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A Self-Learning Manual - Institution of Engineers Mauritius

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A <strong>Self</strong>-<strong>Learning</strong> <strong>Manual</strong><br />

Mastering Different Fields <strong>of</strong> Civil Engineering Works (VC-Q&A Method) Vincent T. H. CHU<br />

Level Two (Advanced FAQs)<br />

Part II: Miscellaneous<br />

1. Does liquefaction occur to sand only? (M1)<br />

In liquefaction, the pore water pressure builds up steadily and eventually<br />

approaches a value equal to the confining pressure. In an earthquake,<br />

however, there is not enough time for the water in the pores <strong>of</strong> the soil to be<br />

squeezed out. Instead, the water is trapped and this avoids the soil<br />

particles from moving closer together. Consequently, this results in an<br />

increase in water pressure which reduces the contact forces between the<br />

individual soil particles, thereby s<strong>of</strong>tening and weakening the soil.<br />

Eventually, soils particles lose contact with each other and behave like a<br />

liquid.<br />

Hence, the type <strong>of</strong> soils which is susceptible to liquefaction is the one like<br />

sand whose resistance to deformation is mobilized by frictional forces<br />

between particles under confining pressure. In case the soil is fine grained,<br />

cohesive forces tends to develop between these fine particles and it is<br />

difficult to separate them. Therefore, sand with increasing content <strong>of</strong> fines<br />

tends to increase its resistance to liquefaction.<br />

The consequence <strong>of</strong> liquefaction is that the subsequent settlements after<br />

liquefaction may damage the overlying structures. Moreover, for sloping<br />

ground lateral flow may result which is undesirable. Liquefaction only<br />

occurs to saturated soils.<br />

2. What are the measures to reduce the effects <strong>of</strong> soil liquefaction?<br />

(M1)<br />

To reduce the effect <strong>of</strong> soil liquefaction, it is intended to reduce the pore<br />

water pressure induced during earthquake shaking. This can be achieved<br />

by providing better drainage in soils (e.g. wick drains, sand drains etc. )<br />

and densification <strong>of</strong> soils (e.g. vibr<strong>of</strong>lotation, dynamic compaction etc.).<br />

Liquefaction hazards can be reduced by improving the drainage ability <strong>of</strong><br />

the soil. If the pore water within the soil can drain freely, the build-up <strong>of</strong><br />

excess pore water pressure would be reduced accordingly.<br />

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