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an engineering geological characterisation of tropical clays - GBV

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112<br />

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

Cohesion c´ (kN/m²)<br />

60,00<br />

50,00<br />

40,00<br />

30,00<br />

20,00<br />

10,00<br />

0,00<br />

n = 41<br />

Cohesion vs Cr<br />

1 1,1 1,2 1,3 1,4 1,5 1,6<br />

Rel. Consistency, Cr<br />

Figure 7.6c. Correlation between cohesion (c´ ) <strong>an</strong>d relative consistency, Cr,<br />

<strong>of</strong> black <strong>clays</strong>.<br />

A poor correlation (R = 0,30) is obtained by relating shear <strong>an</strong>gles <strong>an</strong>d plasticity indices <strong>of</strong> the<br />

<strong>clays</strong> (Fig. 7.7a). A slight improvement in correlation is obtained by plotting the shear <strong>an</strong>gles<br />

against the reciprocal <strong>of</strong> plasticity indices (Fig. 7.8a); but once again, the strength <strong>of</strong><br />

correlation is still low (R = 0,32).<br />

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

Angle <strong>of</strong> shear resist<strong>an</strong>ce<br />

φ´ (°)<br />

35<br />

n = 41 R² = 0,09<br />

30<br />

25<br />

20<br />

15<br />

10<br />

35,015 40,015 45,015 50,015 55,015 60,015<br />

Plasticity index PI (%)<br />

Shear <strong>an</strong>gle vs PI<br />

Figure 7.7a. Correlation between <strong>an</strong>gle <strong>of</strong> shear resist<strong>an</strong>ce (φ´ ) <strong>an</strong>d plasticity<br />

index (PI) <strong>of</strong> black <strong>clays</strong>.

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