As an important type of soil erosion, freeze-thaw erosion occurs primarily at high latitude and
altitude. The overview on the effect of freeze-thaw on soil erosion was provided. Soil erosion …

Freeze-thaw erosion occurs primarily at high latitudes and altitudes. Temperature controlled
freeze-thaw events dislodge soil particles and serve as a catalyst for erosion. This review …

Many studies have been carried out on the influence of freeze–thaw cycles on the
mechanical behavior of cement-or lime-stabilized soils. However, very limited studies have …

As global warming intensifies, there will be increased uncertainty as to the environmental
behavior and risks from heavy metals in industrial/legacy contaminated sites in permafrost …

A large alpine meadow in a seasonal permafrost zone exists in the west of Sichuan, which
belongs to a part of the Qinghai–Tibet Plateau, China. Due to the extreme climates and …

As the size of the soil particles varies from 4.75 mm to 1 nm, void spaces form at the
nanolevel. Due to more void spaces impacting a higher plasticity index, more settlement …

The changes in the structure of soil particles configurations due to freeze-thaw (FT) have
great effects on the physical, mechanical, chemical, and biological properties of soil …

In the cold climate regions, repeated freeze–thaw cycles negatively affect the mechanical
behavior of clayey soil material. To minimize or eliminate these negative effects, soil …

Changes in soil performance due to freeze–thaw cycles can lead to subsidence or swelling
of asphalt, which will have a significant impact on road safety performance. The present …

When soil is subjected to freeze–thaw cycles, its macro morphology and overall strength
experience certain changes that often are caused by microscopic modifications of its internal …