The mid-infrared spectrum of a new double carbonate, BaFe[CO3]2

被引:6
|
作者
Boettcher, Michael Ernst [1 ,2 ,3 ]
Gehlken, Peer-Lennart [4 ]
Liang, Wen [5 ,6 ]
机构
[1] Leibniz Inst Baltic Sea Res IOW, Geochem & Isotope Biogeochem, D-18119 Warnemunde, Germany
[2] Univ Greifswald, Marine Geochem, D-17489 Greifswald, Germany
[3] Univ Rostock, Interdisciplinary Fac, Dept Maritime Syst, D-18059 Rostock, Germany
[4] Testing Raw & Residual Mineral Mat, Muhlengasse 1, D-37136 Ebergotzen, Germany
[5] Guizhou Minzu Univ, Coll Mat Sci & Engn, Guiyang 550025, Peoples R China
[6] Chinese Acad Sci, Inst Geochem, Guiyang 550081, Peoples R China
基金
美国国家科学基金会;
关键词
Barium iron carbonate; BaFe[CO3](2); Double carbonate; Infrared spectroscopy; Transmission; Attenuated total reflectance; Norsethite; Dolomite; SOLID-SOLUTIONS; ISOTOPE FRACTIONATION; VIBRATIONAL-SPECTRA; CRYSTAL-STRUCTURE; X-RAY; NORSETHITE; DOLOMITE; BAMN(CO3)(2); BAMG(CO3)2; WITHERITE;
D O I
10.1016/j.molstruc.2021.131899
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
BaFe[CO3](2), a new double carbonate from the norsethite-type family of carbonates, was recently discovered and synthesized at high-pressure-temperature (high-PT) conditions. Two polymorphs of the new double carbonate were identified belonging to the R (3) over barm and R (3) over barc space groups, respectively(1). In the present communication we present for the first time the mid-infrared (IR) spectra (measured with transmission infrared spectroscopy and attenuated total reflectance infrared spectroscopy) and assign the observed bands to the respective fundamental and combined IR-active modes. This study, therefore, adds new spectroscopic results to the previous crystal chemical characterization of the new double carbonate. Results are compared to those of other Ba-bearing double carbonates with the norsethite-type structures. With substitution of Ba2+ in the double carbonate lattice by increasingly smaller cations a decrease in wavenumbers of absorption bands is observed. Due to similar crystal structures, and masses and radii of the cations, the IR spectra of both BaFe[CO3](2) carbonates are similar to the ones observed for BaMn[CO3](2) and BaMg[CO3](2), with some characteristic deviations. The carbon isotope shift coefficient of 0.969 for upsilon(2) of the carbonate ion group agrees with previous theoretical predictions. (C) 2021 Elsevier B.V. All rights reserved.
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页数:5
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