an engineering geological characterisation of tropical clays - GBV
an engineering geological characterisation of tropical clays - GBV
an engineering geological characterisation of tropical clays - GBV
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strongly suggest that the whole soil thickness <strong>of</strong> black <strong>clays</strong> <strong>of</strong> the current study area is more<br />
or less homogenous <strong>an</strong>d uniform in terms <strong>of</strong> linear shrinkage <strong>an</strong>d, possibly, other index <strong>an</strong>d/or<br />
<strong>engineering</strong> properties.<br />
Linear shrinkage values obtained for the red soils are comparatively low <strong>an</strong>d r<strong>an</strong>ge from 10-<br />
11%.<br />
8.5 Free swell<br />
The distribution <strong>of</strong> free swell values along the five field pr<strong>of</strong>iles in this study is presented in<br />
Figure (8.9). Pr<strong>of</strong>iles A, B, C, D <strong>an</strong>d E show free swell values <strong>of</strong> 115-135%, 120-145%, 105-<br />
130%, 110-130 <strong>an</strong>d 120-135% for depths <strong>of</strong> less th<strong>an</strong> 0,50m concentrated about a me<strong>an</strong> value<br />
<strong>of</strong> 126%; <strong>an</strong>d 100-145%, 120-145%, 110-145%, 130-145% <strong>an</strong>d 120-145% for depths 0f 0,5m<br />
<strong>an</strong>d over, concentrated about a me<strong>an</strong> value <strong>of</strong> 132%, respectively. The complete set <strong>of</strong> data is<br />
given in Table (8.1).<br />
Distribution <strong>of</strong> free swell values at a depth <strong>of</strong> less th<strong>an</strong> 0,50m across the study area is<br />
characterised by minimum <strong>an</strong>d maximun values <strong>of</strong> 105% <strong>an</strong>d 145% respectively, giving a<br />
r<strong>an</strong>ge <strong>of</strong> 40%, medi<strong>an</strong> <strong>an</strong>d mode <strong>of</strong> 125%, me<strong>an</strong> <strong>of</strong> 126% as well as a st<strong>an</strong>dard deviation <strong>of</strong><br />
8,26 <strong>an</strong>d vari<strong>an</strong>ce <strong>of</strong> 68,25.<br />
Free swell variation; < 0,50m depth<br />
Free swell (%)<br />
160<br />
140<br />
120<br />
100<br />
80<br />
60<br />
40<br />
20<br />
0<br />
0 2000 4000 6000 8000 10000 12000<br />
Dist<strong>an</strong>ce along pr<strong>of</strong>ile (m)<br />
Pr<strong>of</strong>ile A<br />
Pr<strong>of</strong>ile B<br />
Pr<strong>of</strong>ile C<br />
Pr<strong>of</strong>ile D<br />
Pr<strong>of</strong>ile E<br />
Figure 8.9a. Free swell variation across the study area at depths <strong>of</strong> less th<strong>an</strong><br />
0,5m (north-south dist<strong>an</strong>ce: 4000 m).<br />
On the other h<strong>an</strong>d, black <strong>clays</strong> at depths <strong>of</strong> 0,50m <strong>an</strong>d over exhibit free swell values <strong>of</strong><br />
between 100% <strong>an</strong>d 145% with a r<strong>an</strong>ge <strong>of</strong> 45%, across the study area. A medi<strong>an</strong> <strong>an</strong>d mode <strong>of</strong><br />
135%, me<strong>an</strong> <strong>of</strong> 132%, st<strong>an</strong>dard deviation <strong>of</strong> 11,33 <strong>an</strong>d vari<strong>an</strong>ce <strong>of</strong> 128,28 were also<br />
calculated for the depth.