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

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Chapter 2 SAMPLING AND SAMPLING<br />

DISTURBANCE<br />

Figure 2.1 Effects of<br />

Tube Sampling Disturbance of Lightly Overconsolidated Natural (‘Structured’)<br />

Clay on: (a) Stress Path <strong>and</strong> Strength during Undrained Triaxial Compression<br />

(b)<br />

One-Dimensional Compressibility during Oedometer Testing<br />

(II)<br />

Compressibilit<br />

ty <strong>and</strong> Stiffness<br />

The effects of sampling on compressibility (as measured in the oedometer, for example) are difficult<br />

to assesss because of bedding effects, particularly in heavily overconsolidated clays. The use of local<br />

axial strain measurement on triaxial specimens during the past decade has produced new <strong>and</strong> more<br />

reliable stiffness dataa than can normally be expected from<br />

routine one-dimensional consolidation<br />

tests, It is now known that the measured small-strain stiffnesses of clays, most relevant to many<br />

geotechnical engineering problems, is for a given clay approximately<br />

linearly proportional to the<br />

mean effective stress at the time of measurement. This means that changes in effective stress as<br />

a<br />

result of disturbance are directly translated into proportional changes in measured soil stiffness.<br />

Because of the growing appreciation of the influence of bedding <strong>and</strong> effective stress changes on<br />

measured stiffness, it<br />

has becomee common practice in the<br />

UK to adopt<br />

laboratory methods which<br />

will avoid<br />

these problems. In heavily overconsolidated clays, small-strain stiffness is often normalized<br />

with respect to the mean effectivee stress at the start of shear (p’o=(σ’1+σ’2+σ’3)/3). Alternatively,<br />

the stiffness of bonded soils is perhaps more appropriately normalized with respect to undrained<br />

2-8<br />

March 2009

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