Response of soil physical properties to tillage and residue management on two soils in a cool temperate environment.

摘要

In view of their potential benefits, reduced or no tillage (NT) systems are being advocated worldwide. Concerns about impairment of some soil conditions, however, cast doubt on their unqualified acceptance. We evaluated the effects of 6 years of tillage and residue management on bulk density, penetration resistance, aggregation and infiltration rate of a Black Chernozem at Innisfail (loam, 65 g kg-1 organic matter, Udic Boroll) and a Gray Luvisol at Rimbey (loam, 31 g kg-1 organic matter, Boralf) cropped to monoculture spring barley (Hordeum vulgare L.) in a cool temperate climate in Alberta, Canada. Tillage systems were no tillage and tillage with rototilling (T), and two residue levels were straw removed (-S) and straw retained (+S). Bulk density (BD) of the 0-7.5 and 7.5-15 cm depths was significantly greater under NT (1.13-1.58 Mg m-3) than under T (0.99-1.41 Mg m-3) in both soils, irrespective of residue management. In both soils, penetration resistance (PR) was greater under NT than under T to 15 cm depth. Residue retention significantly reduced PR of the 0-10 cm soil in NT, but not in T. In the 0-5 cm depth of the Black Chernozem, the 2 mm fraction of dry aggregates was highest under NT+S (72%), and lowest under T-S (50%). The wind-erodible fraction (dry aggregates 1 mm size) was smallest (18%) under NT+S and largest (39%) under T-S. Soil aggregation benefited more from NT than from residue retention. Proportion of wind-erodible aggregates was generally greater in the Gray Luvisol than in the Black Chernozem. In the Black Chernozem, steady-state infiltration rate (IR) was significantly lower (33%) under NT than under T. Residue retention improved IR in both NT and T. In the Gray Luvisol, IR was not significantly affected by tillage and residue management. Despite firmer soil, NT and residue retention are recommended to improve aggregation in the cool temperate region of Western Canada..