Geoscience Reference
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Table 4.1 Laboratory shear box test results of peats ( after Al-Raziqi et al ., 2003).
Angle of
Moisture
Organic
Liquid
von
internal
content
content
limit
Post
Cohesion
friction
Location
(%)
(%)
(%)
scale
(kPa)
(degree)
Banting, Selangor
211
85
294
H1
9-11
9-20
195
79
219
H2
6-11
9-16
832
84
361
H5
8-10
7-10
219
94
316
H6
11-12
9-12
225
85
166
H8
8-12
6-11
Kg. Jawa, Selangor
215
78
180
H3
10-12
6-14
209
89
325
H6
12-14
7-25
786
85
368
H8
7-11
8-13
Kg. Jawa, Selangor
680
85
298
H3
11-12
10-15
747
93
352
H5
10-12
5-10
720
83
282
H7
7-9
9-12
Dengkil, N. Sembilan (west Malaysia)
246
98
305
H2
13-17
3-12
301
98
335
H5
11
13-15
786
83
377
H8
8-9
12-20
Figure 4.3 Friction angle of fibrous, hemic and sapric peats ( after Kazemian et al ., 2012(a)).
so as to have all three varieties: fibrous, hemic and sapric peats. The organic con-
tents were reported to be 94%, 81% and 75% for fibrous, hemic and sapric peats,
respectively. Similarly, the fibre contents were reported to be 79%, 53% and 31%
respectively. Further, Kazemian et al. (2012) have also presented the cohesion of vari-
ous peats (Figure 4.4). The strength parameters of fibrous peat are higher than those
of hemic and sapric peats, as these are affected by the content of fibres, as stated by
Edil (1997).
 
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