Fourier-transform infrared spectroscopy (FTIR) analysis of triclinic and hexagonal birnessites

被引:45
|
作者
Ling, Florence T. [1 ]
Post, Jeffrey E. [2 ]
Heaney, Peter J. [1 ]
Kubicki, James D. [3 ]
Santelli, Cara M. [4 ]
机构
[1] Penn State Univ, Dept Geosci, University Pk, PA 16802 USA
[2] Smithsonian Inst, Dept Mineral Sci, NHB 119, Washington, DC 20013 USA
[3] Univ Texas El Paso, Dept Geol Sci, El Paso, TX 79968 USA
[4] Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA
关键词
Birnessite; Manganese oxide; FTIR; EXAFS; Density functional theory; BIOGENIC MN-OXIDES; MANGANESE OXIDE; POWDER DIFFRACTION; RIETVELD REFINEMENT; PSEUDOMONAS-PUTIDA; IR-SPECTRA; OXIDATION; MINERALS; TODOROKITE; DENSITY;
D O I
10.1016/j.saa.2017.01.032
中图分类号
O433 [光谱学];
学科分类号
0703 ; 070302 ;
摘要
The characterization of birnessite structures is particularly challenging for poorly crystalline materials of biogenic origin, and a determination of the relative concentrations of triclinic and hexagonal birnessite in a mixed assemblage has typically required synchrotron-based spectroscopy and diffraction approaches. In this study, Fourier transform infrared spectroscopy (FTIR) is demonstrated to be capable of differentiating synthetic triclinic Nabirnessite and synthetic hexagonal H-birnessite. Furthermore, IR spectral deconvolution of peaks resulting from Mn O lattice vibrations between 400 and 750 cm(-1) yield results comparable to those obtained by linear combination fitting of synchrotron X-ray absorption fine structure (EXAFS) data when applied to known mixtures of triclinic and hexagonal birnessites. Density functional theory (DFT) calculations suggest that an infrared absorbance peak at-1628 cm(-1) may be related to OH vibrations near vacancy sites. The integrated intensity of this peak may show sensitivity to vacancy concentrations in the Mn octahedral sheet for different birnessites. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:32 / 46
页数:15
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