Determination of mean crystallite dimensions from X-ray diffraction peak profiles: A comparative analysis of synthetic hematites

被引:43
作者
Crosa, R
Boero, V
Franchini-Angela, M
机构
[1] Univ Turin, Dipartimento Valorizzaz & Protez Risorse Agrofore, I-10095 Turin, Italy
[2] Univ Turin, Dipartimento Sci Mineral & Petrolog, I-10125 Turin, Italy
关键词
BET; hematite; iron oxides; mean crystallite dimension; powder X-ray diffraction; surface area; XRD;
D O I
10.1346/CCMN.1999.0470608
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 [物理化学]; 081704 [应用化学];
摘要
X-ray diffraction (XRD) profile analysis of eight synthetic hematite samples was performed to identify the best parameters for determining the apparent mean crystallite dimension (D) and, consequently, surface area. The samples are comparable to soil hematite with respect to crystallinity. The procedure included: a) deconvolution of the XRD peaks to Gauss and Cauchy components and subtraction of the instrumental profile, b) determination of D from full-width at half-maximum, integral breadth, and integral breadth measurements of the Cauchy component, and c) comparison of deduced surface areas with those obtained by the N-2-BET adsorption method. As expected, D values are strongly influenced by the broadening parameters. An appropriate selection of peaks is required to obtain size values along the crystallographic axes a (hkl: 110, 300) and c (hkl: 104, 116) and to calculate reliable surface areas. Using the Cauchy component of the above peaks, the calculated surface areas compared well with those measured by the N-2-BET adsorption method.
引用
收藏
页码:742 / 747
页数:6
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