鳞片岩
赤铁矿
针铁矿
正交晶系
材料科学
结构精修
矿物学
结晶学
化学
晶体结构
物理化学
吸附
出处
期刊:Clay Minerals
[Cambridge University Press]
日期:2002-12-01
卷期号:37 (4): 629-638
被引量:14
标识
DOI:10.1180/0009855023740065
摘要
Abstract X-ray powder diffraction patterns were simulated for nano-sized hematite, goethite and lepidocrocite by three-dimensional integration in reciprocal space. The cell-edge lengths were refined together with the size parameters X and X e of the Thompson-Cox-Hastings function, which for orthorhombic structures was extended by a biaxial broadening parameter X o . Variations of the structure factors across broad peaks resulted in apparent peak shifts and concomitant shifts in celledge lengths, which were significantly correlated with the size parameters for hematite and partially correlated for goethite and lepidocrocite. Regression equations are given for correcting cell-edge lengths obtained from Rietveld fits for size-induced shifts.
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