Strain rate effect on the tensile strength of frozen silt

Tension tests at constant rates were conducted on remolded saturated frozen Fairbanks silt with medium density at -5°C for various machine speeds. It is found that the tensile strength depends strongly upon strain rate and the critical strain rate for ductile-brittle transition was about 10-2S_1. The peak tensile strength condierably decreases with decreasing strain rate for ductile failure, while it slightly decreases with increasing strain rate in the brittle region. The failure strain also varies with strain rate, but the initial tangent modulus is found not to be depend upon strain rate.

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Publication Details

Published
2026-02-12
DOI
https://doi.org/10.1201/9781003763062_24
Citations
11
Primary Topic
Climate change and permafrost
Type
article
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article

Strain rate effect on the tensile strength of frozen silt

David L. Carbee, Yuanlin Zhu
11 citations
Climate change and permafrost
article

Strain rate effect on the tensile strength of frozen silt

David L. Carbee, Yuanlin Zhu
article en
11 citations

Abstract

Tension tests at constant rates were conducted on remolded saturated frozen Fairbanks silt with medium density at -5°C for various machine speeds. It is found that the tensile strength depends strongly upon strain rate and the critical strain rate for ductile-brittle transition was about 10-2S_1. The peak tensile strength condierably decreases with decreasing strain rate for ductile failure, while it slightly decreases with increasing strain rate in the brittle region. The failure strain also varies with strain rate, but the initial tangent modulus is found not to be depend upon strain rate.

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