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Crystal structures of laihunite and intermediate phases between laihunite-1M and fayalite: Z-contrast imaging and ab initio study
Huifang Xu;  Zhizhang Shen;   Hiromi Konishi;  Pingqiu Fu;  Izabela Szlufarska
2014
Source PublicationAmerican Mineralogist
Volume99Issue:5-6Pages:881-889
Abstract

Crystals of laihunite from Xiaolaihe of Liaoning Province, northeast China, were studied using selected-area electron diffraction (SAED), high-resolution transmission electron microscopy (HRTEM), and Z-contrast imaging. Z-contrast images directly reveal ordered vacancies in M1 sites. The results confirm early structural models for 1-layer laihunite (or laihunite-1M) with ideal stoichiometry of □0.5Fe2+0.5Fe 3+SiO4. 2-layer laihunite and 3-layer laihunite are found to be chemically different from laihunite-1M. The 2-layer laihunite can be viewed as a periodic intergrowth of laihunite and fayalite in the 1:1 ratio. The 3-layer laihunite can be considered to be a periodic intergrowth of laihunite and fayalite in the 1:0.5 ratio along the c-axis. Ideal stoichiometries for the 2-layer structure and the 3-layer structure are □0.5Fe 2+2.5Fe3+[SiO4]2 and □1.0Fe2+3.0Fe3+ 2.0[SiO4]3, respectively. The structural intergrowth of the 3-layer laihunite and the 1-layer lahunite results in chemical compositions falling within the range between the two aforementioned structures, such as the chemical formula of □0.4Fe 2+0.8Fe3+0.8SiO4, reported earlier in the literature. The crystal structures of the 1-layer laihunite (1M), the 2-layer laihunite (2M), and the 3-layer laihunite (3Or) determined from Z-contrast images and ab initio calculations using the density functional theory (DFT) have space groups of P21/b, P21/b, and Pbnm, respectively. The previously reported monoclinic symmetry for the 3-layer laihunite may be an artifact due to overlapping diffraction spots from both, the laihunite-3Or and the laihunite-1M. Our study demonstrates that the method of combining Z-contrast imaging and ab initio calculation can be effectively used for identifying structures of nano-phases in host crystals. Perhaps more importantly, Z-contrast imaging provides a powerful means for direct observation of vacancies and other defects, and may be utilized to map vacancies in Fe3+-bearing olivines, the alignments of which can greatly affect anisotropic diffusion in such structures.

KeywordLaihunite vacancy Ordering z-contrast Imaging dft hrtem superstructure olivine oxidation
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/11172
Collection矿床地球化学国家重点实验室
Affiliation1.NASA Astrobiology Institute, Department of Geoscience, University of Wisconsin-Madison, Madison, WI 53706, United States
2.Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550002, China
3.Department of Materials Science and Engineering, University of Wisconsin-Madison, Madison, WI 53706, United States 摘要
Recommended Citation
GB/T 7714
Huifang Xu;Zhizhang Shen; Hiromi Konishi;Pingqiu Fu;Izabela Szlufarska. Crystal structures of laihunite and intermediate phases between laihunite-1M and fayalite: Z-contrast imaging and ab initio study[J]. American Mineralogist,2014,99(5-6):881-889.
APA Huifang Xu;Zhizhang Shen; Hiromi Konishi;Pingqiu Fu;Izabela Szlufarska.(2014).Crystal structures of laihunite and intermediate phases between laihunite-1M and fayalite: Z-contrast imaging and ab initio study.American Mineralogist,99(5-6),881-889.
MLA Huifang Xu;Zhizhang Shen; Hiromi Konishi;Pingqiu Fu;Izabela Szlufarska."Crystal structures of laihunite and intermediate phases between laihunite-1M and fayalite: Z-contrast imaging and ab initio study".American Mineralogist 99.5-6(2014):881-889.
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