Laboratory and experimental tests in huge amount are required during engineering surveys for large and critical buildings and structures especially in complex geological conditions. The laboratory investigations are applicable in cases with no possibility for field tests. However, as a rule the results obtained from laboratory investigations (in particular compression tests) ...

Mass construction of structures is complicated on collapsing soils. The time course of deformations in collapsing soils is determined by their moisture content. Since collapsing soils are usually in a low moisture state, their compressive strain from external load occurs within a relatively brief time. Soil subsidence, and equally collapsing in the water-saturated state, ...

Mass construction of structures is complicated on collapsing soils. The time course of deformations in collapsing soils is determined by their moisture content. Since collapsing soils are usually in a low moisture state, their compressive strain from external load occurs within a relatively brief time. Soil subsidence, and equally collapsing in the water-saturated state, ...

Laboratory and experimental tests in huge amount are required during engineering surveys for large and critical buildings and structures especially in complex geological conditions. The laboratory investigations are applicable in cases with no possibility for field tests. However, as a rule the results obtained from laboratory investigations (in particular compression tests) ...

Laboratory and experimental tests in huge amount are required during engineering surveys for large and critical buildings and structures especially in complex geological conditions. The laboratory investigations are applicable in cases with no possibility for field tests. However, as a rule the results obtained from laboratory investigations (in particular compression tests) ...

Mass construction of structures is complicated on collapsing soils. The time course of deformations in collapsing soils is determined by their moisture content. Since collapsing soils are usually in a low moisture state, their compressive strain from external load occurs within a relatively brief time. Soil subsidence, and equally collapsing in the water-saturated state, ...