Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Flow of water in soils at small hydraulic gradients
It is shown that permeability of fully saturated sand-gravel actually increases when hydraulic gradient decreases below 0.2; permeability on unsaturated soil decreases; conception of S.A.Roxa (1950) that clay soil is impermeable at small hydraulic gradients is further investigated and its application in favor of accuracy when investigating settlement of structures is demonstrated.
Flow of water in soils at small hydraulic gradients
It is shown that permeability of fully saturated sand-gravel actually increases when hydraulic gradient decreases below 0.2; permeability on unsaturated soil decreases; conception of S.A.Roxa (1950) that clay soil is impermeable at small hydraulic gradients is further investigated and its application in favor of accuracy when investigating settlement of structures is demonstrated.
Flow of water in soils at small hydraulic gradients
RILEM Bul
Mencl, V. (Autor:in) / Bobkova, J. (Autor:in) / Hanzlova, V. (Autor:in)
1965
2 pages
Report
Englisch
© Metadata Copyright Elsevier B. V. All rights reserved.
| Engineering Index Backfile | 1930
| Engineering Index Backfile | 1930
Experimental Investigation of Critical Hydraulic Gradients for Unstable Soils
| British Library Conference Proceedings | 2011
Coupled heat and moisture flow in unsaturated soils under opposing thermal and hydraulic gradients
| British Library Conference Proceedings | 2000