DHARM
156 GEOTECHNICAL ENGINEERING
∴ k 2 = 0 2025
0 1296
.
.
× 0.36 = 5.625 × 10–1 mm/s.
Example 5.15. Permeability tests on a soil sample gave the following data:
Test No. Void ratio Temperature °C Permeability in 10–3
mm/s
1 0.63 20 0.36
2 1.08 36 1.80
Estimate the coefficient of permeability at 27°C for a void ratio of 0.90.
Viscosity at 20 C = 1.009 10 N.sec/mm
Viscosity at 36 C = 0 10 N.sec/mm
Viscosity at 27 C = 0 10 N.sec/mm
Unit weight = 9.81 10 N/mm
2
2
2
63
°×
°×
°×
U
V
|
W
|
×
−
−
−
−
9
9
9
706
855
.
.
γ
According to Poisuelle’s equation adapted to flow through soil,
k = D
e
e
s^2 C
3
1
..
()
.
γ
μ+
From test 1,
0 36 10 9 81 10
1 009 10
063
163
3
2
6
9
.^3
.
.
.
.(. )
(. )
× = ×
×
−−
DC −
s
= 1491.46
∴ Ds^2. C = 2.414 × 10–7
From test 2,
1 80 10 9 81 10
0 706 10
108
208
3
2
6
9
.^3
.
.
.
.(. )
.
× = ×
×
−−
DC −
s
= 8415.35
∴ Ds^2. C = 2.139 × 10–7
Average value of Ds^2. C = 2.2765 × 10–7
∴ At 27°C and a void ratio of 0.90,
k = 2.2765 × 10–7 ×
981 10
0 855 10
090
19
6
9
.^3
.
.(. )
.
×
×
−
− = 1.002 × 10–3 mm/s.
Example 5.16. To what height would water rise in a glass capillary tube of 0.01 mm diam-
eter? What is the water pressure just under the meniscus in the capillary tube?
Capillary rise, hc =
4 T
d
s
γwc
, where Ts is surface tension of water and γw is its unit weight
and dc is the diameter of the capillary tube.
∴ hc =
47310
981 10 001
6
6
××
××
−
..− mm, assuming Ts = 73 × 10
–6 N/mm and
= 30/0.01 mm γw = 9.81 × 10–6 N/mm^3.
= 3000 mm or 3 m.
Water pressure just under the meniscus in the tube
= 3000 × 9.81 × 10–6 N/mm^2