DHARM
COMPOSITION OF SOIL TERMINOLOGY AND DEFINITIONS 19
∴ wsat = e/G or e = wsat.G ...(Eq. 2.22)
na =
V
V
VV
VV
v
v
v
v
v
v
e
v
v
e
avw
sv
v
s
w
s
v
s
w
= − s
+
=
−
+
=
−
1 1 +
But S.e = Vw/Vs
∴ na =
eSe
e
eS
e
−
+
= −
+
.()
1
1
1
...(Eq. 2.23)
Also na = ()ee^1 + (1 – S) = n(1 – S) ...(Eq. 2.24)
ac = Va/Vv
S = Vw/Vv
ac + S =
()VV
V
aw
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 Saturation
γ = W/V =
WW
VV
WWW
VVV
sw
sv
sws
svs
+
+
= +
+
(/)
(/)
1
1
But Ww/Ws = w, as a fraction ;
V
V
v
s
= e ; and
W
V
s
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 +
γ
But 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
HG
I
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)