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an engineering geological characterisation of tropical clays - GBV

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170<br />

1°19´S 4000<br />

Pr<strong>of</strong>ile dist<strong>an</strong>ce (m) Pr<strong>of</strong>ile dist<strong>an</strong>ce (m)<br />

3000<br />

2000<br />

West<br />

1000<br />

1°21.5´S<br />

1°19´S 4000<br />

3000<br />

2000<br />

West<br />

1000<br />

% clay variation (< 0,5 m)<br />

0<br />

0 1000 2000 3000 4000 5000 6000 7000 8000 9000 10000<br />

36°49´E<br />

South Pr<strong>of</strong>ile dist<strong>an</strong>ce (m)<br />

36°55´E<br />

% clay variation (> 0,5 m)<br />

%clay<br />

35<br />

34<br />

33<br />

32<br />

31<br />

30<br />

29<br />

28<br />

27<br />

26<br />

25<br />

24<br />

23<br />

22<br />

21<br />

20<br />

19<br />

18<br />

17<br />

16<br />

15<br />

14<br />

1°21.5´S<br />

0<br />

0 1000 2000 3000 4000 5000 6000 7000 8000 9000 10000<br />

36°49´E<br />

South<br />

Pr<strong>of</strong>ile dist<strong>an</strong>ce (m) 36°55´E<br />

38<br />

36<br />

34<br />

32<br />

30<br />

28<br />

26<br />

24<br />

22<br />

20<br />

18<br />

16<br />

14<br />

Figure 8.11. Contour maps showing distribution <strong>an</strong>d variation <strong>of</strong> %clay in black <strong>clays</strong>.<br />

40<br />

% clay<br />

The variation <strong>of</strong> percentage fines is also identical at the two depth intervals, in terms <strong>of</strong><br />

maximum <strong>an</strong>d minimum values <strong>of</strong> 96% <strong>an</strong>d 74% (r<strong>an</strong>ge: 22%); <strong>an</strong>d 93% <strong>an</strong>d 72% (r<strong>an</strong>ge:<br />

21%), respectively; as well as medi<strong>an</strong>, mode <strong>an</strong>d me<strong>an</strong> values <strong>of</strong> about 90%. St<strong>an</strong>dard<br />

deviations registered for the data sets at the two depth intervals are also <strong>of</strong> the same order <strong>of</strong><br />

magnitude, i.e. 3,81 <strong>an</strong>d 4,50, respectively. The variation along field pr<strong>of</strong>iles at the two depth<br />

intervals is also illustrated in Figure (8.12) <strong>an</strong>d a contoured representation in Fig.(8.13).

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