Long-term tillage and wheel traffic effects on a poorly drained mollic ochraqualf in northwest Ohio. 1. Soil physical properties, root distribution and grain yield of corn and soybean

• Published in: Soil & tillage research Vol. 14; no. 4; pp. 341 - 358
• Main Authors: Lal, R., Logan, T.J., Fausey, N.R.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.09.1989
• Subjects: COMPACTACION DEL SUELO; COMPACTAGE DU SOL; CROP YIELD; GLYCINE MAX; LABRANZA; OHIO; PROPIEDADES FISICO-QUIMICAS (SUELO); PROPRIETE PHYSICO-CHIMIQUE DU SOL; RENDEMENT DES CULTURES; RENDIMIENTO DE CULTIVOS; ROOT SYSTEMS; SISTEMA RADICULAR; SOIL CHEMICOPHYSICAL PROPERTIES; SOIL COMPACTION; SYSTEME RACINAIRE; TILLAGE; TRAVAIL DU SOL; ZEA MAYS
• ISSN: 0167-1987; 1879-3444
• DOI: 10.1016/0167-1987(89)90054-8

Effects of 12 years of 4 tillage systems, were studied on soil bulk density, infiltration rate, penetration resistance, structural stability of aggregates, root length density, moisture release characteristics and grain yield. The objective of this study was to assess long-term effects of tillage methods and guided traffic on soil properties and crop response on a heavy-textured poorly drained soil. Tillage systems included: (A) continuous no-till for 12 years; (B) no-till for 10 years followed by plow-till for 2 years; (C) plow-till for 10 years followed by no-till for 2 years; (D) continuous plow-till for 12 years. Wheel tracks had significant effects on soil physical properties. Soil in the traffic zone (TZ) in no-till treatment had higher bulk density and penetration resistance (PR) for the upper 0–30-cm layer than plow-till treatment. The PR for the surface layer in TZ was 25–46% more than in the row zone (RZ). Mean soil bulk density in the TZ of no-till plots was about 12% more than in the RZ (1.53 vs. 1.36 g cm −3). Changeover from no-till to plow-till decreased PR in RZ and TZ by 50–60% while that from plow-till to no-till increased PR by 10–20%. Similar effects were observed in percent aggregation and the mean weight diameter. In no-till treatments both initial and equilibrium infiltration rates were significantly lower in TZ than RZ (27.5 vs. 6.8 cm h −1 initial and 10.0 vs. 1.5 cm h −1 final). There were more macropores (> 2 mm) for the TZ in no-till compared with the plow-till treatments. Fine or micropores were comparatively more numerous in the sub-soil of no-till than plow-till treatments. The median aggregate size (D 50) was 6.2, 4.2, 4.8 and 3.5 mm for Treatments A, B, C and D, respectively. Root length density of corn in plow-till plots was significantly more than that in no-till plots for the top 0–20-cm layer. Corn and soybean yields were greater in plow-till than no-till treatments. Grain yields in Treatment D were greater than those in Treatment A by 10% for corn and by 6% for soybean.