Structural model for the biogenic Mn oxide produced by Pseudomonas putida

双锰矿 扩展X射线吸收精细结构 材料科学 结晶学 八面体 氧化物 微晶 吸收光谱法 无机化学 化学 晶体结构 量子力学 物理 冶金 氧化锰
作者
Mario Villalobos,Bruno Lanson,Alain Manceau,Brandy M. Toner,Garrison Sposito
出处
期刊:American Mineralogist [Mineralogical Society of America]
卷期号:91 (4): 489-502 被引量:295
标识
DOI:10.2138/am.2006.1925
摘要

X-ray diffraction (XRD) and Mn K-edge extended X-ray absorption fine structure (EXAFS) spectroscopy were combined to elaborate a structural model for phyllomanganates (layer-type Mn oxides) lacking 3D ordering (turbostratic stacking). These techniques were applied to a sample produced by a common soil and freshwater bacterium (Pseudomonas putida), and to two synthetic analogs, δ-MnO2 and acid birnessite, obtained by the reduction of potassium permanganate with MnCl2 and HCl, respectively. To interpret the diffraction and spectroscopic data, we applied an XRD simulation technique utilized previously for well-crystallized birnessite varieties, complementing this approach with single-scattering-path simulations of the Mn K-edge EXAFS spectra. Our structural analyses revealed that all three Mn oxides have an hexagonal layer symmetry with layers comprising edgesharing Mn4+O6 octahedra and cation vacancies, but no layer Mn3+O6 octahedra. The proportion of cation vacancies in the layers ranged from 6 to 17%, these vacancies being charge-compensated in the interlayer by protons, alkali metals, and Mn atoms, in amounts that vary with the phyllomanganate species and synthesis medium. Both vacancies and interlayer Mn were most abundant in the biogenic oxide. The diffracting crystallites contained three to six randomly stacked layers and have coherent scattering domains of 19.42 Å in the c* direction, and of 60.85 Å in the a-b plane. Thus, the Mn oxides investigated here are nanoparticles that bear significant permanent structural charge resulting from cation layer vacancies and variable surface charge from unsaturated O atoms at layer edges.
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