The objective of this study was to evaluate alterations in the physical soil quality of a Dystroferric Red Latosol (Typic Haplorthox) caused by chiseling, after thirteen years of no-tillage. The experiment consisted of two management systems: soil chiseling down to a 0.30 m depth (NTC) and no-tillage (NT). Undisturbed soil samples were collected at depths of 0-0.15 m and 0.15-0.30 m, and the soil water retention curve, the soil resistance to penetration curve, the soil bulk density, and the "Least Limiting Water Potential" (LLWP) were determined. The results showed that the chiseling caused modifications in soil porosity in the 0-0.15 m layer, maintaining appropriate aeration conditions in water matric potentials under 0.01 MPa. On the other hand, the strongest limitations by soil penetration resistance in matric potentials under 1.5 MPa were verified in the NTC soil management. In the 0.15-0.30 m soil layer under the NTC treatment, the soil penetration resistance was the upper limit of the LLWP. The results of the study indicate that under the present management condition, chiseling is not necessary in this soil.
soil penetration resistance; no-tillage; soil structure; least limiting water potential (LLWP)
