Spatial variation of infiltration rate and compactness in paddy fields

Abstract

Percolation loss of water in rice fields is a major cause of low water use efficiency. Variation of infiltration rate and soil compactness in four paddy fields (with clay, silty clay, clay loam, and loam textures) was investigated in northern Iran. In each field, in longitudinal and transverse directions, points located 0.5, 2.5, 6.5, 12.5, … m from the bunds were selected and water infiltration rate and resistance to penetration of a pocket penetrometer were measured. The results showed that in clay soil, average final infiltration rate (f c ) in longitudinal direction, transverse direction, and center of the field was 0.216, 0.136, and 0.08 cm day -1 , respectively. The f c for loamy soil was 2.77, 2.32, and 0.409 cm day -1 , respectively. Similar differences were observed in the other two soil textures. In general, effect of direction of the field for measuring infiltration rate was not statistically significant. Loam and clay loam soils, with resistance to penetration of 0.37 and 0.33 kg cm -2 , were not significantly different. But, clay and silty clay soils with resistance to penetration of 0.25 and 0.14 kg cm -2 were significantly different (P \ 0.05). Resistance to penetration of the penetrometer was not affected significantly (P \ 0.05) by direction of measuring this parameter in the field. The conclusion is that if measured soil physical properties in a paddy field are going to be representative of the whole field, they should be measured at different locations, especially near the bunds. Another strategy for obtaining a representative infiltration rate or compactness for a paddy field is uniform puddling of the field.