Results 151 to 160 of about 1,971 (205)

Hydraulic property variations with depth in a loess mudstone landslide. [PDF]

Sci Rep
Liu W, Lin G, Liu Q, Su X.
europepmc   +1 more source

Advances in Flow of Water Through Variably Saturated Soils: A Review of Model Approaches and Experimental Investigations with Use of Sensors. [PDF]

Sensors (Basel)
Osame PU, Peretomode E, Hawez HK.
europepmc   +1 more source

A new method for predicting the shear strength of loess based on moisture content and large and medium pore volume. [PDF]

Sci Rep
Zhang Y, Zhou C, Bian M, Li Z, Fan X.
europepmc   +1 more source

Lime and Fly Ash Co-Solidification Treatment of Oil-Contaminated Soil: Characteristics in Different Water Environments and Evaluation of Engineering Reuse. [PDF]

Toxics
Yu H, Gao P, Li H, Li M.
europepmc   +1 more source

Comparative Study of Effect of SWCC on Seepage Characteristics in Unsaturated Soils

Journal of the Korea Academia-Industrial cooperation Society
Seung-Hyun Lee, Eung-Seok Kim
openaire   +1 more source

Molecular species delimitation analysis of Leptotrombidium spp. and other chigger species parasitizing birds in Malaysia. [PDF]

J Med Entomol
Rajasegaran P, Tan KK, Khoo JJ, Mansor MS, Ahmad Khusaini MKS, AbuBakar S, Ya'cob Z, Makepeace BL.   +7 more
europepmc   +1 more source

Multi-scale soil moisture dynamics in arid mined Loess Plateau arise from crack evolution and microstructure collapse. [PDF]

Sci Rep
Ma T, Tang F, Zhang F.
europepmc   +1 more source

Hydraulic conductivities of unsaturated bauxite: Directly measured and SWCC-based

H. Wang, J. Tan Tian, J. Koseki
openaire   +1 more source

The Effect of Temperature on the SWCC and Estimation of the SWCC from Moisture Profile under a Controlled Thermal Gradient [PDF]

, 2014
In many situations, the upper layers of soil above the ground water table are in a state of unsaturated condition. Although unsaturated soils are found throughout the world, they are predominant in arid or semi-arid regions. In these areas, the soil water characteristic curve (SWCC) which relates the water content to the matric suction could be used as
Roshani, Pedram
openaire   +3 more sources

Laboratory versus field SWCC data

, 2009
Soil Water Characteristic Curves (SWCCs) are typically determined in the laboratory by performing drying tests on samples in a Tempe cell. In some cases, re-wetting is also carried out. The advantage of using drying tests is that they are carried out from the saturated state at a given sample test density, so that there is some chance of obtaining ...
Williams, D. J.
openaire   +2 more sources