Speciation of AsIII and AsV in hydrothermal fluids by in situ X-ray absorption spectroscopy

被引:18
作者
Testemale, Denis [1 ,2 ]
Pokrovski, Gleb S. [3 ]
Hazemann, Jean-Louis [1 ,2 ]
机构
[1] Inst Neel, Dept MCMF, F-38042 Grenoble, France
[2] FAME Beamline ESRF, F-38043 Grenoble, France
[3] Univ Toulouse 3, GET, CNRS, UMR 5563, F-31400 Toulouse, France
关键词
arsenic speciation; hydrothermal fluid; X-ray absorption spectroscopy; XANES ab initio calculations; high-pressure cell; THERMODYNAMIC PROPERTIES; ARSENIC SPECIATION; AQUEOUS-SOLUTIONS; HIGH-TEMPERATURE; FINE-STRUCTURE; HYDROXIDE COMPLEXES; CRUSTAL FLUIDS; DEGREES-C; WATER; SOLUBILITY;
D O I
10.1127/0935-1221/2011/0023-2104
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The speciation of arsenic (III) and (V) in aqueous acidic and basic solutions at ambient conditions, and of arsenic (V) in acidic solutions at 270 bars from 30 to 300 degrees C was investigated using in situ X-Ray Absorption Spectroscopy (XAS). Both Extended X-Ray Absorption Fine Structure (EXAFS) analysis and X-Ray Absorption Near Edge Structure (XANES) ab initio calculations were used to determine the structure of dominant arsenic species in solution. At ambient conditions, the deprotonation of As-III(OH)(3) and (AsO)-O-V(OH)(3) species with increasing pH is demonstrated by analysis of their XANES signals, in agreement with available arsenious and arsenic acid dissociation constants. In basic conditions, the dominant species is a deprotonated form of the As(OH)(3) acid, with a very similar symmetry. The speciation of As-V in acidic hydrothermal fluids is dominated by the (AsO)-O-V(OH)(3) complex over a wide temperature and pressure range, to at least 300 degrees C and 300 bars. The first-shell As structure in the (AsO)-O-V(OH)(3) species and its deprotonated forms is found to be a distorted tetrahedron, similar to the base AsO4 unit of Na2HAsO4 center dot 7H(2)O(s). This work demonstrates new capabilities of XAS coupled with molecular modelling to decipher deprotonation reactions that affect mineral solubilities and chemical elements mobility in aqueous crustal fluids.
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页码:379 / 390
页数:12
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