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

 

Introduction

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.

 

Reservoir siltation in Australia

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).

 

Comparison between Australian and overseas siltation rates

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

 

 

 

Sediment flushing devices

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.

 

Flood Hydrology and Dam safety

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.

 

Discussion

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) !

 

Summary and Conclusion

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.

 

References

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