TY - JOUR
T1 - Experimental evaluation of the pore-access size distribution of sands
AU - Feia, Sadok
AU - Ghabezloo, Siavash
AU - Bruchon, Jean François
AU - Sulem, Jean
AU - Canou, Jean
AU - Dupla, Jean Claude
PY - 2014/1/1
Y1 - 2014/1/1
N2 - A simple experimental method is presented for evaluation of the pore-access size distribution of sands and, more generally, of cohesionless granular materials. The water-retention curve of a sand specimen is evaluated using a technique similar to the hanging column method (ASTM 2008) [ASTM D6836: Standard Test Methods for Determination of the Soil Water Chararcteristic Curve for Desorption Using a Hanging Column, Pressure Extractor, Chilled Mirror Hygrometer, and/or Centrifuge, Annual Book of ASTM Standards, ASTM International, West Conshohocken, PA, 2008] by application of a step-by-step variation of suction and measure of the corresponding changes in water content. The pore-access size distribution is then evaluated from the water-retention curve using the Young-Laplace law, which links the suction to the pore-access radius. The efficiency of this experimental method is demonstrated by studying the influence of various parameters such as the shape and the size of the grains, the spreading of the grain-size distribution, and also the relative density of the specimen on the pore-size distribution.
AB - A simple experimental method is presented for evaluation of the pore-access size distribution of sands and, more generally, of cohesionless granular materials. The water-retention curve of a sand specimen is evaluated using a technique similar to the hanging column method (ASTM 2008) [ASTM D6836: Standard Test Methods for Determination of the Soil Water Chararcteristic Curve for Desorption Using a Hanging Column, Pressure Extractor, Chilled Mirror Hygrometer, and/or Centrifuge, Annual Book of ASTM Standards, ASTM International, West Conshohocken, PA, 2008] by application of a step-by-step variation of suction and measure of the corresponding changes in water content. The pore-access size distribution is then evaluated from the water-retention curve using the Young-Laplace law, which links the suction to the pore-access radius. The efficiency of this experimental method is demonstrated by studying the influence of various parameters such as the shape and the size of the grains, the spreading of the grain-size distribution, and also the relative density of the specimen on the pore-size distribution.
KW - Pore size distribution
KW - Porosity
KW - Sand
KW - Water retention curve
UR - https://www.scopus.com/pages/publications/84904352931
U2 - 10.1520/GTJ20130126
DO - 10.1520/GTJ20130126
M3 - Article
AN - SCOPUS:84904352931
SN - 0149-6115
VL - 37
JO - Geotechnical Testing Journal
JF - Geotechnical Testing Journal
IS - 4
ER -