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During each test a sequence of eight
photographs was taken, the first prior to
pushing, the remainder at approximately
1.0 mm upward displacement interval. A
typical load versus displacement curve is
given in figure 3. It shows a smooth peak
followed by a softening stage, the numbers
on the curve are the serial numbers of the
photographs. The stereocomparator used
in . this study was a Zeiss Jena Stecometer
type C.
8-DISCUSSION & CONCLUSION
In this study, the sand used was a uniform
subrounded sand from Leighton Buzzard.
Tests were performed at a relative density
(I/D) of 75% anda depth/diameter (D/B)
ratio of 4. When the anchor is subjected
to loading the load is transmitted to the
sand surrounding it. The deformations
occuring in the sand were observed and
recorded. Figures 4 to 7? show the
displacements and strains for one
increment of the applied load. Thev show
the zones of the bed that responded to the
applied load. It should be noted that
displacement contours are given in mms and
maximum strain contours in percentages.
100 120 140 160
mm
FIG. 4 : CONTOURS OF VERTICAL DISPLACEMENTS IN
LEIGHTON BUZZARD SAND,
D/B=4. ID = 75%, 9 = 27 mm.
T I [
100 120 140 160
mm
FIG.5: CONTOURS OF HORIZONTAL DISPLACEMENTS IN
LEIGHTON BUZZARD SAND,
BiB=4, 10=75%,
5 = 2.7 mm.
For a vertical displacement of 2.7 mm, it
can be seen that the zone of sand
responding to this increment of load
extends approximately from 0.125 B to 2.0
B to the side of the plate anchor and a
clear discontinuity of displacements can
be seen in figure 6. The vertical
displacement diminishes as the distance
above the plate increases. The horizontal
displacements are insignificant and occur
mainly above the side of the plate. It
was observed that it this stage the sand
has begun to fall into the cavity left
below the plate anchor as it rises. The
shear has developed and is extending in a
generally vertical direction upward from
the edge of the plate anchor. The
immedi ate effect of this propagation is
depicted in figure 7. In this case, the
shape of the failure surface is defined by
the shape of the boundary of the disturbed
zone of sand (i.e. a frustrum of cone).
The salient observation drawn from this
study is that the pseudo stereo-
photogrammetry technique can yield
accurate measurements and it is possible
by measuring both the vertical and
horizontal displacements within the sand
bed to establish the relative displacement
occuring throughout the bed for any
increment of displacement of the anchor.
It is therefore possible to build up
information on displacements in the sand
bed increment by increment throughout the
loading and displacement of the anchor.