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an engineering geological characterisation of tropical clays - GBV

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58<br />

Chapter 6<br />

Chemical <strong>an</strong>d mineralogical <strong>an</strong>alyses<br />

6.1 Introduction<br />

A number <strong>of</strong> soil samples previously collected from the field were subjected to laboratory<br />

chemical <strong>an</strong>d mineralogical <strong>an</strong>alyses <strong>an</strong>d/ or studies using the X-ray fluorescence (XRF), X-<br />

ray diffraction (XRD) <strong>an</strong>d sc<strong>an</strong>ning electron microscope (SEM) techniques.<br />

6.2 X-ray fluorescence (XRF) studies<br />

6.2.1 Scope <strong>an</strong>d method<br />

Chemical <strong>an</strong>alyses were carried out using X-ray fluorescence technique to determine the<br />

percentage composition <strong>of</strong> major oxides in the clay soils, <strong>an</strong>d include SiO2, Al2O3, Fe2O3,<br />

FeO, MgO, CaO, MnO, Na2O, K2O, TiO2, P2O5 <strong>an</strong>d SO4. Percentage content <strong>of</strong> F, Cl, S<br />

<strong>an</strong>d Cr, as well as losses on ignition were also determined. The <strong>an</strong>alysis results have been<br />

useful in computing mineral contents in the tested soils (according to Olphen <strong>an</strong>d Fripiat,<br />

1979), especially where direct measurement <strong>of</strong> mineralogical compositions, such as kaolinite<br />

in red soils, has proved difficult.<br />

A PW-1480 (Rh 100kV LiF220 Ge111 T1AP) X-ray spectrometer <strong>an</strong>d a shale (<strong>clays</strong>tone)<br />

st<strong>an</strong>dard were employed in the XRF <strong>an</strong>alysis. Preparation <strong>of</strong> test specimens involved mixing<br />

<strong>of</strong> Hoechst wax (as diluent) with soil sample at a ratio <strong>of</strong> 1:5 to make a homogenous mixture.<br />

6.2.2 Results<br />

Results <strong>of</strong> chemical <strong>an</strong>alyses obtained for the soils in this study are presented in Table 6.1 for<br />

red soils <strong>an</strong>d Table 6.2 for black <strong>clays</strong>.<br />

Table 6.1. Results <strong>of</strong> chemical <strong>an</strong>alyses <strong>of</strong> red soils obtained in this study.<br />

% content <strong>of</strong>: Rd1-30cm Rd1-100cm Rd1-200cm Rd1-400cm<br />

SiO2 47,50 47,10 47,20 47,6<br />

Al2O3 32,20 33,40 33,20 33,30<br />

Fe2O3 15,30 15,50 15,50 15,20<br />

FeO - - - -<br />

BaO 0,062 0,061 0,071 0,064<br />

MgO 0,12 0,097 0,14 0,13<br />

CaO 0,26 0,24 0,16 0,26<br />

Na2O ‹ ‹ ‹ ‹<br />

K2O 0,96 0,66 0,68 0,60<br />

P2O5 0,19 0,086 0,096 0,062<br />

ZrO2 0,37 0,37 0,37 0,36<br />

TiO2 1,57 1,51 1,51 1,46<br />

MnO 0,96 0,53 0,61 0,52<br />

Loss on ignition - - - -<br />

Total 99,49 99,55 99,54 99,56<br />

Rd1-30cm, Rd1-100cm, Rd1-200cm & Rd1-400cm are red soil samples.

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