作者: F. R. Zaidelman , A. S. Nikiforova
DOI: 10.1080/03650349709366007
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摘要: An attempt is made to formulate general regularities of changes in the amount and composition Mn‐Fe conoretions soils humid landscapes, confined various soil‐forming rocks within Russian platform. It concluded, that intensive formation concretions highly conditioned by waterlogging degree their hydrological regime. The content always maximum gley‐like (seldom gley ones), independing on genesis parent rocks; fraction distribution proves be stable time; Mn declined with increasing waterloggiing soils, while Fe becomes increased; highest accumulation such microelements as Co, Pb, Cd observed concretions, which are rich Mn. characterized a high X‐ray‐amorphous well low magnetic susceptibility. chemical shown preferable for quantitative diagnosis water‐logging...