Application of Clay Crystallite-Size in Soil Genesis Studies

Citation data:

Proceedings of the Iowa Academy of Science, Vol: 74, Issue: 1, Page: 122-129

Publication Year:
1967
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Repository URL:
https://scholarworks.uni.edu/pias/vol74/iss1/22
Author(s):
Arnold, R. W.
artifact description
Many soils have clay-enriched horizons that are thought to result from pedogenic processes. Various hypotheses are proposed for expected clay size-distributions in soil profiles. The average size of clay crystallites determined by the amount of broadening of x-ray diffraction peaks ranged from 160 to >2000Aº , but the lack of trends in four loess-derived soils did not permit the hypotheses to be evaluated. An unexpected relationship in a well expressed illuvial horizon was noted: as the percent of accumulated clay increased to the observed maximum the average crystallite size also increased rather than decreased as proposed. This suggests that small-sized illuvial clay particles undergo reorganization to form larger stable crystallites. Knowledge of clay crystallite size is expected to supplement other data in interpreting soil genesis.