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Investigating the moisture-temperature-deformation interaction in geogrid-reinforced loess under cyclic freezing and thawing

2026 · E3S Web of Conferences · 0 citations · 1 references

Abstract

Frost heave and thaw settlement from cyclic freezing and thawing (F-T) damage infrastructure like roadbeds in cold regions. Geogrids can help control this damage, but their mechanism in complex F-T processes is unclear. This study uses lab tests to examine how geogrids affect moisture, temperature, and deformation in loess during F-T cycles at different initial moisture levels (13%, 16%, 19%). Results show that geogrids disrupt heat flow, creating a temperature buffer, while high moisture slows cooling. The geogrid cut maximum frost heave by 33.6% at 16% moisture but did not change its depth. Thaw settlement changed from a single peak to two peaks, showing the geogrid splits the soil into separate zones. Major water movement to deep soil only happened with high initial moisture. These results explain how geogrids reduce frost heave, aiding better design for cold-region construction.

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