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SILTATION OF AUSTRALIAN
RESERVOIRS : SOME OBSERVATIONS AND DAM SAFETY IMPLICATIONS
H. CHANSON
and D.P. JAMES
Department
of Civil Engineering, The University of Queensland, Brisbane QLD 4072,
Australia
Fax: (61
7) 33 65 45 99 - Email: h.chanson@mailbox.uq.edu.au
Abstract
The Australian continent can experience extreme
sedimentation rates which affect water supply systems. The study documents
complete reservoir siltation events. Sedimentation problems were observed
predominantly with small to medium size reservoirs (catchment area less than
100 km2). The effects of reservoir siltation are analysed in terms
of dam safety. In several cases, the sediment load associated with major flood
events would create high loads on the dam wall, especially in the cases of thin
concrete structures. For such situations, the tested concrete strength could be
less than twice the load, and the safety of the dam becomes questionable.
Keywords: reservoir siltation, Australian reservoirs, extreme sedimentation, hydrology, dam safety
Reservoir siltation affects the safety of old reservoirs in
several ways. The reservoir sediment increases the load on the dam wall. The
reduction of reservoir storage capacity reduces the attenuation of the flood
and it may increase the outflow, hence the head above crest, for a given
reservoir inflow. Often the original hydrological study of ancient reservoirs
relied on a small sample of data, and the estimated inflow underestimated the
'real' probable maximum flood (PMF) of the catchment-reservoir system.
Altogether the sediment weight and larger head above crest create higher
pressures on the dam wall (fig. 1).
In this paper, the writers review extreme siltation cases of
Australian reservoirs. Then they discuss the implications in terms of dam
safety, with practical examples.
Several Australian dams failed slowly because of reservoir
siltation, although the authorities do no acknowledge it. The writers
investigated reservoir siltation cases (e.g. CHANSON and JAMES 1998a,b).
Between 1890 and 1960, numerous dams became fully-silted, mostly in New South
Wales (Table 1, Fig. 2, 3, 4 and 5). De Burgh dam (Fig. 2) was disused in 1929
after the dismantlement of the railway line. It is the oldest reinforced concrete
thin arch in Australia. Koorawatha dam (Fig. 3) was the second arch dam built
at the same site. Both structures became fully-silted by bed-load material. The
siltation of Cunningham Creek dam (Fig. 4) was well-documented by HELLSTRÖM
(1941) (suspension sedimentation predominantly). Illalong Creek (Fig. 5) was
completed two years after and it is located less than 30-km from Cunningham
Creek.
Some reservoirs became fully-silted in less than 20 years,
and their failure affected the local economy. The list (Table 1) includes town
water supply reservoirs (e.g. Moore Creek dam), railway dams (e.g. Gap weir)
and mining reservoirs (e.g. Junction Reefs).
Table 2 summarises (well-documented) extreme siltation
events in Australia. The analysis suggests that sedimentation rates in
Australia were high. The siltation of Quipolly reservoir between 1941-1943 was
an extraordinary event. The Korrumbyn Creek dam sedimentation was very rapid : i.e., less than 7 years !
The site selection was improper (CHANSON and JAMES 1998a). Overall
sedimentation problems were experienced mostly with small to medium size
reservoirs : i.e., catchment area less than 100 km2 typically. In
contrast large reservoirs have not been sedimenting rapidly at the exception of
Melton, Eppalock and Eildon reservoirs, all in Victoria. Heavy siltation at
Eildon was experienced in 1940 during torrential rainfalls, following bushfires
which destroyed more than 50% of the catchment forest (JOSEPH 1953). At
Eppalock, the catchment was affected by extensive gold mining, tree clearing
and hydraulic mining during the period 1851-1890, and rabbit infestation was
another problem (DAVIES 1996).
Since the 1950s, lower siltation rates have been experienced
on the Australia continent. The decrease in reservoir sedimentation is related
to the introduction of new farming techniques, new land conservation practices
and an awareness of soil erosion problems. The trend is characteristic in New
South Wales, Victoria, South Australia and Queensland.
Note that most extreme (recorded) siltation rates were
observed during short duration studies (1 to 10 years) and there is no
information on long-term siltation (over 70 years).
