Staines Reservoirs

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Coordinates: 51°26′49″N 0°29′12″W / 51.44694°N 0.48667°W / 51.44694; -0.48667
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Staines Reservoirs
Two large reservoirs surrounded by flat land and housing
Stanwell and the Staines Reservoirs in 2011
Staines Reservoirs is located in Surrey
Staines Reservoirs
Staines Reservoirs
LocationSurrey
Coordinates51°26′49″N 0°29′12″W / 51.44694°N 0.48667°W / 51.44694; -0.48667
Typereservoir puddle clay embankment
Primary inflows295,496 cubic metres/day
Primary outflows364,000 cubic metres/day
Catchment areaRiver Thames
Basin countriesUnited Kingdom
Built1902
Surface area172 ha (430 acres)
Average depthDam walls 6.4–10.67 m (21.0–35.0 ft) high
Water volume15,175,000 m3 (535,900,000 cu ft)

The Staines Reservoirs are two large pumped storage reservoirs sitting to the east of the King George VI Reservoir near Heathrow airport in Surrey within the Colne Valley regional park. The village of Stanwell is mainly to the north east, and the town of Staines is to the south.

Both adjoin, west, the A3044. The south one adjoins the A30 where the road is bypassed by the intra-M25 motorway network but is a trunk road, maintained by National Highways. They were completed in 1902.[1]

History[edit]

For reliable and plentiful water supplies, three London water companies resolved to construct and operate two large reservoirs at seasonally waterlogged land partly in the parish of Staines, otherwise in Stanwell.[2] These would be pumped storage reservoirs to hold water abstracted from the Thames[3] receiving it from an aqueduct, then delivering it by another to treatment works for their supply pipes. The three were the New River Company, the Grand Junction Water Company and the West Middlesex Water Company.[4]

To obtain full indemnity and a compulsory purchase standard mechanism they promoted the Staines Reservoir Bill of 1896.[4] The Bill was opposed by some landowners, London and Middlesex County Councils. Nevertheless, the Bill was enacted, with amendments, as the Staines Reservoirs, &c. Act 1896 (59 & 60 Vict. c.ccxli).[4] The companies formed a joint committee to oversee the construction.[2] The two reservoirs, North and South, are separated by a 1,030-metre embankment dam. The embankments of the two have a 6- to 8-metre-deep puddle clay core having scoured out the surface gravel to the underlying London Clay.[5] They have total capacity of 3,338 million gallons (15.175 million m3) and were completed in 1902.[4] The valve towers are to the west.

Later in the same year of building the three companies, and seven others, dissolved into the Metropolitan Water Board – under the Metropolis Water Act 1902.

Operation[edit]

The reservoirs are filled from the Staines Reservoirs Aqueduct, built as part of the works. Water was originally lifted from the aqueduct to the reservoirs by five steam driven engines, each with a capacity of 16 million gallons per day (72,737 m3/day).[2] The engines were housed in Staines pumping station south-west of the south reservoir. Under the original legal provisions, when the flow of the river at Bell Weir exceeded 265 million gallons a day (1.205 million m3/d) the joint company could abstract any surplus up to 100 million gallons (454,609 m3) of which 35 million gallons (159,113 m3) could be run directly to the filter beds at Hampton and the surplus (295,496 m3/day) pumped into the reservoirs.[6] The top water level in the North Reservoir is 3 m higher than the South reservoir.[5] Water for treatment and use is drawn from the reservoirs through the valve towers and delivered to the aqueduct to flow south-east to several water treatment works.

The Metropolitan Water Board operated the reservoirs until the Board was abolished in 1974 under the provisions of the Water Act 1973 and ownership and control transferred to the Thames Water Authority, now Thames Water.

In 1992 there was a proposal to increase the capacity of the reservoirs by raising the height of the dam walls and removing the dividing embankment.[7] The work was estimated to take up to six years to complete.

From April 2020 a sheet pile cut-off wall was installed in two places to prevent leakage of water through the core of the south reservoir's embankment.[8]

The area has been designated a Site of Special Scientific Interest (SSSI) as it carries important wintering populations of tufted ducks, pochard, goosander and goldeneye.[9]

Staines Reservoirs Aqueduct[edit]

River Ash and North Thames Reservoirs
Legend
 Thames
1.
2.
Intake of aqueduct (with sluice)
Colne Brook
County or Shire Ditch
Wraysbury River
Colne (feeder of the three above)
Ash
Pumping Station to 3. & 4. & 5.
overflow sluice to the Ash
Gravity-drained aqueduct
 A308  road
(River Ash under aqueduct)
 A308  road
Pumping Station to 6.
Ashford Treatment Works for 6.
 A244  road
Kempton Treatment Works
(some water sent directly to below)
7.Grand Junction Reservoir
Hampton Treatment Works
 8.
Thames

