DHARMCOMPOSITION OF SOIL TERMINOLOGY AND DEFINITIONS 19∴ wsat = e/G or e = wsat.G ...(Eq. 2.22)na =V
VVV
VVv
vv
v
v
vev
v
eavw
svv
sw
s
v
sw
= − s
+=−+=−1 1 +But S.e = Vw/Vs∴ na =eSe
eeS
e−
+= −
+.()
11
1...(Eq. 2.23)Also na = ()ee^1 + (1 – S) = n(1 – S) ...(Eq. 2.24)
ac = Va/Vv
S = Vw/Vvac + S =()VV
Vaw
v+
= Vv/Vv = 1∴ ac = (1 – S) ...(Eq. 2.25)
In view of Eq. 2.25, Eq. 2.24 becomes na = n.ac, which is Eq. 2.20.2.3.2 Relationships Involving Unit Weights, Grain Specific Gravity, Void
Ratio, and Degree of Saturationγ = W/V =WW
VVWWW
VVVsw
svsws
svs+
+= +
+(/)
(/)1
1But Ww/Ws = w, as a fraction ;V
Vv
s= e ; andW
Vs
s= γs = G.γw∴ γ = G w
w e
γ ()
()1
1+
+(w as a fraction) ...(Eq. 2.26)Further, γ =()
()GwG
e w+
1 +γBut w.G = S.e∴γ =(.)
().GSe
e w+
1 +γ (S as a fraction) ...(Eq. 2.27)This is a general equation from which the unit weights corresponding to the saturated
and dry states of soil may be got by substituting S = 1 and S = 0 respectively (as a fraction).∴γsat =Ge
e w+
+F
HGI
1 KJ.γ ...(Eq. 2.28)and γd =
G
e. w
()
γ
1 +...(Eq. 2.29)Note. γsat and γd may be derived from first principles also in just the same way as γ.
The submerged unit weight γ′ may be written as :
γ′ = γsat – γw ...(Eq. 2.12)