The characterization of soils, clays, and clay firing products

被引：36

作者：

Murad, E ^{[1
]}

机构：

[1] Bayer Geol Landesamt, D-96049 Bamberg, Germany

来源：

HYPERFINE INTERACTIONS | 1998年 / 111卷 / 1-4期

关键词：

D O I：

10.1023/A:1012649532742

中图分类号：

O64 [物理化学（理论化学）、化学物理学]; O56 [分子物理学、原子物理学];

学科分类号：

070203 ; 070304 ; 081704 ; 1406 ;

摘要：

Mossbauer spectroscopic studies of soils are generally centered around the characterization of Fe3+ oxides, making use of distinctive magnetic properties of the different oxides and the high sensitivity of the technique for magnetically ordered phases. Most work on clays and clay minerals, in contrast, focuses on the determination of the oxidation state of iron, iron structural site occupancies and distortions, and the transformations that take place during clay firing.

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页码：251 / 259

页数：9

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