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now all fall close to a single curved line. The data are plotted to logarithmic scales in
Fig. 10.22(b). They are close to a straight line with B in Eq. (10.14) and, scaling from
the diagram, B
=
0.5.
Example 10.3: Dilation and equivalent state Table 10.3 shows the data for the peak
states for the set of shear tests given in Tables 10.1 and 10.2. The critical friction angle
is
φ c and the angle of dilation
is given by Eq. (10.19). Values for e λ are calculated
from Eq. (9.7) and Fig. 10.23(a) shows the variation of
ψ
φ + ψ
with e λ . The state
parameter S v is calculated from Eq. (9.19) with e =
2.17 and Fig. 10.23(b) shows the
variation of peak stress ratio with S v .
Reference
Schofield, A. N. (1980) 'Cambridge geotechnical centrifuge operations', Geotechnique , 30 ,3,
227-268.
Further reading
Atkinson, J. H. and P. L. Bransby (1978) The Mechanics of Soils , McGraw-Hill, London.
Muir Wood, D. M. (1991) Soil Behaviour and Critical State Soil Mechanics , Cambridge
University Press, Cambridge.
Schofield, A. N. and C. P. Wroth (1968) Critical State Soil Mechanics , McGraw-Hill, London.
Taylor, D. W. (1948) Fundamentals of Soil Mechanics , Wiley, New York.
 
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