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an engineering geological characterisation of tropical clays - GBV

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134<br />

Black <strong>clays</strong><br />

0,45<br />

0,43<br />

n = 6<br />

Compression index Cc<br />

0,41<br />

0,39<br />

0,37<br />

0,35<br />

0,33<br />

0,31<br />

0,29<br />

Cc = 0,0099(122-LL)<br />

R 2 = 0,73<br />

Cc vs LL<br />

0,27<br />

0,25<br />

75 80 85 90 95<br />

Liquid limit LL (%)<br />

Figure 7.23. Correlation between laboratory determined liquid limits <strong>an</strong>d<br />

compression indices for black <strong>clays</strong>.<br />

Black <strong>clays</strong> <strong>an</strong>d red soils<br />

Compression index Cc<br />

0,5<br />

0,4<br />

0,3<br />

0,2<br />

0,1<br />

0<br />

n = 9<br />

Cc = 0,0016(308-LL)<br />

R 2 = 0,34<br />

Cc vs LL<br />

0 20 40 60 80 100<br />

Liquid limit, LL (%)<br />

Figure 7.24. Correlation between laboratory determined liquid limits <strong>an</strong>d<br />

compression indices for black <strong>clays</strong> <strong>an</strong>d red soils.<br />

Calculated values <strong>of</strong> compression index for black <strong>clays</strong>, cc(b), as well as for combined black<br />

<strong>clays</strong> <strong>an</strong>d red soils, cc(br), as derived from laboratory measured liquid limits using the<br />

relationships <strong>of</strong> Equations (7.47 & 7.48) are presented in Table (7.16); alongside laboratory<br />

determined compression indices, cc. The strength <strong>of</strong> correlation between so calculated <strong>an</strong>d<br />

laboratory measured compression indices are strong (R = 0,85) for the black <strong>clays</strong> alone; <strong>an</strong>d<br />

only moderate (R = 0,58) for combined black <strong>clays</strong> <strong>an</strong>d red soils. However, values <strong>of</strong><br />

compression indices calculated from laboratory liquid limits using Skempton´s relationship,<br />

i.e. ( Cc(sk) = 0,009(LL-10) are generally overestimated with respect to laboratory determined<br />

compression indices for black <strong>clays</strong> (Table 7.16). The overestimation could be accounted for

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