TY - JOUR
T1 - Hydraulic conductivity of fine-grained soils subjected to freeze-thaw cycles
AU - Feng, Shuyin
AU - Ibraim, Erdin
AU - Vardanega, Paul J
N1 - Funding Information:
The first author thanks Dr. S. Kearns from the University of Bristol for helpful discussions related to the SEM images, and Mr. G. Martin from the University of Bristol for technical support during the geotechnical laboratory testing programme. The first author acknowledges the support from the China Scholarship Council ( 201708060067 ) during her doctoral studies at the University of Bristol .
Publisher Copyright:
© 2023 The Authors
PY - 2023/9/1
Y1 - 2023/9/1
N2 - This paper presents laboratory data from tests on four fine-grained soils: reconstituted Kaolinite, destructured Bothkennar clay, reconstituted Bothkennar clay, and reconstituted Gault clay. The soil samples were conditioned in an oedometer cell while being subjected to varying numbers of freezing and thawing cycles. The influence of freeze-thaw cycles on key soil parameters, including the hydraulic conductivity, Atterberg limits, compression and swelling index was studied. The experimental results were then compared with the analysis of a previously published database of hydraulic conductivity measurements on fine-grained soils called FG/KSAT-1358. The paper demonstrates that while multiple cycles of freezing and thawing affect some of the studied soil parameters, such as the Atterberg limits and the compression characteristics, the effects on the hydraulic conductivity transformation model parameters, linking the water content ratio to hydraulic conductivity are less apparent. The results are useful for geotechnical and pavement engineers when making assessments of freeze-thaw effects on subgrade materials in cold regions.
AB - This paper presents laboratory data from tests on four fine-grained soils: reconstituted Kaolinite, destructured Bothkennar clay, reconstituted Bothkennar clay, and reconstituted Gault clay. The soil samples were conditioned in an oedometer cell while being subjected to varying numbers of freezing and thawing cycles. The influence of freeze-thaw cycles on key soil parameters, including the hydraulic conductivity, Atterberg limits, compression and swelling index was studied. The experimental results were then compared with the analysis of a previously published database of hydraulic conductivity measurements on fine-grained soils called FG/KSAT-1358. The paper demonstrates that while multiple cycles of freezing and thawing affect some of the studied soil parameters, such as the Atterberg limits and the compression characteristics, the effects on the hydraulic conductivity transformation model parameters, linking the water content ratio to hydraulic conductivity are less apparent. The results are useful for geotechnical and pavement engineers when making assessments of freeze-thaw effects on subgrade materials in cold regions.
KW - Freeze-thaw
KW - Clays
KW - Atterberg limits
KW - Hydraulic conductivity
U2 - 10.1016/j.coldregions.2023.103902
DO - 10.1016/j.coldregions.2023.103902
M3 - Article (Academic Journal)
VL - 213
JO - Cold Regions Science and Technology
JF - Cold Regions Science and Technology
M1 - 103902
ER -