Analysis of changes in volume and propagation of cracks in expansive soil due to changes in water content
27/Nov/2020
ABSTRACT Expansive clay soils are a problem for agriculture and engineering because they are susceptible to change in volume due to seasonal variation in water content and temperature. One of its morphological properties is slickensides, which result from the ability to contract and crack when dry and expand by wetting. The objective of this study was to evaluate the processes of expansion and formation and propagation of cracks due to the change in water content over time. The expansion process […]
Rheological Parameters as Affected by Water Tension in Subtropical Soils
06/Jun/2016
ABSTRACT Rheological parameters have been used to study the interaction between particles and the structural strength of soils subjected to mechanical stresses, in which soil composition and water content most strongly affect soil resistance to deformation. Our objective was to evaluate the effect of water tension on rheological parameters of soils with different mineralogical, physical, and chemical composition. Surface and subsurface horizons of four Oxisols, two Ultisols, one Alfisol, and one Vertisol were physically and chemically characterized; their rheological parameters […]
Soil elasticity as affected by water and organic carbon content
01/Apr/2008
The organic carbon accumulation observed in soils under no-till system can increase the soil elasticity, resulting in a higher resistance to soil compaction. This study was carried out to evaluate the effects of water content and soil organic carbon (SOC) enrichment on soil elasticity. Samples of a Hapludalf and a Typic Hapludox in southern Brazil, both with a significant variation in SOC content, were equilibrated at four different water tensions, and then loaded and unloaded on a uniaxial apparatus. The […]
Inter and intra-aggregate strength in direct shear tests of a typic hapludox
01/Apr/2007
For aggregated soils the Mohr failure line can be separated into two straight lines, with different slopes and intercepts. In the range of low normal load, when the slope is very steep and the intercept is small, the failure line is defined by the friction and cohesion inter-aggregates, while for the higher load range the slope becomes smaller and intercept is larger, which defines the intra-aggregate friction and cohesion. Therefore, for aggregated soils the normal load range used in the […]