Theory
Prove: `gamma_(sb)=(G-1)/(1+e)*gamma_w`.where,`gamma_(sb)` represents submerged unit weight.
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Prove: `gamma_d=gamma_t/(1+w)`
We know, by definition,
`gamma_d=W_s/V`
`=W_s/V*W/W`
`=(W/V)/((W_w+W_s)/W_s)`
`=gamma_t/(1+W_w/W_s)`
`=gamma_t/(1+w)`
Thus, `gamma_d=gamma_t/(1+w)`
All Chapters — Soil Mechanics
Introduction
Index properties of soil
Phase Diagram Of Soil
Soil Indentification and Classification
Soil Structure and Clay Minerals
Soil Compaction
Principle of Effective Stress, Capillarity, and Permeability
Seepage through Soils
Vertical Stress below Applied Load
Compressibility of Soils
Shear Strength of Soil
Stability of Slopes
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