Atmosphere process of infiltration or evaporation affect the behavior of geotechnical structures located near the soil surface. This paper focuses on the drying process of soils due to evaporation. The scaling laws are analyzed and afterwards the results on applying two cycles of heating and cooling on a soil mass are presented. Based on these results, conclusions about the feasibility of reproducing evaporation on centrifuge models are recommended
Studies conducted in the past reveal that heat transfer through a soil mass depends basically on its...
The methods of mathematical description of evaporation processes from light soils of the arid zone o...
Evaporation is an important component of the soil water balance. It is composed of water flow and tr...
Soil-atmospheric interaction processes such as infiltration or evaporation can have a significant ef...
The behavior of geotechnical structures located near the soil surface is highly influenced by unsatu...
The soil water evaporation is a critical component of both the surface energy balance and water bala...
Migration of heat and mass transfer through geomaterials is of great interest in various civil and e...
The behavior of geotechnical structures located near the soil surface is highly influenced by unsatu...
ICPMG 2018, 9th International Conference on Physical Modelling in Geotechnics, LONDRES, ROYAUME-UNI,...
Due to climate change, soil desiccating became a serious concern in the agricultural area of Belgium...
International audienceThe global warming and climate change have aroused increasing attention to the...
Soil shrinks as it desiccates, and the magnitude of shrinkage can be large for clayey soils. The dr...
The use of centrifuge modeling where unsaturated soils are involved is more limited than its use in ...
Extreme, extended wet and dry seasons increase the adverse effects that soil wetting and drying cycl...
Soils undergoing desiccation exhibit shrinkage and eventually cracking. That may become an environme...
Studies conducted in the past reveal that heat transfer through a soil mass depends basically on its...
The methods of mathematical description of evaporation processes from light soils of the arid zone o...
Evaporation is an important component of the soil water balance. It is composed of water flow and tr...
Soil-atmospheric interaction processes such as infiltration or evaporation can have a significant ef...
The behavior of geotechnical structures located near the soil surface is highly influenced by unsatu...
The soil water evaporation is a critical component of both the surface energy balance and water bala...
Migration of heat and mass transfer through geomaterials is of great interest in various civil and e...
The behavior of geotechnical structures located near the soil surface is highly influenced by unsatu...
ICPMG 2018, 9th International Conference on Physical Modelling in Geotechnics, LONDRES, ROYAUME-UNI,...
Due to climate change, soil desiccating became a serious concern in the agricultural area of Belgium...
International audienceThe global warming and climate change have aroused increasing attention to the...
Soil shrinks as it desiccates, and the magnitude of shrinkage can be large for clayey soils. The dr...
The use of centrifuge modeling where unsaturated soils are involved is more limited than its use in ...
Extreme, extended wet and dry seasons increase the adverse effects that soil wetting and drying cycl...
Soils undergoing desiccation exhibit shrinkage and eventually cracking. That may become an environme...
Studies conducted in the past reveal that heat transfer through a soil mass depends basically on its...
The methods of mathematical description of evaporation processes from light soils of the arid zone o...
Evaporation is an important component of the soil water balance. It is composed of water flow and tr...