L. A. [1 ]
Nikolaeva, I. Yu. [2 ]
Tarnopolskaya, M. E. [2 ]
Volchenkova, V. A. [3 ]
机构
[1] Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow 119017, Russia
[2] Moscow MV Lomonosov State Univ, Dept Geol, Moscow 119991, Russia
[3] Russian Acad Sci, Baikov Inst Met & Mat Sci, Moscow 119334, Russia
基金
俄罗斯科学基金会;
关键词
copper; silver; solubility; hydrothermal fluids; experiment; chloride complexes; RAY-ABSORPTION SPECTROSCOPY; THERMODYNAMIC PROPERTIES; WIDE-RANGE; COMPLEXES; TEMPERATURE; TRANSPORT; SILVER; WATER; COPPER(I)-CHLORIDE; 0-DEGREES-C;
D O I
10.1134/S1075701523010075
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The coupled solubility of Cu-(cr) and Ag-(cr) was measured in acidic chloride solutions at 350 degrees C/1000 bar, 450 degrees C/1000 bar, and 653 degrees C/1450 bar in a wide range of chloride concentrations (0.02m HCl + (0-15m) NaCl). The experiments were performed using the autoclave (350, 450 degrees C) and ampoule (653 degrees C) techniques, the dissolved metal concentrations were measured after quenching the experimental system. The equilibrium constants of the reaction combining the dominant forms of transport of the metals are determined: Cu-(cr) + AgCl2- = Ag-(cr) + CuCl2- K(Cu-Ag)degrees. The calculated reaction constant is independent of chloride concentration. It is known that AgCl2- dominates in the studied chloride concentration range. Therefore, the main copper form of occurrence is CuCl2- in all experimental fluids with chloride content up to 47 wt %, which is close to the NaCl saturation limit. The constant of the coupled Cu and Ag solubility was determined for the experimental PT parameters as log K(Cu-Ag)degrees = 2.65 +/- 0.20 (350 degrees C/1000 bar), 2.28 +/- 0.10 (450 degrees C/1000 bar), and 1.49 +/- 0.34 (653 degrees C/1450 bar). These data, together with values from the literature for temperatures from 200 to 900 degrees C and pressure up to 2000 bar, were fitted to the density model equation: log K(Cu-Ag)degrees = 1.066 + 1.108 x 10(3)T(K)(-1) + 3.585 logd(w) - 1.443logd(w) x 10(3) T(K)(-1), where d(w) is the pure water density. According to these data, copper is much more soluble in chloride solutions compared to silver, but the difference in the solubility decreases with the increase in temperature. Reliable literature data on the silver solubility constant allow that of copper solubility to be calculated: Cu-(cr) + HCl(aq) + Cl- =CuCl2- = 0.5H(2(aq)) K-(Cu)degrees, log K-(Cu)degrees = 1.39 +/- 0.20 (350 degrees C, 1000 bar), 1.91 +/- 0.10 (450 degrees C, 1000 bar), and 2.06 +/- 0.34 (653 degrees C, 1450 bar). The new values of K-(Cu)degrees are combined with reliable literature data to calculate the density-model parameters. The obtained density-model equation can be used to calculate the copper solubility constant up to 800 degrees C and pressures up to 2000 bar: log K-(Cu)degrees = 6.889 - 3.298 x 10(3)T(K)(-1) + 8.694logd(w) - 4.807logd(w) x 10(3)T(K)(-1). The solubility of chalcopyrite in the system with pyrite-hematite-magnetite and K-feldspar-muscovite-quartz mineral buffer assemblages is discussed.
引用
收藏
页码:11 / 27
页数:17
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