Preprints
https://doi.org/10.5194/egusphere-2025-4383
https://doi.org/10.5194/egusphere-2025-4383
14 Nov 2025
 | 14 Nov 2025
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Behavior of Snow Containing an Ice Lens under Compressive Loading

Marin Nicole Blaisdell and Ian Baker

Abstract. In order to understand the effects of strain rate on the mechanical response of snow containing an ice lens perpendicular to the loading direction, specimens with and without ice lenses were compressed at several different rates from 4 x 10-4 to 1.2 x 10-2 s-1. It was found that snow columns with an included ice lens follow the same behavior as homogeneous snow for the range of strain rates tested, the sole difference being a six-fold increase in stress at a given strain when an ice lens is present. For all samples, low strain rates (4 x 10-4 to 1.2 x 10-3 s-1) resulted in a smooth steady increase in stress with increasing strain, whereas at high strain rates (4 x 10-3 to 1.2 x 10-2 s-1) two loading regimes occurred; up to ~20 % strain stresses minimally increased, while higher strains led to a more rapid stress increase. Snow columns both with and without an ice lens showed the highest resistance to loading at intermediate rates (2.1 x 10-3 to 3 x 10-3 s-1) which allowed for reconfiguration of the ice particles whilst inducing pressure sintering to strengthen existing bonds. Stress differences between aged and fresh snow were distinct but not as large as those between ice lens-containing and homogenous snow, indicating that ice lenses have a higher contribution to snow strength than sintering alone.

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Marin Nicole Blaisdell and Ian Baker

Status: open (until 26 Dec 2025)

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Marin Nicole Blaisdell and Ian Baker
Marin Nicole Blaisdell and Ian Baker

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Short summary
Snow with and without an ice lens was compressed at varying rates to understand how loading affects microstructure and mechanical response. Results show that snow with an ice lens is six-times stronger than without, and both types produced highest stresses at intermediate rates until high strain. Maximum connectivity between ice particles occurred at high strength, when force is adequate to strengthen bonds but insufficient for reconfiguration. This has implications for avalanche forecasting.
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