铁酸盐
结晶学
扩展X射线吸收精细结构
赤铁矿
材料科学
直线(几何图形)
衍射
八面体
光谱学
散射
化学
晶体结构
物理
矿物学
吸收光谱法
数学
几何学
光学
有机化学
吸附
量子力学
作者
V. A. Drits,B. A. Sakharov,A. L. Salyn,A. Manceau
出处
期刊:Clay Minerals
[Cambridge University Press]
日期:1993-06-01
卷期号:28 (2): 185-207
被引量:343
标识
DOI:10.1180/claymin.1993.028.2.02
摘要
Abstract The structure of 6-line and 2-line ferrihydrite (Fh) has been reconsidered. X-ray diffraction (XRD) curves were first simulated for the different structural models so far proposed, and it is shown that neither of these corresponds to the actual structure of ferrihydrite. On the basis of agreement between experimental and simulated XRD curves it is shown that Fh is a mixture of three components: (i) Defect-free Fh consisting of anionic ABACA . . . close packing in which Fe atoms occupy only octahedral sites with 50% probability; the hexagonal unit-cell parameters are a = 2-96 Å and c = 9-40 Å, and the space group is P 1c. (ii) Defective Fh in which Ac 1 Bc 2 A and Ab 1 Cb 2 A structural fragments occur with equal probability and alternate completely at random; Fe atoms within each of these fragments have identical ordered distribution with in the hexagonal super-cell with a = 5.26 Å. (iii) Ultradispersed hematite with mean dimension of coherent scattering domains (CSD) of 10-20 Å. The main structural difference between 6-line and 2-line Fh is the size of their CSD which is extremely small for the latter structure. Nearest Fe-Fe distances calculated for this new structural model are very close to those determined by EXAFS spectroscopy on the same samples.
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