EXPERIMENTAL AND THEORETICAL VIBRATIONAL SPECTROSCOPIC EVALUATION OF ARSENATE COORDINATION IN AQUEOUS SOLUTIONS, SOLIDS, AND AT MINERAL-WATER INTERFACES - REEVALUATION OF EXAFS RESULTS AND TOPOLOGICAL FACTORS IN PREDICTING GEOMETRY AND EVIDENCE FOR MONODENTATE COMPLEXES

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dc.contributor.author Myneni S.C.B.
dc.contributor.author Traina S.J.
dc.contributor.author Waychunas G.A.
dc.contributor.author Logan T.J.
dc.date.accessioned 2020-12-30T02:36:36Z
dc.date.available 2020-12-30T02:36:36Z
dc.date.issued 1998
dc.identifier https://elibrary.ru/item.asp?id=121630
dc.identifier.citation Geochimica et Cosmochimica Acta, 1998, , 19, 3285-3300
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/21685
dc.description.abstract Arsenate (AsO43-) is a common species in oxidizing aquatic systems and hydrothermal fluids, and its solubility and partitioning into different mineral phases are determined by the nature of AsO43- coordination, solution pH, type of soluble cations, and H2O structure at the mineral-fluid interfaces. While the vibrational spectroscopy has been widely used in examining the AsO43- coordination chemistry, insufficient knowledge on the correlation of AsO43- molecular structure and its vibrational spectra impeded the complete spectral interpretation. In this paper, we evaluated the vibrational spectroscopy of AsO43- in solutions, crystals, and sorbed on mineral surfaces using theoretical (semiempirical, for aqueous species) and experimental studies, with emphasis on the protonation, hydration, and metal complexation influence on the As-O symmetric stretching vibrations. Theoretical predictions are in excellent agreement with the experimental studies and helped in the evaluation of vibrational modes of several arsenate-complexes and in the interpretation of experimental spectra. These vibrational spectroscopic studies (IR, Raman) suggest that the symmetry of AsO43- polyhedron is strongly distorted, and its As-O vibrations are affected by protonation and the relative influence on AsO43- structure decreases in the order: H+ # cation =< H2O. For all AsO43- complexes, the As-OX symmetric stretching (X = metal, H+, H2O; =<820 cm-1) shifted to lower wavenumbers when compared to that of uncomplexed AsO43-. In addition, the As-OH symmetric stretching of protonated arsenates in aqueous solutions shift to higher energies with increasing protonation (<720, <770, <790 cm-1 for HAsO42-, H2AsO4-, and H3AsO40, respectively). The protonated arsenates in crystalline solids show the same trend with little variation in As-OH symmetric stretching vibrations. Since metal complexation of protonated AsO43- does not influence the As-OH vibrations significantly, deducing symmetry information from their vibrational spectra is difficult. However, for metal unprotonated-AsO43- complexes, the shifts in As-OM (M = metal) vibrations are influenced only by the nature of complexing cation and the type of coordination, and hence the AsO43- coordination environment can be interpreted directly from the splitting of As-O degenerate vibrations and relative shifts in the As-OM modes. This information is critical in evaluating the structure of AsO43- sorption complexes at the solid-water interfaces. The vibrational spectra of other tetrahedral oxoanions are expected to be along similar lines.
dc.title EXPERIMENTAL AND THEORETICAL VIBRATIONAL SPECTROSCOPIC EVALUATION OF ARSENATE COORDINATION IN AQUEOUS SOLUTIONS, SOLIDS, AND AT MINERAL-WATER INTERFACES - REEVALUATION OF EXAFS RESULTS AND TOPOLOGICAL FACTORS IN PREDICTING GEOMETRY AND EVIDENCE FOR MONODENTATE COMPLEXES
dc.type Статья


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