Ferrihydrite transformations in flooded paddy soils: rates, pathways, and product spatial distributions.

Between weeks six and twelve, there was an increasing trend in the lepidocrocite crystallite size of samples from CS and UB soils (from 99 nm to 113 nm and from 73 nm to 100 nm, respectively) which cannot be definitively discerned from the uncertainty of the replicate measurements.

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