DHARM18 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 Contentn = V
Vv, as a fraction=VV
VV
VW
GVss s
w− =− =− 11
γ∴ n =^1 −W
GVd
γw...(Eq. 2.17)This may provide a practical approach to the determination of n.e =V
Vv
s=()VV
VV
VVG
Ws
ssw
s−
=−= 11 −γ∴ e =VG
Ww
d..γ − 1
...(Eq. 2.18)This may provide a practical approach to the determination of e.n = V
Vv e = V
Vv
s1/n = V/Vv =VV
VV
VV
Ve e
esv
vs
vv
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
Va
vand n =V
Vv∴ nac =V
Va = n
aor na = n.ac ...(Eq. 2.20)
By definition,
w = Ww/Ws, as fraction ; S = Vw/Vv, as fraction ; e = Vv/Vs
S.e = Vw/Vsw = Ww/Ws =V
VV
VGws
ssws
sw.
..
..γ
γγ
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.