3 results

Aeration condition of a clayey oxisol under long-term no-tillage

Edner Betioli Junior, Cássio Antônio Tormena, Wagner Henrique Moreira, Bruce C. Ball, Getulio Coutinho Figueiredo, Álvaro Pires da Silva, [...]

01/Jun/2014

The hypothesis of this study was that the absence of soil tillage in long-term no-tillage (NT) systems can be detrimental to soil aeration. The objective was to assess the aeration condition of an Oxisol (Rhodic Ferrasol), very clayey texture (750 g kg-1 of clay; 200 g kg-1 of sand), after 30 years of cultivation under NT. The physical property soil air permeability (Ka) is sensitive to changes in the soil pore system. Aside from Ka, the air-filled porosity (ε a) […]

Physical quality of untilled oxisol subjected to mechanical and biological decompaction

Sérgio Damaso da Silveira Junior, Alvaro Pires da Silva, Getulio Coutinho Figueiredo, Cássio Antonio Tormena, Neyde Fabíola Balarezo Giarola

01/Dec/2012

Chiseling and winter cover crops have been adopted to improve the soil physical properties related to aeration. This study aimed to evaluate the effects of winter cover crops and chiseling on physical properties of a Typic Hapludox, clayey texture, after 16 years under no-tillage. The treatments were applied in May 2009, as follows: no-tillage (PD), no-tillage mechanically chiseled to a depth of 0.25 m (PD-E), and biologically aerated soil with no-tillage radish (PD-B). The experiment was arranged in a randomized […]

Soil air permeability in a Rhodic Hapludox under different tillage systems

Sueli Rodrigues, Alvaro Pires da Silva, Neyde Fabíola Balarezo Giarola, Jadir Aparecido Rosa

01/Feb/2011

Air permeability (Kα) can be used to assess soil structure changes resulting from different tillage systems. This study tested the hypothesis that the reduced soil disturbance in no-tillage results in continuous pores and better soil aeration conditions. The objective was to evaluate the aeration of a Rhodic Hapludox under conventional tillage (CT) and no-tillage (NT), based on soil air permeability (Kα), air-filled porosity (εa) and indices of pore continuity (K1 and N). Eighty undisturbed soil cores (2 treatments x 2 […]