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an engineering geological characterisation of tropical clays - GBV

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183<br />

Black <strong>clays</strong>; plasticity index/ linear shrinkage<br />

60<br />

n = 36<br />

Plasticity index PI (%)<br />

55<br />

50<br />

45<br />

40<br />

35<br />

PI = 1,89LS<br />

PI = 1,87LS<br />

less th<strong>an</strong> 0,50m depth<br />

0,50m depth <strong>an</strong>d<br />

greater<br />

Linear (less th<strong>an</strong><br />

0,50m depth)<br />

Linear (0,50m depth<br />

<strong>an</strong>d greater)<br />

30<br />

20 25 30<br />

Linear shrinkage LS (%)<br />

Figure 10.1. Correlation <strong>of</strong> laboratory measured values <strong>of</strong> plasticity index <strong>an</strong>d linear<br />

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

From the diagram, the plasticity index <strong>of</strong> black <strong>clays</strong> could be approximately estimated by the<br />

relationship<br />

<strong>an</strong>d<br />

PI = 1,87*LS (10.2)<br />

PI = 1,89*LS (10.3)<br />

for soil depths <strong>of</strong> less th<strong>an</strong> 0,50m <strong>an</strong>d those <strong>of</strong> depths <strong>of</strong> 0,50m <strong>an</strong>d greater, respectively. The<br />

two relationships derived for the two depth intervals are practically identical, <strong>an</strong>d this serves<br />

to support <strong>an</strong>d confirm <strong>an</strong> earlier suggestion that the black <strong>clays</strong> <strong>of</strong> the study area are<br />

homogeneous in their <strong>engineering</strong> character. On the average therefore, the plasticity index <strong>of</strong><br />

the whole soil thickness <strong>of</strong> black <strong>clays</strong> across the study area could be estimated from the<br />

average relationship <strong>of</strong><br />

PI = 1,88*LS (10.4)<br />

Calculated values <strong>of</strong> plasticity index, PILS, as estimated from laboratory measured values <strong>of</strong><br />

linear shrinkage, LS, using the above new relationship in Equation (10.4) are presented in<br />

Table (10.1), both for depths <strong>of</strong> less th<strong>an</strong> 0,50m <strong>an</strong>d those <strong>of</strong> 0,50m <strong>an</strong>d greater. A<br />

comparison <strong>of</strong> the so calculated values <strong>of</strong> plasticity index (PILS) with plasticity index values<br />

measured in the laboratory (PI meas.) reveals a generally close agreement between the two sets<br />

<strong>of</strong> data. The maximum <strong>an</strong>d minimum values as well as the medi<strong>an</strong>, mode <strong>an</strong>d me<strong>an</strong> values<br />

obtained for the two sets <strong>of</strong> data are identical at each one <strong>of</strong> the two depth intervals. This<br />

implies that Equation (10.4) above is a better <strong>an</strong>d preferred estimator for the plasticity index<br />

<strong>of</strong> black <strong>clays</strong> th<strong>an</strong> the British st<strong>an</strong>dard relationship <strong>of</strong> Equation (10.1). In addition, values <strong>of</strong>

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