05.03.2013 Views

A Self-Learning Manual - Institution of Engineers Mauritius

A Self-Learning Manual - Institution of Engineers Mauritius

A Self-Learning Manual - Institution of Engineers Mauritius

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

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 />

marine fill is lower.<br />

8. Why are observed settlements in reclamation normally larger than<br />

calculated? (R6)<br />

Settlement in reclamation area occurs as a result <strong>of</strong> primary consolidation<br />

(i.e. by dissipation <strong>of</strong> excess pore water pressure) and secondary<br />

compression which involves creep <strong>of</strong> soils. Creep <strong>of</strong> soils occurs by<br />

viscous squeezing out <strong>of</strong> absorbed water in double layers <strong>of</strong> clay particles<br />

and rearrangement <strong>of</strong> clay particles under loading.<br />

In the calculation <strong>of</strong> settlement in reclamation, there are generally two<br />

methods available. The first method assumes that creep occurs during the<br />

process <strong>of</strong> primary consolidation, which appears to be logically correct. On<br />

the other hand, the second method assumes that creep <strong>of</strong> soils occurs<br />

after primary consolidation and hence at the end <strong>of</strong> consolidation period<br />

the calculation settlement is equal to primary consolidation only without<br />

any consideration <strong>of</strong> creep effects. This method <strong>of</strong> settlement calculation is<br />

well adopted by most consulting firms and hence leads to underestimation<br />

<strong>of</strong> total settlement.<br />

9. Should silt curtain be designed to touch seabed?<br />

Silt curtains are impermeable vertical barriers extending from the seawater<br />

surface to their designed depths. The curtains are held in a vertical position<br />

by the carrier float on their top and a curtain weight at their bottom. A<br />

tension cable is designed at the carrier float to resist stresses incurred by<br />

currents. Moreover, the silt curtains are anchored to the seabed to hold<br />

them in the designed configuration.<br />

In essence, the depth <strong>of</strong> silt curtains should not be so long and touch the<br />

seabed because the bottom segment <strong>of</strong> the silt curtains would be trapped<br />

inside the newly accumulated sediment, thus resulting in the sinking <strong>of</strong> the<br />

curtain. It is difficult to remove these sunken curtains. Moreover, reversal<br />

tidal and current actions may cause movement <strong>of</strong> bottom region <strong>of</strong> curtains<br />

which stir up the settled suspensions and create additional turbidity.<br />

10. Vibrocompaction is carried out to loose sand after reclamation by<br />

filling sand. How to determine the in-situ density <strong>of</strong> filled sand? (R7)<br />

It is difficult to obtain undisturbed samples <strong>of</strong> sand to measure the in-situ<br />

density. The relative density <strong>of</strong> in-situ sand can be determined by<br />

179

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

Saved successfully!

Ooh no, something went wrong!