Figure 1 -
Effects of reservoir siltation on dam wall pressure

Fig. 2 -
De Burgh dam, Baren Jack NSW, 1908 (Photograph in July 1998)
H = 5 m -
Fully-silted railway reservoir

Surprisingly most Australian dams have been inadequately
equipped with flushing devices. Some did not have scour pipe (e.g. Gap weir
1902). Most reservoirs were equipped with a small scour outlet (
= 0.3 to 0.5 m) inadequate to desilt a reservoir. For example, DARLEY (1900)
recommended a "24-inch" diameter outlet. Only few dams were equipped
with two or more flushing systems : e.g., the Illalong Creek dam (1914,
Binalong NSW) completed in 1914 and now fully-silted (Fig. 5) !
Table 1 -
Examples of major siltation of Australia dams
|
Reservoir |
Location |
Completion
date |
End of
use |
Purpose |
|
(1) |
(2) |
(3) |
(4) |
(5) |
|
Sheba dams |
Nundle
NSW |
1888 |
-- (*) |
Mining. Two dams. |
|
Corona |
Broken
Hill NSW |
1890 |
1910 (*) |
Irrigation. |
|
Laanecoorie |
Maryborough
VIC |
1891 |
Still in
use |
Irrigation. |
|
Stephens Creek |
Broken
Hill NSW |
1892 |
Still in
use |
Town water supply. |
|
Junction Reefs |
Lyndhurst
NSW |
1896 |
1930? (*) |
Hydropower for mining
activities. |
|
Moore Creek |
Tamworth
NSW |
1898 |
1924 (*) |
Town water supply. |
|
Koorawatha No. 1 |
Cowra
NSW |
1901 |
1911 (*) |
Railway supply. Replaced
by 2nd dam. |
|
Gap |
Werris
Creek |
1902 |
1924 (*) |
Railway supply. |
|
Pekina Creek |
Orroroo
SA |
1907 |
1984 |
Irrigation and town water
supply. |
|
de Burgh dam |
Barren
Jack NSW |
1908 |
1929 (*) |
Railway and town water
supply. |
|
Koorawatha No. 2 |
Cowra
NSW |
1911 |
-- (*) |
Railway supply. |
|
Pykes Creek |
Ballan
VIC |
1911 |
Still in
use |
Irrigation and water
supply. |
|
Pekina Creek |
Orroroo
SA |
1910s |
1930s (*) |
Town water supply. |
|
Cunningham Creek |
Harden
NSW |
1912 |
1929 (*) |
Railway supply. |
|
Illalong Creek |
Binalong
NSW |
1914 |
1985? (*) |
Railway supply. |
|
Umberumberka |
Broken
Hill NSW |
1915 |
Still in
use |
Town water supply. |
|
Melton |
Werribee
VIC |
1916 |
Still in
use |
Irrigation. |
|
Korrumbyn Creek |
Murwillumbah
NSW |
1918 |
1924? (*) |
Town water supply. |
|
Borenore Creek |
Orange
NSW |
1928 |
Still in
use |
Railway supply. Town
water supply today. |
|
Eppalock |
Central
Victoria |
1932 |
Still in
use |
Irrigation and water
supply |
|
Quipolly |
Werris
Creek NSW |
1932 |
1955 (*) |
Railway supply. |
|
Inverell |
Inverell
NSW |
1939 |
1982 (*) |
Town water supply. |
|
Arrona Gorge dam |
Leigh
Creek Town SA |
1950 |
-- |
Mining and town water
supply. |
Reference : Present study, CHANSON and JAMES (1998a,b).
Note : (*) :
reservoir fully-silted today; (--) : information not available.
Reservoir siltation affects the safety of old reservoirs :
by reducing the flood attenuation and by increasing the wall pressure. The
author re-analysed the storm hydrograph of several Australian reservoirs
affected by siltation (e.g. Moore Creek 1898, Korrumbyn Creek 1918, Quipolly No.
1 1932). The study shows that, in most cases, the storage capacity was
very-small. The reservoir became full before the storm peak flow and it did not
attenuate the flood (e.g. 1910 flood at Moore Creek). Once the reservoir was
full, the outflow would almost equals the inflow (i.e. no translation) and the
additional storage capacity was negligible compared to the inflow volume.
