Response of Vertisols, Andosols, and Alisols to paddy management
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文摘

Changes in the proportion of short range-ordered Fe oxides depend on soil texture.

No accumulation of Fe oxides in subsoils

Organic matter (OM) input rather than storage capacity limits OM accumulation.

No evidence for ferrolysis in paddy soils

Characteristics of initial soil types were mainly preserved during paddy soil evolution.

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