Full text: Proceedings, XXth congress (Part 7)

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International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004 
  
positioning technique has become to use in deformation 
measurements (Erol, 1999). 
GPS technique has benefits of high accuracy and simultaneous 
3-D positioning; however there are handicaps about vertical 
positioning using this technique. Because, the height 
component is the least accurately determined GPS coordinate, 
predominantly due to inherent geometric weakness and 
atmospheric errors (Featherstone et al., 1998; Celik et al., 
2001). 
Therefore, using GPS measurement technique in deformation 
measurements with millimeter level accuracy requires some 
special precautions that increase the measurement accuracy in 
GPS observables via eliminating or reducing some error sources 
such as using forced centering equipments, applying special 
measuring techniques like rapid static method for short 
baselines or designing special equipments for precise antenna 
height readings (Erol and Ayan, 2003). 
In some cases, even these special precautions might be 
insufficient to reach the necessary accuracy level; at that time to 
support GPS measurements with another measurement 
technique would be very useful as an improving solution. 
In this study, 1D and 3D deformation analysis of a large viaduct 
using GPS and Precise Levelling measurements are 
implemented. The control network points were positioned with 
GPS measurement technique and height differences were 
supported with precise levelling measurements. As the result of 
measurement campaigns, the X, Y, Z cartesian coordinates and 
height differences were determined from the GPS 
measurements and precise levelling measurements respectively. 
Later on, deformation analysis using the height differences 
according to provided data from the GPS and the data from the 
precise levelling were carried out separately. Then, the 3D 
deformation analysis using the GPS measurements data was 
carried out too. Explanation on used analysis methods and 
founded results will be given in addition to general review of 
deformation analysis methods in the following sections. 
2. OVERVIEW OF DEFORMATION MEASUREMENT 
TECHNIQUES 
As it is mentioned in the introduction part, measurement 
techniques were divided mainly into two different groups as 
geodetic and non-geodetic techniques. These main techniques 
can also be divided sub-techniques. In the following, it can be 
found short descriptions of the used techniques in deformation 
measurements. 
GPS; Global Positioning System offers advantages over 
conventional terrestrial methods. Intervisibility between 
stations is not strictly necessary, allowing greater flexibility in 
the selection of station locations than for terrestrial geodetic 
surveys. Measurements can be carried out during night or day, 
under varying weather conditions, which makes GPS 
measurements economical, especially when multiple receivers 
can be deployed on the structure during the survey. With the 
recent developed rapid static positioning techniques, the time 
for the measurements at each station is reduced to a few 
minutes (Anonym, 2002). 
Photogrammetry; 1f an object is photographed from two or 
more survey points of known relative positions (known 
coordinates) with a known relative orientation of the camera(s), 
623 
relative positions of any identifiable object points can be 
determined from the geometrical relationship between the 
intersecting optical rays which connect the image and object 
points. Aerial photogrammetry has been extensively used in 
determining ground movements in ground subsidence studies in 
mining areas, and terrestrial photogrammetry has been used in 
monitoring of engineering structures. The main advantages of 
using photogrammetry are the reduced time of field work; 
simultaneous three dimensional coordinates; and in principle an 
unlimited number of points can be monitored (Anonym, 2002). 
Tilt and Inclination Measurements; The measurement of tilt is 
usually understood as the determination of a deviation from the 
horizontal plane, while inclination is interpreted as a deviation 
from the vertical. The same instrument that measures tilt at a 
point can be called either a tiltmeter or an inclinometer 
depending on the interpretation of the results (Anonym, 2002). 
The some of new techniques for deformation monitoring can be 
listed as follows. : 
Insar; Elevations can be determined from Synthetic Aperture 
Radar (SAR) images by interferometric methods. This involves 
the use of two antennas, displaced either vertically or 
horizontally, installed on the same satellite or aircraft platform. 
One of the antennas transmits the signal, but both receive it, 
resulting in two images being created. The most accurate form 
of interferometric measurement is differential interferometry 
(InSAR), which involves the determination of elevation 
differences between two epochs of terrain measurement. In this 
case, the variations in the radar signal phases are determined 
between the two epochs, which reveal terrain surface 
deformations that may have occurred between the two 
occasions when the images were recorded. It is claimed that 
height differences as small as one centimeter can be detected by 
this method. Such a technique therefore has the potential of 
being a cost effective, near-continuous, remote method of 
measuring terrain subsidence due to mining, and ground 
movement due to land subsidence, earthquake or volcanic 
activity, etc. 
(http://www.gmat.unsw.edu.au/snap/work/insar.htm, accessed 
May 2004). 
Pseudolite; It is well known that for GPS-based deformation 
monitoring systems, the accuracy, availability, reliability and 
integrity of the positioning solutions is heavily dependent on 
the number, and geometric distribution, of the satellites being 
tracked. However, in some situations, such as in urban 
canyons, monitoring in valleys and in deep open-cut mines, the 
number of visible satellites may not be sufficient to reliably 
determine precise coordinates. Furthermore, it is impossible to 
use GPS for indoor applications and due to limitations of the 
GPS satellite geometry; the accuracy of the height component is 
generally 2 or 3 times worse than the horizontal components. 
These factors make it difficult to address GPS deformation 
monitoring applications in areas where the number of visible 
satellites is limited or satellite geometry is poor, especially 
where real-time high accuracy height component monitoring is 
needed, as in such applications as ground subsidence or 
deformation monitoring of man-made structures. Therefore, in 
order to improve the performance of GPS-only deformation 
monitoring systems, the integration of GPS with other 
technologies needs to be investigated. 
Pseudolites (pseudo-satellites), which are ground-based 
transmitters of GPS-like signals, can significantly enhance the 
 
	        
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