Structural and 57Fe Mössbauer spectroscopic characterization of the synthetic NaFeSi2O6 (aegirine) – CaMgSi2O6 (diopside) solid solution series
Structural and 57Fe Mössbauer spectroscopic characterization of the synthetic NaFeSi2O6 (aegirine) – CaMgSi2O6 (diopside) solid solution series
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合成 NaFeSi2O6(aegirine)-CaMgSi2O6(透辉石)固溶体系列的结构和 57Fe 穆斯堡尔光谱表征
DOI:
10.1524/zkri.2012.1514
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发表时间:
2012
期刊:
影响因子:
--
通讯作者:
G. Roth
中科院分区:
文献类型:
--
作者:
G. Redhammer;G. Tippelt;G. Amthauer;G. Roth
Abstract Clinopyroxenes along the aegrine – diopside join have been synthesized from flux growth and high pressure experiments. Samples were characterized by 57Fe Mössbauer spectroscopy and single crystal X-ray diffraction. Coordination, bond lenghts and – angles and polyhedral distortion parameters are discussed as a function of composition. All samples exhibit C2/c space group symmetry and show smooth variation of structural parameters with chemistry. While the lattice parameters a and b increase with increasing diopside component, c decreases, even if the smaller Fe3+ cation is replaced by the larger Mg2+ one. A distinctly decreasing M1—M1 cationic distance within the octahedral chain from aegirine to diopside suggests, that decreasing repulsive forces between M1 catäions with decreasing charge of the M1 cation is responsible for this behaviour. In 57Fe Mössbauer spectroscopy, small amount of Fe2+ were detected in the samples of the high pressure experiments. The quadrupole splitting of both, Fe2+ and Fe3+ suggests an increasing distortion of the Fe-octahedra with increasing diopside content, while the overall distortion of the M1 sites decrease. This shows that local structural units may behave quite differently as compared to the average structure.