The Staines Reservoirs Aqueduct is a 13 km (8.1 mi) aqueduct[10] that runs from the River Thames at Hythe End in Buckinghamshire (51°26'24.4"N 0°32'28.8"W) to the Red House distribution reservoir (51°25'11.6"N 0°23'20.4"W) near Kempton Park.[10] It was built by the Staines Reservoirs Joint Committee and originally completed in 1902.[6] The maximum flow capacity of the aqueduct is 364 million litres per day (364,000 m3/day).[10]

Water is drawn from the north side of the Thames about 300 yards above Bell Weir, at a decorative sluice house.[2] This is provided with sluices to control the flow and screens to prevent debris entering the aqueduct. The water runs underground for about 350 yards in a north-east direction, it then flows in two steel siphons under the Colne Brook. It continues in a concrete lined open conduit, before going under the Wraysbury river in steel siphons, then east across Staines Moor and another siphon under the River Colne to Staines pumping station. From here water is lifted into the Staines and King George VI reservoirs by pumps.[2]

Water for treatment and use is drawn from the Staines and King George VI Reservoirs and flows along the Staines Reservoirs Aqueduct in an east-south-east direction to Ashford, then around the north side of Queen Mary Reservoir, water discharged from the reservoir enters the aqueduct at this point. The aqueduct continues across Ashford Common with a connection to Ashford Common water treatment works and then across Sunbury Common.[11] From Sunbury Common the aqueduct changes direction to the north-east, it curves around the north side of Kempton Park race course with connections to Sunbury and Kempton Park water treatment works, and flows in a south-east direction into the Red House distribution reservoir (51°25'11.6"N 0°23'20.4"W).[12] From here a pipeline and an open aqueduct takes water south to the reservoirs at the west end of Hampton waterworks.[13] From 1916 experiments were undertaken to pre-treat the water in the aqueduct with chlorine added to the water from the Staines reservoirs.[13]

To increase the supply of water the aqueduct was paralleled underground in the 1960s by the Staines–Kempton aqueduct tunnel.[14] This was built by the Metropolitan Water Board between 1960–63 and runs from Little Hythe on the Thames to the water treatment works at Kempton Park. It is 7.64 kilometres (4.75 mi) long and 2.4 metres (7 ft 10 in) in diameter.[10] The tunnel is lined with 150,000 expanded concrete wedge blocks. The contractors for the project were Edmund Nuttall, Sons and Company Limited.[15]

In February 2014, after a sustained period of heavy rain, the River Thames was at a high level that caused water to back up in the River Colne.[16] This then spilt into the Staines Reservoirs Aqueduct, which channelled the water to Staines. The aqueduct spilt over into the River Ash, which overtopped its banks and flooded about 80 houses in the Leacroft and Priory Green areas and damaged the aqueduct.[17]

See also[edit]

References[edit]

  1. ^ British History on line
  2. ^ a b c d e Hunter, W. (1 October 1901). "Visit to the Staines Reservoir Works". Journal of the Sanitary Institute. 22 (4): 571–73.
  3. ^ Bell, F. G. (1979). Engineering Geology and Geotechnics. Butterworth-Heinemann Ltd. pp. 268–9. ISBN 9780408003551.
  4. ^ a b c d London Metropolitan Archives (1897–1902). "Staines reservoir joint committee: water supply and distribution". aim25.com. Retrieved 16 June 2020.
  5. ^ a b "Long-term stress measurements in the clay cores of storage reservoir embankments" (PDF). British Dams.org. Retrieved 17 June 2020.
  6. ^ a b "The Staines Reservoirs". The Times. 18 June 1901. p. 5.
  7. ^ "Water Resources Development Options" (PDF). September 1992. Retrieved 17 June 2020.
  8. ^ "Reservoir work to keep London's taps flowing for another 120 years". Thames Water. 14 April 2020. Retrieved 18 June 2020.
  9. ^ Colne Valley Park Archived 6 February 2007 at the Wayback Machine
  10. ^ a b c d "Staines-Kempton Tunnel Aqueduct". Engineering Timelines. 1960. Retrieved 16 June 2020.
  11. ^ Ordnance Survey Six-inch map, Middlesex XXIV.NE, dated 1920
  12. ^ Ordnance Survey six-inch map, London Sheet Q, dated 1920
  13. ^ a b Wray, Anthony (December 2015). "Water Quality, Morbidity, and Mortality in London,1906-1926" (PDF). eh.net. Retrieved 16 June 2020.
  14. ^ Cuthbert, Eric William and Frank Wood (1962). "The Thames-Lee tunnel water main". Proceedings of the Institution of Civil Engineers. 23 (4): 690–704. doi:10.1680/iicep.1962.10819. Retrieved 19 June 2020.
  15. ^ "A new water tunnel". New Scientist. 8 (201): 788. 22 September 1960.
  16. ^ Surrey County Council (20 April 2015). "Flood Investigation Report River Ash and Knowle Green Area" (PDF). Surrey County Council. Retrieved 19 June 2020.
  17. ^ Goble, R. A. (7 March 2015). Staines aqueduct Flooding 2014. Retrieved 19 June 2020. {{cite book}}: |website= ignored (help)

External links[edit]

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