31.12.2013 Views

an engineering geological characterisation of tropical clays - GBV

an engineering geological characterisation of tropical clays - GBV

an engineering geological characterisation of tropical clays - GBV

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

141<br />

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

Swelling pressure SP (kPa)<br />

120<br />

n = 7<br />

100<br />

80<br />

60<br />

40<br />

20<br />

0<br />

10 15 20 25 30 35 40<br />

Natural moisture Wn (%)<br />

Wn vs SP<br />

Figure 7.33. Correlation between Wn <strong>an</strong>d SP.<br />

7.4.7.2 Swelling test<br />

Swelling is the increase in volume <strong>of</strong> a soil due to absorption <strong>of</strong> water within the voids when<br />

the applied stress is reduced. It is therefore the reverse <strong>an</strong>d opposite process <strong>of</strong> consolidation,<br />

<strong>an</strong>d occurs when overconsolidated <strong>clays</strong> are allowed free access to water (Nelson <strong>an</strong>d Miller,<br />

1992). In consolidation tests, swelling is represented by the unloading portion <strong>of</strong> the e/ log p<br />

curve (Fig. 7.18 ). The mech<strong>an</strong>ism <strong>of</strong> swelling is explained by <strong>an</strong> overconsolidated soil<br />

possessing high suction tensions within its skeleton on unloading, thereby drawing water into<br />

the voids. The resulting increase in volume <strong>of</strong> voids causes the soil to swell <strong>an</strong>d eventually<br />

disintegrate.<br />

Testing procedure involved use <strong>of</strong> same apparatus as in the st<strong>an</strong>dard oedometer consolidation<br />

test. However, the height <strong>of</strong> soil specimen was 3 mm less th<strong>an</strong> the height <strong>of</strong> consolidation<br />

ring; so that the specimen was laterally confined at all times during swelling. The space in the<br />

ring above test specimen was taken up by a flat metal disc <strong>of</strong> 3 mm thickness <strong>an</strong>d diameter<br />

about 1 mm less th<strong>an</strong> the internal diameter <strong>of</strong> ring. The specimen in the ring was weighed,<br />

assembled in oedometer cell <strong>an</strong>d mounted in the load frame <strong>of</strong> consolidation press. Initial<br />

height <strong>of</strong> specimen was given by height <strong>of</strong> ring less the average disc thickness.<br />

Swelling pressure, SP, was determined as described above. After establishment <strong>of</strong><br />

equilibrium, the swelling test was performed by unloading the specimen in stages from the<br />

swelling pressure, SP, as the starting point; <strong>an</strong>d by following <strong>an</strong> unloading sequence <strong>of</strong><br />

halving the loads at each successive decrement, i.e. 1/2SP, 1/4SP, 1/8SP, <strong>an</strong>d so on down to<br />

the smallest load required. Each unloading stage was maintained until equilibrium had been<br />

reached <strong>an</strong>d no further ch<strong>an</strong>ge in compression gauge reading was observed. During<br />

unloading, cumulative amount <strong>of</strong> swell (mm) undergone by the specimen for successive<br />

decrements <strong>of</strong> load was recorded by noting the ch<strong>an</strong>ge in compression gauge reading from its<br />

initial position.<br />

The cumulative swell (S mm) under each load decrement was recorded <strong>an</strong>d expressed as a<br />

percentage <strong>of</strong> the ultimate amount <strong>of</strong> swell (Smax mm) which was registered with specimen<br />

under zero load. Results <strong>of</strong> cumulative percentage swelling (S %) recorded against

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!