In general, soil puddlability depends on moisture content, soil type, tillage implement, and cultural practices and observed that the amount of dispersed aggregates decreased with
increasing intensity, but was offset by organic amendments, which was attributed to formation of stable macroaggregates with macropores in the organic amended soil.
In general, soil puddlability depends on moisture content, soil type, tillage implement, and cultural practices and observed that the amount of dispersed aggregates decreased with
increasing intensity, but was offset by organic amendments, which was attributed to formation of stable macroaggregates with macropores in the organic amended soil.
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