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Figure 4.4 Cohesion of fibrous, hemic and sapric peats ( after Kazemian et al ., 2012(b)).
Table 4.2 Vane shear strength of peat ( after Al-Raziqi et al ., 2003).
Field
Moisture
Organic
Liquid
von
vane shear
content
content
limit
Post
strength
Location
(%)
(%)
(%)
scale
(kPa)
Banting, Selangor
211
85
294
H1
10-12
195
79
219
H2
11
832
84
361
H5
10
219
94
316
H6
7-9
225
85
166
H8
4
802
83
362
H10
4-6
Kg. Jawa, Klang
214
79
180
H3
11
225
84
325
H6
8
618
88
368
H8
5
Kg. Jawa, Klang
680
85
298
H3
10-15
747
93
352
H5
5-10
720
83
282
H7
9-12
Dengkil, N. Sembilan (West Malaysia)
246
98
305
H2
9-13
301
98
335
H5
6-10
786
83
377
H8
3-6
Berengbengkel, Central Kalimantan
467-1224
41-99
-
H2-H5
6-17
4.3 VANE SHEAR STRENGTH
Table 4.2 shows the vane shear strength of various tropical peats obtained from West
Malaysia using the small field vane shear test. The undrained shear strength of the peat
soil ( S u ) is in the range 3-15 kPa, which is generally much lower than that of mineral
soils (soft clays).
 
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