At Moore Creek, a concrete thin arch dam, the spillway was
designed to pass 100 m3/s before dam overtopping, corresponding to a
1-in-40 year flood event. But the designers allowed for a 0.6-m [2-ft] dam
crest surcharge (WADE 1909), corresponding to a 270 m3/s overflow.
For that surcharge, the wall compression stress was about 2.2 MPa (clear-water
reservoir). A recent re-analysis of the catchment hydrology argued that the PMF
inflow would be about 1500 m3/s. For the 1500 m3/s peak
inflow, the head above spillway crest would be about 4 metres, leading to a
compression stress of the concrete arch of about 2.5 MPa at base for a
water-filled reservoir and about 4.5 MPa for a fully-silted reservoir !
Fig. 3 - Koorawatha dam (No. 2), Koorawatha NSW, 1911 (Photograph on 28 December 1997)H = 9.1 m - Fully-silted railway reservoir

Fig. 4 -
Cunningham Creek dam, Harden NSW, 1912 (Photograph on 28 December 1997)
H = 16 m
(?), e = 0.93 m - Fully-silted railway reservoir since the 1930s

These values must be compared with the concrete resistance.
During the 19th century, the strength of concrete was lower than today.
Typically, concrete strengths (at 6 months) ranged from 2 to 15 MPa (CHANSON
and JAMES 1998b). DARLEY (1900) who designed Moore Creek dam performed concrete
tests : "the average crushing strength of a large number of specimen,
[...] six months old, has been ascertained by testing to vary from about 70 to
145 tons per square foot - 80 tons may be taken as a safe average" (p. 53)
{1 ton/ft2
0.1073 MPa}.
For a fully-silted concrete arch wall (e.g. Moore Creek),
the effect of reservoir siltation and a more accurate estimate of the PMF
indicate that the arch wall stress could be larger than half of the original
concrete stre
ngth. The resulting safety factor is very low (i.e. less than
2) although most concrete structures were designed with a safety factor of 5
(DARLEY 1900, WADE 1909). There are concerns for the safety of old concrete
dams and several fully-silted reservoirs have low safety records : Moore Creek,
Cunningham Creek, Korrumbyn Creek, Quipolly No. 1.
With good quality concrete, the concrete strength is
expected to increase with age. At the Barossa dam (1902), the measured
compressive strength was 19.5 MPa at 90 day and 43.5 MPa 80 years later
(DOHERTY and SCHMITT 1987). But, in some cases (e.g. Victoria dam WA, Lithgow
No. 2 dam, NSW), concrete deterioration occurred and diminished the wall
resistance. Proper in-situ tests of concrete strengths are required for
fully-silted concrete dams.
The above calculations are optimistic because they do not
take into account the presence of trees and bush at the dam crest. In several
cases (e.g. Moore Creek, de Burgh, Korrumbyn Creek), a forest occupies the
reservoir and trees sit on the dam crest. The obstruction caused by the trees
would cause a backwater effect associated with an additional wall surcharge
(e.g. Fig. 2) !
The study demonstrates that reservoir sedimentation has been
a serious problem in Australia. Several reservoirs (Table 1) became
fully-silted because the designers did not take into account correctly the soil
erosion and sediment transport processes, and no soil conservation practice was
introduced.
Fully-silted reservoirs stand as a source of embarrassment
for the scientists and the public. They are also a potential hazards. During a
large flood event (e.g. PMF), the sediment weight adds to the wall compression
stress and the safety factor (ratio of concrete strength to load) could become
less than two ! With concrete structures, the properties of the wall must be
tested in-situ. Further a proper analysis of the reservoir catchment and dam
wall should be conducted for each individual structure.
CHANSON, H., and JAMES, P. (1998a). "Rapid Reservoir
Sedimentation of Four Historic Thin Arch Dams in Australia." Jl of Performance of Constructed Facilities,
ASCE, Vol. 12, No. 2, May, pp. 85-92. Errata : Vol. 12, No. 3, p.169.
CHANSON, H., and JAMES, D.P. (1998b). "Historical
Development of Arch Dams in Australia : from Advanced Designs to Engineering
Failures." Research Report CE 157,
Dept. of Civil Engineering, The University of Queensland, Brisbane, Australia.
DARLEY, C.W. (1900). "Curved Concrete Walls for Storage
Reservoirs." Proc. Royal Soc. of New
South Wales, Australia, 19 Dec., Vol. 34, pp. xlix-lxii.
