Rain Infiltration as Affected by Wheat Residue Amount and Distribution in Ridged Tillage

Abstract

AbstractTexas South Plains production systems for conserving rainfall and reducing wind erosion in cotton (Gossypium hirsutum L.), a low‐residue crop, include the spring chemical termination of winter wheat (Triticum aestivum L.) overseeded post‐harvest into cotton. This practice often increases cotton lint yields under irrigation, but residues hinder weed control and increase production costs. This study characterized infiltration response to (i) residue weathering and soil consolidation with ridges, (ii) residue distribution on the ridge or in the furrow, and (iii) flat or standing architectures and residue amounts. Simulated rain was applied at 65 mm h−1 for 1 h into a bare Olton clay loam (fine, mixed, thermic Aridic Paleustoll). Mean cumulative infiltration was lowest for bare soil (28.7 mm), but increased curvilinearly with increasing residue amounts, leveling at 49.0 mm. Cumulative infiltration with residues distributed on the ridge (42 mm) or in the furrows (44 mm) were the same even though water in the furrow absorbed drop impact. A minimum amount of residue (0.7 Mg ha−1) to intercept raindrop impact was needed to increase rain infiltration, but increasing residue above a residue threshold of 2.4 Mg ha−1 had no effect because of sufficient drop impact interception. Increases in infiltration were related to the residue amount rather than to the bed or furrow location. Partial residue cover and tillage operations that lodge crop residues may increase infiltration.