The role of Pb(II) complexes in hydrothermal mass transfer: An X-ray absorption spectroscopic study

被引:29
作者
Etschmann, Barbara E. [1 ]
Mei, Yuan [1 ,2 ]
Liu, Weihua [2 ]
Sherman, Dave [3 ]
Testemale, Denis [4 ]
Muller, Harald [5 ]
Rae, Nicholas [6 ]
Kappen, Peter [6 ]
Brugger, Joel [1 ,7 ]
机构
[1] Monash Univ, Sch Earth Atmosphere & Environm, Clayton, Vic 3800, Australia
[2] CSIRO Mineral Resources, Clayton, Vic 3168, Australia
[3] Univ Bristol, Sch Earth Sci, Bristol BS8 1RJ, Avon, England
[4] Inst Neel, 25 Ave Martyrs Batiment,BP 166, F-38042 Grenoble 9, France
[5] European Synchrotron Res Facil, 6 Rue Jules Horowitz, F-38043 Grenoble, France
[6] Australian Synchrotron, Clayton, Vic 3148, Australia
[7] Australian Res Council, Australian Copper Uranium Transformat Res Hub, Canberra, ACT, Australia
基金
澳大利亚研究理事会;
关键词
Lead; Coordination chemistry; XAS spectroscopy; Chloride complexing; Bisulfide complexing; Molecular dynamics simulations; MOLECULAR-DYNAMICS SIMULATIONS; LEAD(II) CHLORIDE COMPLEXES; AQUEOUS METAL-COMPLEXES; AB-INITIO; THERMODYNAMIC PROPERTIES; FORMATION-CONSTANTS; FLUIDS INSIGHTS; SYSTEM H2O-NACL; DEGREES-C; SPECIATION;
D O I
10.1016/j.chemgeo.2018.10.022
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We studied the nature and geometry of Pb(II) complexes in chloride-, bromide-, and bisulfide-bearing solutions in situ at pressures of 600 and 800 bar and temperatures up to 489 degrees C using in situ XAS spectroscopy combined with ab initio molecular dynamics (MD) simulations. In halide-free acidic solutions, Pb(II) complexes to approximately seven water ligands (predominantly Pb(H2O)(7)](2+)) at 30 degrees C; this hydration number reduces to approximately six ligands at 191 degrees C. Due to the influence of a stereochemically active electron lone pair, Pb(II) halide complexes are characterised by a broad bond distance distribution, highly flexible structures, and a distinct gap for excess electron density. Residual maps (based on R-factor) of parameter space confirmed that many possible parameter combinations resulted in equally satisfactory fits of the EXAFS data. Thus, EXAFS interpretation was constrained using MD simulations and results of experimental speciation and solubility studies available in the literature. The results indicate that in chloride-bearing solutions, at T > 200 degrees C, Pb(II) has a maximum coordination of four to five ligands, and the Pb-complex is always coordinated to a combination of water and chloride; even at 400 <= T <= 500 degrees C in an acidified solution containing similar to 10 m Cl-, the predominant Pb(II) complex is [Pb(H2O)(1-2)Cl-3](-) . The highest order bromide complex similarly contains three halide ligands ([Pb(H2O)(0)Br-.5(3)](-) in a similar to 4 m Br- acidified solution above 400 degrees C), but the hydration number is lower than in the case of chloride. With regard to bisulfide complexing, the solubility of galena in the presence of bisulfide was lower than expected from extrapolations using available low temperature solubility data, but the formation of Pb (II) bisulfide complexes was confirmed by the increase in solubility with increase in bisulfide concentration. The new data show that in terms of coordination geometry, Pb(II) behaves like semi-metals such as Sb(III), As (III), Bi(III), or Te(IV), which are affected by a stereochemically active lone pair, rather than like divalent first row transition metals such as Zn. Pb(II)-chloride complexes with a maximum of three chloride ligands are the dominant complexes responsible for Pb transport. In contrast, Zn(II) forms tetrahedral chloride complexes, and ZnCl42- is stable in brines up to temperatures >= 300 degrees C. These differences in coordination chemistry, combined with the differences in solubilities of Zn and Pb minerals, account for Zn/Pb fractionation in hydrothermal fluids.
引用
收藏
页码:88 / 106
页数:19
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