Abstract
Changes in N, P, K, Ca and Mg in soil and rice plants were investigated during a cropping season following a long fallow period in a system of traditional cultivation practised for several centuries, under a village tank irrigation system. Soil, N, P, K, Ca and Mg were not found to be deficient for rice production throughout the season. Flooding did not produce toxic levels of Fe and Na and soil pH remained at 6.4 during the season. The average grain yield (3.5 t/ha) without any addition of chemical fertilizer was almost the same as that from fields under major irrigation systems where fertilizer application (less than the recommended level) was common. The sustainability of soil fertility under the traditional system of rice cultivation appears to be dependent upon long fallow periods. The natural build-up of soil fertility during a three-year fallow was evidently adequate to support a good growth of the crop which produced a yield comparable to that obtained in chemically fertilized, more intensively cropped rice fields under major irrigation systems.
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