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Volume 6 – Geotechnical Manual, Site Investigation and Engineering ...

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Chapter 2 SAMPLING AND SAMPLING<br />

DISTURBANCE<br />

shear strength, although it may be<br />

difficult to determine the true in situ value of this. In situ stiffness<br />

can then be recovered<br />

if p’o(in situ) or cu(in situ) be estimated. In lightly overconsolidated natural<br />

clay Clayton et al. (1992) have shown, however, that even the careful reestablishment of in situ<br />

effective stress levels before shearing cannot fully recover the undisturbed stiffness behaviour of the<br />

soil.<br />

A 60% reduction in E u / p’ o (measured locally,<br />

<strong>and</strong> after re-establishment of in situ<br />

stresses) was<br />

obtained for the Bothkennar clay following tube sampling strain excursions of ±2% %, for example.<br />

The results of a literature survey<br />

by Hopper (1992) are shown in Fig. 2.2. Here the very severe<br />

effects of tube sampling (including<br />

the effects of borehole disturbance, <strong>and</strong> obtained<br />

by comparing<br />

test results from tube samples with<br />

those on block samples in the same soil type) can be seen.<br />

Figure 2.2 Influence of Tube<br />

Sampling Disturbance on<br />

Undrained Strength <strong>and</strong> Stiffness<br />

(From a Survey by Hopper 1992).<br />

March 2009<br />

2-9

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