1. C.J. Pretorius¹, W.F. Schmidt¹ C.S. van Staden¹
K. Egger²
¹ Department of Water Affairs and Forestry, Republic of South Africa
² Schneider Ingenieur AG, Chur, Switzerland
10th INTERNATIONAL SYMPOSIUM ON DEFORMATION MEASUREMENTS
Orange, California, USA
THE EXTENSIVE GEODETIC SYSTEM USED FOR THE
MONITORING OF A 185 METRE HIGH ARCH DAM
IN
SOUTHERN AFRICA
2. •Provide Lesotho with hydro-
electricity
Features:
•double curvature arch dam
•185 m high above foundation
•crest length of 710 meter
•crest thickness 9 meter
•base width 60 meters
•To supplement water to the
Gauteng industrial area of the
Republic of South Africa;
Main objectives:
Katse Dam
4. Reference : Meas 9101
Point P01
Meas du dv dz
9211 .0 .4 .4
9612 .1 .1 -11.6
9709 -.2 .1 -13.3
9803 -.2 .2 -14.6
9807 .1 .0 -15.3
Point P02
Meas du dv dz
9211 .0 .3 -.5
9612 -9.9 2.4 -8.7
9709 -11.8 5.0 -17.3
9803 -12.4 5.1 -18.1
9807 -11.9 5.4 -19.1
Point P08
Meas du dv dz
9211 3.2 -.6 -1.7
9612 4.0 -.7 -11.1
9709 3.9 1.0 -13.6
9803 3.6 1.4 -14.2
9807 3.8 .1 -15.4
Deformations after impounding started 1996
5. • Correlation between pendulums and the Geodetic triangulation may take place
on the crest of the dam, galleries inside the dam wall and exits on the downstream
face of the dam
Concept of the Geodetic Deformation Measurements
• Close correlation between Instrumentation and Geodetic measurements
Correlation between Instrumentation and the Geodetic System
• Results of instruments which record relative displacements, when evaluated
together with Geodetic results, their relative displacements become absolute
• Multistage Geodetic system - full, reduced and mini measurements
have to be employed
• Establishment of an extensive triangulation network
Measurement intervals
• Concrete dams are subject to expansion and contraction because of changes in
temperature and pressure of the water load between summer and winter
• Monitoring therefore takes place during late summer (February) and winter (August) when
the expansion and contraction is at its maximum and minimum
15. Dam Wall
E Gallery
Left Flank
Rock Abutment
Gallery Exit
Pillar
Gallery Exit
Point
Traverse Pillars/Brackets
E - ACCESS
El: 1994 - 2036
Gallery Exit
Bracket
17. Adjustment Method used
• Helmert/91 program system
• Three-dimensional adjustment
• Based on theory of least squares
Definition of Adjustment
• Constants and Unknown parameters (co-ordinates etc.)
• Definition of the generalised Helmert - transformation
• Definition of an adequate stochastic model
18. Network
Mean Error Ellipses (U,V) Code A B Theta Mhe
mm mm o mm
Primary Pillar : P01 .39 .28 58.58 1.49
El 2060 Pillar : P115 .23 .19 85.13 .46
Alignment Point : R111 .40 .39 122.11 .50
Parapet Target : 111 .54 .52 37.04 .50
Bench mark : C11 ..... ..... ........ .47
El 2005 Pillar : P200 .27 .22 90.44 .43
El 1945 Pillar : P300 .28 .23 88.46 .42
The mean error ellipses depend on:
• Accuracy of observations
• Geometry of the geodetic network, and
• Selection of fixed points/Helmert control points
19. Traverses
Mean Error Ellipses (U,V) Code A B Theta Mhe
mm mm o mm
El 2005 Right Flank : 253 .34 .29 160.15 .30
Centre Bracket : 200 .14 .09 179.06 .17
Left Flank : 236 .22 .16 38.04 .24
El 1945 Right Flank : 337 .67 .22 150.49 .37
Centre Bracket : 300 .13 .10 179.42 .24
Left Flank : 336 .62 .21 28.16 .42
El 1900 Right Flank : 427 1.93 .57 153.31 .67
Centre Bracket : 400 .70 .44 179.20 .59
Left Flank : 426 1.67 .52 27.55 .69
Optical Align Point El 2052 : TA11 .47 .42 73.47 ....
Hanging Pendulum : DH0 .49 .39 101.09 ....
Inverse Pendulum :VKM0 1.37 .59 177.18 ....
Altrimetric Wire : AW11 .... .... .... .35
Mean error ellipses refer to Optical Alignment and Gallery
exit points as fixed points in the adjustments
28. • The Geodetic Scheme is of a high standard
• The scheme gives a high degree of information on the behaviour of the
dam
• Scheme is not only based on the network and traverse disposition but
also on the inclusion of the total pendulum system
• Scheme offers a variety of reduced measurements
• Easily accessible and ensure a high efficiency
• Provides adequate geodetic information of the structure and the
surrounding areas over a long period of time.
Conclusions