No-tillage associated to cover crops may maintain soil quality, improving or preserving favorable soil physical conditions for plant growth. This study assessed soil bulk density, porosity, penetration resistance, and water infiltration of a PALEUDALF, in the Experimental Area of the Soil Science Department of the Federal University of Santa Maria, in Santa Maria, RS, Brazil, in an experiment started in 1991, with the following crop successions and rotations: (1) Corn/Soybean - Jackbean - MFP; (2) Bare soil - SDES; (3) Corn/Soybean - Fallow -POU; (4) Corn/Soybean - Ryegrass + Vetch - AZEV; (5) Corn/Soybean - Mucuna - MUC; (7) Natural Grass - CNA; (6) Corn/Soybean - Oilseed radish - NFO. Soil bulk density was affected in the 0-0.10 m layer; values were highest in the SDES. Total soil porosity and soil macroporosity were closely correlated to a depth of 0.10 m. Major restriction to root penetration occurred in the surface layer (0-0.03 m) in the SDES treatment, and NFO had greatest values at 0.16-0.18 m depth. The water infiltration rate was lowest in SDES and CNA treatments in all evaluations, while in the others infiltration was constant and statistically equal. Constantly uncovered soil induces degradation in soil physical properties. The studied cropping systems confirmed significant benefits in soil density, porosity, resistance, and water infiltration rate under long term no-tillage.
soil compaction; porosity; water infiltration; cover crops; tropical legumes; oilseed radish
