gwkwong
Civil/Environmental
- Sep 7, 2007
- 30
I am confused with basic principal of drained shear strength.
In drained condition, the pore water pressure dissipate and the load will be carried by the soil grain itself. In this case, the effective soil density is the total density of the soil. But if the soil is below the groundwater level, we will have to use the total soil density minus the density of the water to get the effective density of the soil. So what is the mechanism behind this, where the soil is submerged but yet "drained".
In drained condition, the pore water pressure dissipate and the load will be carried by the soil grain itself. In this case, the effective soil density is the total density of the soil. But if the soil is below the groundwater level, we will have to use the total soil density minus the density of the water to get the effective density of the soil. So what is the mechanism behind this, where the soil is submerged but yet "drained".