INFLUENCE OF DIFFERENT DEPTHS OF PLOWING ON THE PHYSICAL PROPERTIES OF A CLAY SOIL AT GUYENNE, QUEBEC
J. R. LESSARD, HERMAN A. HAMILTON, M. P. LEVESQUE, S. J. Bourget
Abstract
J. R. LESSARD, HERMAN A. HAMILTON, M. P. LEVESQUE, S. J. Bourget
Abstract
An experiment was initiated in 1955 to study the effect of plowing to depths of 6, 12 and 24 inches on the physical properties of a Guyenne clay soil. A 4-year crop rotation was established. Soil core samples were taken in 1957, 1959 and 1960 and determinations of bulk density and porosities were made. The soil particle-size distribution was determined for all tillage treatments in 1960.Plowing to a depth of 24 inches resulted in higher bulk density and lower non-capifiary porosity values in the surface 6-inch soil layer of soil than the 6- and 12-inch plowing. The 18- to 24-inch soil layer was less packed than the corresponding undisturbed layers at the same depth, as a result of deep tillage. The clay content of the 0- to 6-inch layer of soil was also increased by 24-inch plowing. Year-to-year data showed the importance of seasonal climatic conditions on the soil physical properties.
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An experiment was initiated in 1955 to study the effect of plowing to depths of 6, 12 and 24 inches on the physical properties of a Guyenne clay soil. A 4-year crop rotation was established. Soil core samples were taken in 1957, 1959 and 1960 and determinations of bulk density and porosities were made. The soil particle-size distribution was determined for all tillage treatments in 1960.Plowing to a depth of 24 inches resulted in higher bulk density and lower non-capifiary porosity values in the surface 6-inch soil layer of soil than the 6- and 12-inch plowing. The 18- to 24-inch soil layer was less packed than the corresponding undisturbed layers at the same depth, as a result of deep tillage. The clay content of the 0- to 6-inch layer of soil was also increased by 24-inch plowing. Year-to-year data showed the importance of seasonal climatic conditions on the soil physical properties.
Key concepts: Plough, Bulk density, Tillage, Soil science, Porosity, Environmental science, Soil structure, Soil horizon