1963•Canadian Journal of Soil ScienceRequires access

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

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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.

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Available 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.

Key concepts: Plough, Bulk density, Tillage, Soil science, Porosity, Environmental science, Soil structure, Soil horizon

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