Summary
In six paddy soils from the same volcanic-ash parent material, incubated under submergence, the reduction of ferric iron proceeded linearly against time. A significant negative correlation (r=−0.906, p<0.05) was found between the rate of consumption of ferric iron (reduction) and the ratio of the rate of consumption of organic N compounds to that of ferric iron. Organic N compounds are the main substrate for the iron-reduction metabolism in the soils in which the rate of iron reduction is slow. re]19751028
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Kagawa, H. The significance of organic N compounds as the substrate for the iron-reduction metabolism in the submerged paddy soils. Plant Soil 47, 81–88 (1977). https://doi.org/10.1007/BF00010370
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DOI: https://doi.org/10.1007/BF00010370