Figure 3
From: Dynamic constitutive model of frozen soil that considers the evolution of volume fraction of ice
Adiabatic temperature rise curve of frozen soil with moisture content of 10% at − 28 °C.
Figure 3 | Scientific Reports
From: Dynamic constitutive model of frozen soil that considers the evolution of volume fraction of ice
Adiabatic temperature rise curve of frozen soil with moisture content of 10% at − 28 °C.
