PHOTOGRAM METRIC ENGINEERING
2
Professor Schwidefsky, in his paper, de
fined five steps of automation arranged in
order of increasing performance which may
generally be described as computers, analog-
to-digital and digital-to-analog converters,
signal orienters, signal correlators, and finally
form recognizers. Photogrammetric examples
of the first step are the classical stereoplotters
and the more recent analytical plotters, and
of the second step, automatic coordinato-
graphs. Equipment representing the third and
fifth steps exist only as experimental models;
but the fourth step is illustrated by several
instruments to be discussed in this paper, the
best known of which is the Stereomat.
Servo-Driven Plotting Table
An example of the judicious application of
new techniques to familiar problems is illus
trated in the paper of Professor C. Trom
betti, Instituto Geografico Militare, Florence,
entitled, “Drawing Tables Driven by Elec
tronic Servos for Analogical Photogram
metric Plotters.” In this development
synchro-transmitters are used to transfer X-
and T-movements from the plotter to
synchro-receivers on the independently
mounted plotting table. The plotting surface
of this table, the 030M, is exceptionally large,
being 200X150 square centimeters. In order
to avoid loss of transmission accuracy, a
double-speed synchro-transmission is em
ployed. Preliminary results showed that posi
tioning accuracy was well within allowable
map error, a result which could not be
achieved with any other type of servo sys
tem.
Differential Rectification
Another area which has received much
attention in recent times is the production of
orthophotographs. In a line map it is difficult
to present anywhere near the detail found
in an aerial photograph. As a working
plan many earth scientists find the rich detail
of aerial photography of special advantage.
When he begins to measure, however, he
quickly finds the differential scale relations in
tolerable. The first correction the photo-
grammetrist can offer is to correct the scale
errors produced by camera orientation.
Rectification of this type, however, ina plane
correction which will not remove the scale
errors resulting from terrain relief. This latter
correction requires some process of differential
rectification. Methods of achieving differ
ential rectification include zonal rectification,
the division of the terrain into polyhedral
surfaces, the French method of facets, the
Soviet method of the reversed terrain model,
and the combination of differential image
rectification with stereoscopic plotting.
The combination of differential rectifica
tion directly with stereoscopic plotting pro
vides a magnification change continuously
controlled by the stereoplotter. The first
suggestion of this approach came from Lac-
mann in 1931; however, his proposal was not
instrumented. As early as 1935 Gallus-Ferber
provided a typical example of what can be ac
complished by equipment of this type. More
recently, production instruments have been
developed in America under the name of
Orthophotoscope and in the Soviet Union as
the Slot-Rectifier FT-Shch 1.
In equipment of this type the model is pro
filed in parallel strips and the image from one
of the stereopairs is exposed differentially
through a slit. If the model is created in a
double-projection instrument, scale correc
tions are made by varying the projection
distance according to the scale on the profile.
(If an optical model, as such, does not exist,
as in the stereometer-type instruments to be
discussed later, then, scale and displacement
are determined by a computer.) The stereo
scopic profile method is employed in the Slot-
Rectifier, the American Orthophotoscope, and
in the Gigas-Zeiss Orthophotoscope.
T-64 Orthophotoscope
Significant changes made in the ortho
photoscope developed by the U. S. Geological
Survey have been summarized by Marvin B.
Scher in a paper entitled, “New Develop
ments in Orthophotography.” At the Ninth
Congress the cylindrical drum I960 Ortho-
photoscope was described. The new T-64,
shown in Figure 1, employs an inclined plane
as the film supporting platform. Critical
mechanical adjustments required in the
drum-type instrument dictated the return to
the flat platform. However, for operator
viewing, comfort and convenience the plat
form is tilted toward the operator approxi
mately 40 degrees from the horizontal plane.
In extending the area of coverage provided
by orthophotography, the U. S. Geological
Survey has produced orthophotomosaics.
Scaling and orientation of the individual
orthophotographs are accomplished by stereo
templet triangulation. Uniquely, the data re
quired for the stereotemplets can be derived
directly from the orthonegatives.