an engineering geological characterisation of tropical clays - GBV
an engineering geological characterisation of tropical clays - GBV
an engineering geological characterisation of tropical clays - GBV
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Table 10.2. Calculated <strong>an</strong>d laboratory measured values <strong>of</strong> plasticity index <strong>of</strong> red soils.<br />
Soil type Depth (m) Sample No. LS (%) PI meas. (%) PIBS (%) PILS (%)<br />
0,30 Rd1-30cm 10 18 21 18<br />
Red soils 1,00 Rd1-100cm 11 21 23 20<br />
2,00 Rd1-200cm 11 20 23 20<br />
4,00 Rd1-400cm 11 18 23 20<br />
0,30 Rd2-30cm 10 19 21 18<br />
1,00 Rd2-100cm 11 22 23 20<br />
2,00 Rd2-200cm 11 21 23 20<br />
4,00 Rd2-400cm 11 19 23 20<br />
max 11 22 23 20<br />
Statistical min 10 18 21 18<br />
<strong>an</strong>alysis r<strong>an</strong>ge 1 5 2 2<br />
medi<strong>an</strong> 11 20 23 20<br />
mode 11 #NV 23 20<br />
me<strong>an</strong> 11 20 23 20<br />
std 0,46 1,62 0,99 0,85<br />
var 0,21 2,63 0,97 0,72<br />
cov 0,76 0,65<br />
correlation 0,54 0,54<br />
as obtained for the black <strong>clays</strong> in this study at depths <strong>of</strong> less th<strong>an</strong> 0,50m as well as those at<br />
0,50m <strong>an</strong>d greater, are given in Table (10.1).<br />
Calculated values <strong>of</strong> plasticity index, PI(BS), as estimated from laboratory determined linear<br />
shrinkage values using the British St<strong>an</strong>dard relationship (BS 1377: 1967), i.e.<br />
PI = 2,13 * LS ( derivation based on British soils) (10.1)<br />
are also included in the table for the two depth intervals. The calculated plasticity index<br />
values are observed to be overestimated with respect to the laboratory determined values for<br />
both the two depth intervals. A comparison <strong>of</strong> the respective maximum <strong>an</strong>d minimum values<br />
as well as the medi<strong>an</strong>, mode <strong>an</strong>d me<strong>an</strong> values <strong>of</strong> calculated <strong>an</strong>d measured plasticity indices<br />
further indicates <strong>an</strong>d confirms <strong>an</strong> overestimation <strong>of</strong> the former with respect to the latter (Table<br />
10.1). The overestimation could be attributed to the generally higher org<strong>an</strong>ic content <strong>of</strong><br />
<strong>tropical</strong> black <strong>clays</strong> which tends to inhibit <strong>an</strong>d/ or suppress their plasticity to some degree.<br />
The coefficient <strong>of</strong> variation (covari<strong>an</strong>ce) with respect to the calculated <strong>an</strong>d measured values<br />
are 0,57 <strong>an</strong>d 3,23 for the two depth intervals, respectively. The st<strong>an</strong>dard deviation <strong>an</strong>d<br />
vari<strong>an</strong>ce for the calculated <strong>an</strong>d measured plasticity values are in close agreement <strong>an</strong>d more or<br />
less <strong>of</strong> the same order <strong>of</strong> magnitude in each case, implying a similar form <strong>an</strong>d/ or mode <strong>of</strong><br />
distribution <strong>an</strong>d variation across the study area.<br />
A correlation <strong>of</strong> laboratory measured values <strong>of</strong> plasticity index <strong>an</strong>d linear shrinkage is<br />
presented diagrammatically in Fig. (10.1).