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an engineering geological characterisation of tropical clays - GBV

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127<br />

Cumulative log-time/settlement<br />

curves: black <strong>clays</strong> (SA2-70cm)<br />

Cumulative log-time/settlement<br />

curves: Red soils (RD1-100cm)<br />

cumulative settlement (mm)<br />

time - minutes (log scale)<br />

0,1 10,0 1000,0 100000,0<br />

0<br />

0,2<br />

0,4<br />

0,6<br />

0,8<br />

1<br />

1,2<br />

1,4<br />

1,6<br />

1,8<br />

2<br />

2,2<br />

cumulative settlement (mm)<br />

0,100 10,000 1000,000<br />

0,000<br />

1,000<br />

2,000<br />

3,000<br />

4,000<br />

5,000<br />

time - minutes (log scale)<br />

100000,0<br />

00<br />

2,4<br />

2,6<br />

6,000<br />

2,8<br />

3<br />

Fig. 7.16. Conventional log-time/settlement<br />

curves for black <strong>clays</strong> during loading<br />

<strong>an</strong>d unloading stages.<br />

7,000<br />

Fig. 7.17.Unconventional log-time/settlement<br />

curves for red soils during loading<br />

<strong>an</strong>d unloading stages.<br />

Results <strong>of</strong> voids ratio ch<strong>an</strong>ge <strong>of</strong> soils during loading <strong>an</strong>d unloading stages are summarised in<br />

the form <strong>of</strong> voids ratio/ log pressure (e/log p) curves as shown in Figure (7.18). The curves<br />

for the red soils are generally placed higher up the diagram, implying higher voids ratios <strong>an</strong>d<br />

porosities. On the other h<strong>an</strong>d, e/log p curves for black <strong>clays</strong> occupy lower positions on the<br />

diagram due to their relatively lower voids ratios <strong>an</strong>d porosities. As a result, red soils would<br />

be expected to be more compressible th<strong>an</strong> the black <strong>clays</strong> over the same loading r<strong>an</strong>ge. In<br />

addition, unloading portions <strong>of</strong> the curves are more or less flat <strong>an</strong>d/ or horizontal for the red<br />

soils, while those for black <strong>clays</strong> are relatively steeper. This serves to show once again the<br />

higher potential swelling capabilities <strong>of</strong> black <strong>clays</strong> relative to those <strong>of</strong> red soils.

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