DHARM
80 GEOTECHNICAL ENGINEERING
the original soil was 50, what is the percentage of particles finer computed above in the entire
soil sample?
By Eqs. 3.21 and 3.22,
D = K Ht/
where K =
3
1
μ
γ
w
w()G−
∴ K =
3
1
×
×−
0.001
9.8 ()2.72
= 0.0133 mm
min
cm
D = 0.0133^10
10
mm = 0.0133 mm
This is the largest size remaining at the sampling depth.
By Eq. 3.26,
Nf =
W
W
V
V
p
sp
F
HG
I
KJ
F
HG
I
KJ
× 100
Here Wp = 0.0032 N; Ws = 0.5 N; V = 500 ml; Vp = 10 ml.
∴ Nf =
0.0032
050
500
. 10
× × 100 = 32%
Thus, the percentage of particles finer than 0.0133 mm is 32.
By Eq. 3.28, N = Nf(Wf/W)
Here Wf/W is given as 0.50.
∴ N = 32 × 0.50 = 16
Hence, this percentage is 16, based on the entire sample of soil.
Example 3.12: In a hydrometer analysis, the corrected hydrometer reading in a 1000 ml
uniform soil suspension at the start of sedimentation was 28. After a lapse of 30 minutes, the
corrected hydrometer reading was 12 and the corresponding effective depth 10.5 cm. The spe-
cific gravity of the solids was 2.70. Assuming the viscosity and unit weight of water at the
temperature of the test as 0.001 N-s/m^2 and 9.8 kN/m^3 respectively, determine the weight of
solids mixed in the suspension, the effective diameter corresponding to the 30-min. reading
and the percentage of particles finer than this size.
The corrected hydrometer reading initially, Rhi = 28
∴γi = 0.01028 N/cm^3
But, by Eq. 3.29,
γi = γw + [G – 1)/G] W/V
Substituting,
0.01028 =^001
27 1
2 7 1000
. (. )
.
+
−
× W
whence W =
0 028 2 7
17
..
.
×
N = 0.445 N