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Journal Article

Occurrence and formation of iron oxides in various pedoenvironments

Iron in soils and clay minerals (1988) 267-308
DOI: 10.1007/978-94-009-4007-9_11
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Abstract

Many soil colors, notably those between red, brown, and yellow, are due to solid Fe oxides. Pedogenesis can be understood better if the reactions of Fe in soils are sufficiently well known. -from Author

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APA

Schwertmann, U. (1988). Occurrence and formation of iron oxides in various pedoenvironments. Iron in Soils and Clay Minerals, 267–308. https://doi.org/10.1007/978-94-009-4007-9_11

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