Determination of the Critical State Line in Partially Frozen Sand

A new method for measuring internal pore water pressure (PWP) is introduced to determine the critical state line (CSL) in partially frozen sand, investigating the influence of temperature and strain rate on the critical state parameters. A series of consolidated undrained and drained triaxial tests, along with internal PWP measurements, were conducted on both dense and loose specimens under different temperatures and strain rates. Similarly to unfrozen sand, a unique CSL was established for the partially frozen sand at −3 °C in both stress (q-p′) and void ratio (e-p′) space. The results show that the critical state friction angle (φcs′) is not affected by temperature (warmer than −5 °C) and strain rate, while the critical state cohesion (ccs′) varies with temperature, strain rate and failure mode. The ccs′ increases with decreasing temperature from 23 °C to −3 °C and to −10 °C, but decreases to zero when the strain rate was reduced from 1%/min to 0.1%/min. In e-p′ space, the slope of CSL could be associated with the dilation of partially frozen sand, which increases with decreasing temperature and increasing strain rate, potentially due to the increased contact area between the pore ice and sand grains.

Authors

Institutions

Publication Details

Journal
Geotechnics
Published
2025-02-04
DOI
https://doi.org/10.3390/geotechnics5010010
Citations
1
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
1.30

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Determination of the Critical State Line in Partially Frozen Sand

Nicholas Beier, Yawu Liang, Dave Sego
1 citations
Geotechnics
Climate change and permafrost
1.30
article

Determination of the Critical State Line in Partially Frozen Sand

Nicholas Beier, Yawu Liang, Dave Sego
article en
1 citations

Abstract

A new method for measuring internal pore water pressure (PWP) is introduced to determine the critical state line (CSL) in partially frozen sand, investigating the influence of temperature and strain rate on the critical state parameters. A series of consolidated undrained and drained triaxial tests, along with internal PWP measurements, were conducted on both dense and loose specimens under different temperatures and strain rates. Similarly to unfrozen sand, a unique CSL was established for the partially frozen sand at −3 °C in both stress (q-p′) and void ratio (e-p′) space. The results show that the critical state friction angle (φcs′) is not affected by temperature (warmer than −5 °C) and strain rate, while the critical state cohesion (ccs′) varies with temperature, strain rate and failure mode. The ccs′ increases with decreasing temperature from 23 °C to −3 °C and to −10 °C, but decreases to zero when the strain rate was reduced from 1%/min to 0.1%/min. In e-p′ space, the slope of CSL could be associated with the dilation of partially frozen sand, which increases with decreasing temperature and increasing strain rate, potentially due to the increased contact area between the pore ice and sand grains.

GeotechnicsVol. 5(1)
University of Alberta (CA)
University of Alberta, Natural Sciences and Engineering Research Council of Canada
Openalex Percentile: Top 27%
Climate change and permafrost
1.30
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.

Determination of the Critical State Line in Partially Frozen Sand — Nicholas Beier, Yawu Liang, et al. · Geotechnics (2025) | TGRS Research Map | TGRS