DHARM
18 GEOTECHNICAL ENGINEERING
A number of useful relationships may be derived based on the foregoing definitions and
the soil-phase diagram.
2.3.1 Relationships Involving Porosity, Void Ratio, Degree of Saturation,
Water Content, Percent Air Voids and Air Content
n = V
V
v, as a fraction
=
VV
V
V
V
W
GV
ss s
w
− =− =− 11
γ
∴ n =^1 −
W
GV
d
γw
...(Eq. 2.17)
This may provide a practical approach to the determination of n.
e =
V
V
v
s
=
()VV
V
V
V
VG
W
s
ss
w
s
−
=−= 11 −
γ
∴ e =
VG
W
w
d
..γ − 1
...(Eq. 2.18)
This may provide a practical approach to the determination of e.
n = V
V
v e = V
V
v
s
1/n = V/Vv =
VV
V
V
V
V
V
e e
e
sv
v
s
v
v
v
+ =+=+= 11 / () 1 +
∴ n =
e
()1+e
...(Eq. 2.19)
e = n/(1 – n), by algebraic manipulation ...(Eq. 2.20)
These interrelationships between n and e facilitate computation of one if the other is
known.
Q^ ac =
V
V
a
v
and n =
V
V
v
∴ nac =
V
V
a = n
a
or na = n.ac ...(Eq. 2.20)
By definition,
w = Ww/Ws, as fraction ; S = Vw/Vv, as fraction ; e = Vv/Vs
S.e = Vw/Vs
w = Ww/Ws =
V
V
V
VG
ws
ss
ws
sw
.
.
.
..
γ
γ
γ
γ
= = Vw/VsG = S.e/G
∴ w.G = S.e ...(Eq. 2.21)
(Note. This is valid even if both w and S are expressed as percentages). For saturated condition,
S = 1.