DAVIES, J.A. (1996). "Catchment Management for the
Control of Sediment Delivery : the Case of the Eppalock Catchment,
Victoria." Ph.D. thesis, Dept.
of Civil and Environmental Engrg., University of Melbourne, Australia, 675 pages.
DOHERTY, L.E., and SCHMITT, L.J. (1987). "Concrete in
Barossa Arch Dam." ANCOLD Bulletin,
No. 77, Aug., pp. 56-57.
HELLSTRÖM, B. (1941). "Några Iakttagelser Över Vittring
Erosion Och Slambildning i Malaya Och Australien." Geografiska Annaler, Stockholm, Sweden, No. 1-2, pp. 102-124 (in
Swedish).
JOSEPH, O.F.F. (1953). "Siltation of Reservoirs. Eildon
Surveys Analysed." AQUA, Nov.,
pp. 19-23.
ORTH, F. (1934). "Die Verlandung von Staubecken."
('The Siltation of Reservoirs.') Bautechnik, Vol. 12, No. 26, pp. 345-358 (in
German).
ROWAN, J.S., GOODWILL, P., and GECO, M. (1995).
"Temporal Variability in Catchment Sediment Yield Determined from Repeated
Bathymetric Surveys : Abbeystead Reservoir, U.K.." Phys. Chem. Earth, Vol. 120, No. 2, pp. 199-206.
WADE, L.A.B. (1909). "Concrete and Masonry
Dam-Construction in New South Wales." Min.
of Proc. of Instn. of Civil Engineers, London, Vol. 178, No. 9, Paper 3791,
pp. 1-26. Discussion : Vol. 178, No. 9, pp. 27-110.
Table 2 -
Extreme reservoir siltation rates in Australia
|
Reservoir |
Sedimentation.
rate |
Study
period |
Catchment
area |
Annual
rainfall |
|
|
(!Unexpected End of Expression) |
|
(!Unexpected End of Expression) |
(mm) |
|
(1) |
(2) |
(3) |
(4) |
(5) |
|
Australia |
|
|
|
|
|
Quipolly (*) |
1,143 |
1941-43 |
70 |
686 |
|
Pykes Creek |
465 |
1911-45 |
125 |
-- |
|
Umberumberka |
407 |
1961-64 |
420 |
220 |
|
Corona (*) |
400 |
1890-1910 |
15 |
-- |
|
Eildon |
381 |
1939-40 |
3,885 |
-- |
|
Umberumberka |
330 |
1915-41 |
420 |
220 |
|
Stephens Creek |
238 |
1892-1907 |
510 |
-- |
|
Quipolly (*) |
222 |
1943-52 |
70 |
686 |
|
Pykes Creek |
215 |
1945-60 |
127 |
|
|
Quipolly (*) |
206 |
1932-41 |
70 |
686 |
|
Umberumberka |
195 |
1941-44 |
420 |
220 |
|
Quipolly (*) |
186 |
1952-85 (?) |
70 |
|
|
Moore Creek (*) |
174 |
1911-24 |
51 |
674 |
|
Pekina Creek (*) |
174 |
1911-44 |
136 |
340 to
450 |
|
Melton |
141 |
1916-45 |
1,098 |
470 to
1040 |
|
Tenterfield Creek |
138 |
1930-51 |
38 |
-- |
|
Eppalock |
130 |
1962-68 |
2,000 |
-- |
|
Stephens Creek |
129 |
1944-58 |
510 |
-- |
|
Borenore Creek |
129 |
1928-81 |
22 |
-- |
|
Moore Creek (*) |
128 |
1898-1911 |
51 |
674 |
|
Eppalock |
124 |
1968-76 |
1,850 |
|
|
Korrumbyn Creek (*) |
1,400
(?) |
1918-1924
(?) |
3 |
1,699 |
References : Present study, CHANSON and JAMES (1998a,b),
ORTH (1934), ROWAN et al. (1995).
Notes : (*) fully-silted reservoir; (?) uncertain data; (--)
Data not available.
Fig.5 -
Illalong Creek dam, Binalong NSW, 1914 (Photograph on 28 December 1997)
H = 11.3
m, L = 170 m, R = 91.4 m - Fully-silted railway reservoir, despite two scour
outlets
