DMOOMu
phs.
tion
of
aphs
ent,
at
ure.
in a
in
lass
the
the
the
phs,
the
ixed
onal
be
may
at
not
the
to
for
thod
hich
the
ons.
sted
can
nent
ater
ject
able
used
ents
s or
very
3-RECORDING THE DISPLACEMENT FIELD
An accurate and complete photographic
record of the displacement field should
fulfill the following conditions:
-A set of static reference marks should be
recorded in the photographs. This is
necessary to determine the datum level for
height measurement in the stereo image. In
the present investigation an orthogonal
grid was scored for this purpose on the
inside face of the glass side of the box.
This grid was formed of equal squares 25mm
X 25 mm.
-The camera used should have a good
quality lens capable of producing sharp
negatives so that the objects in the pair
of photos are easily fused when viewed
stereoscopically. In displacement field
work the overlap is 100% and the movement
of particles between photos will be
recorded through the same part of the
lens. Any distortion by the lens will
produce similar errors in succesive photos
and the measurement of the parallaxes
between points will not be significantly
in error. For a high degree of accuracy a
plate camera capable of taking glass
plates or large size negatives is
preferable. In the present study a
Hasselbad 500 LM camera fitted with an
80mm lens, capable of producing a SS5mm by
55mm negative, was used. A clear relief
image is enhanced if the photos contain
contrasts between adjacent objects.
Careful illumination of the model can
improve the texture of the surface and the
quality of the photos. Two floodlights
were positioned at an angle of 45° with
respect to the camera sand bed axis. The
camera had a black screen (with only the
lens protruding) to minimize unwanted
reflections in the glass window. The
camera position was approximately 0.5m
from the edge of the model.
-The camera should be fixed in position
relative to the stationary parts of the
model so that the optical axis is
perpendicular to the plane of
displacements. If the camera moves
between photos this will become apparent,
when a pair of photos is viewed
stereoscopically, by differences in
parallax between points in the model which
are known not to have moved. Andrawes
(1976) stated that the error introduced by
a tilt of the camera of 2? from the
perpendicular will introduce an average
error of about t1% in the value of the
contours. In this study the camera has
been mounted on a rigid pedestal and the
pictures were taken with the help of a
remote control device so that the camera
was not touched during the test.
4-MEASUREMENT OF DISPLACEMENT
The major movements in the anchor model
occur parallel to the vertical axis and
therefore the negatives were set up in the
instrument so that the vertical axis shown
in the negatives was parallel to the x
axix of the instrument. This dramatized
the apparent relief when the pair was
viewed stereoscopically. In the negatives
the grid appears as a distinct white
colour "datum" surface from where the
measuring mark can be driven towards the
elevated sand particles. The measurements
were made point by point along steep
slopes, peaks, depression and breaks in
the relief. If the whole displacement
field is to be reproduced there must be an
interpolation between the measured points.
It was found that measurements at 500
points gave good reproduction of the
images viewed.
S-COMPUTER PROCESSING OF DATA
The author has developed a computer
program which processed all the data given
by the stereocomparator and plotted all
the required diagrams using the UNIRAS
package. The measurements made in the
stecometer are from points which are
randomly spaced throughout the field.
These measurements are used by the program
to calculate the values of the vertical
and horizontal displacements which occur
in the field at the position of the nodes
of a regular grid which covers the whole
field. The fields of the vertical and
horizontal displacement components are
then plotted. The displacement component
values are combined to give the resultant
displacements at the nodes of the grid and
they are also used to derive the strains
throughout the field.
Input Data from
Stecometer
Pre-process Data
Transtorm Coordinates
Calculate Vertical
& Horizontal Displacement
|
Calculate Displacement
Resultant
& Strain Values
Plotting of Contours
of Vertical and Horizontal
Displacement
Plotting of Displacement
Field
Plotting of Contours of
Maximum Shear Strains
Fig. 1 Flow Chart