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Journal Article

The fate of iron during soil formation in humid-temperate environments

Iron in soils and clay minerals (1988) 749-777
DOI: 10.1007/978-94-009-4007-9_21
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Abstract

Soil color is determined mainly by organic matter and Fe compounds. Therefore, many soil forming processes can be reconstructed by analyzing the kind and form of Fe compounds in the different horizons of a soil and in different soils of a landscape. -from Author

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Blume, H. P. (1988). The fate of iron during soil formation in humid-temperate environments. Iron in Soils and Clay Minerals, 749–777. https://doi.org/10.1007/978-94-009-4007-9_21

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