Northumbrian Water Limited is a private limited company registered in England and Wales under company number 2366703, incorporated in this form in 1989.[2]
Area of operations
Northumbrian Water's operations cover an area of 9,400km2 and extend from the urban conurbations of Tyneside, Wearside and Teesside to the sparsely populated rural districts of Durham and Northumberland. A small area around Hartlepool is excluded from NW's water supply licence; this area is supplied by Hartlepool Water, a water-only company.[3]
The total population served by NW is 2.7m people using:[1]
44impounding reservoirs
57water treatment works
344water pumping stations
338water service reservoirs
25,545kmof water mains
418 sewage treatment works
765 sewage pumping stations
29,724kmof sewers (including the transfer of 13,510km of private drains and sewers on 1 October 2011)[1]
Resource zones
NW's operations are split between two resource zones: Berwick and Fowberry resource zone; and Kielder resource zone.[4]
Berwick and Fowberry
This zone covers a small area in north Northumberland, centred on the towns of Berwick and Wooler which has no access to stored water and its water supplies come entirely from an aquifer in the underlying Fell Sandstone, from which water is abstracted via boreholes.
Kielder
99% of the population served by Northumbrian Water is in the Kielder zone, so named from Kielder Water, the largest reservoir in NW's region. The zone is split into three supply zones, Northern, Central and Southern, which correspond broadly to the catchment areas of the rivers Tyne, Wear and Tees respectively, each of which incorporates one of the region's three conurbations.[4]
Under normal circumstances, each zone is self-sufficient in water resources, but provision exists to transfer water from the northern zone to either of the others, via the Kielder Transfer Scheme.
The zone's water supplies are supported by a system of impounding reservoirs, river pumping stations, and water treatment works. There are 29 impounding reservoirs, of which three—Kielder, Derwent and Cow Green— account for 78% of the available capacity of nearly 360,000 million litres; Kielder Water, with a capacity of 196,000 million litres, alone accounts for 55% of available resources.[5]
Water is supplied to the treatment works either from a nearby reservoir or by abstraction from one of the major rivers. In the latter case, the flow of the river has to be maintained by discharging water from a reservoir further upstream.
Northern zone
Northumbrian Water's treatment works at Fontburn, Northumberland
The major reservoir in the Northern zone is Kielder Water. Others include: Fontburn, on the River Font, which feeds an adjacent treatment works; and Catcleugh, on the River Rede, which is connected by the Rede pipeline with Gunnerton treatment works, 27 miles (44km) downstream. Catcleugh is also at the start of a sequence that includes reservoirs at Colt Crag, two at Hallington and a complex of seven at Whittle Dene, where there is also a treatment works.[4][6]
Within the Northern zone, water is abstracted from the North Tyne at Barrasford and from the Tyne at Ovingham, with discharges from Kielder Water ensuring that the minimum regulated flow is maintained in the two rivers. From Barrasford, water is pumped to West Hallington reservoir, while water abstracted at Ovingham is used to supply Horsley treatment works and can also be used to replenish the Whittle Dene complex. The treatment works at Horsley and Whittle Dean jointly meet the needs of Tyneside and south-east Northumberland.[4][6]
Derwent reservoir supplies Mosswood treatment works, 2 miles (4km) away, and Burnhope supplies Wear Valley treatment works at Wearhead. With the opening of the new Wear Valley works, in 2004, an older facility at Tunstall was closed, and Tunstall reservoir is now used solely to maintain regulated flow on the Wear. The reservoirs at Waskerley, Hisehope and Smiddy Shaw supply Honey Hill treatment works, which lies just below Smiddy Shaw; Honey Hill is also supplied from Burnhope.[4][6]
Water is abstracted from the Wear at Chester-le-Street to supply a treatment works at Great Lumley, the minimum flow being maintained through discharges from Burnhope or Tunstall.[4]
In the event that neither Burnhope nor Tunstall can satisfy regulatory discharges to meet the minimum maintained flow on the Wear, water can be transferred into the Wear via the Kielder Transfer Scheme, which can also be used to supplement or replace water from Derwent reservoir or to replenish Waskerley reservoir.[6]
Coastal parts of the Central zone, including Sunderland, are supplied with drinking water from boreholes and shafts that abstract groundwater from aquifers in the underlying Magnesian limestone.[4]
Southern zone
The largest reservoir in the Southern zone is Cow Green, in upper Teesdale, which is used solely to regulate flow in the River Tees. There are two chains of reservoirs on the Lune and the Balder, tributaries of the Tees, which in combination supply a water treatment works at Lartington, just south of Cotherstone. The main reservoirs are Selset and Grassholme in Lunedale, and Balderhead, Blackton and Hury in Baldersdale.[6] Two further reservoirs, at Lockwood Beck and Scaling Dam, on the North Yorkshire Moors, are no longer used for water supply and serve purely as recreational facilities.
Water is abstracted from the Tees for treatment at the Broken Scar treatment works, near Low Coniscliffe on the outskirts of Darlington, and for industrial water at Blackwell, just downstream from Broken Scar, and Low Worsall, near Kirklevington.[6]
Tees Cottage Pumping Station is sited across the A67 from Broken Scar. This Victorian facility, which closed in 1980, is still owned by Northumbrian Water, but is now opened as a museum by a Preservation Trust. It contains a 1904-built rotative beam engine, and a 1914 gas engine, believed to be the largest working preserved example in Europe.
Kielder Transfer Scheme
The Kielder Transfer Scheme provides a means to utilise the excess capacity of Kielder Water to meet shortfalls in either of the Central and Southern zones.[6]
The heart of the scheme is a 21-mile-long (34km) tunnel, the Tyne-Tees Tunnel, through which water flows under gravity to outfalls at Frosterley on the Wear and at Eggleston on the Tees. The tunnel is fed by a pipeline, nearly 4 miles long and 6.5ft (2 metres) in diameter, between Riding Mill, on the Tyne, and Letch House, the high point in the system. There is a direct connection between the tunnel and Mosswood treatment works and further access is provided at Waskerley via a submersible pump in the tunnel's airshaft.[6]
If water is to be transferred, it is abstracted from the Tyne at Riding Mill, a compensating discharge being made from Kielder Water into the North Tyne. From Riding Mill, the water is pumped up the rising main to Letch House, from where it flows downhill through the tunnel.
Under normal conditions, transfers to the Wear and the Tees are not required, as Tunstall and Burnhope reservoirs are usually able to meet the demand for compensating flows on the Wear and Cow Green is able to meet demands on the Tees;[5] since the Scheme became operational, transfers to the Tees have only been required in two years, 1983 and 1989. Transfers to the Central zone are usually required for a period of 12 weeks in the summer, when the reservoirs supplying Honey Hill are unable to meet the full demand.[5]
The River Tyne is a river in North East England. Its length is 73 miles (118 km). It is formed by the North Tyne and the South Tyne, which converge at Warden Rock near Hexham in Northumberland at a place dubbed 'The Meeting of the Waters'.
Ladybower Reservoir is a large Y-shaped, artificial reservoir, the lowest of three in the Upper Derwent Valley in Derbyshire, England. The River Ashop flows into the reservoir from the west; the River Derwent flows south, initially through Howden Reservoir, then Derwent Reservoir, and finally through Ladybower Reservoir. The reservoir is owned by Severn Trent.
Kielder Water is a large man-made reservoir in Northumberland in North East England. It is the largest artificial lake in the United Kingdom by capacity of water and it is surrounded by Kielder Forest, one of the biggest man-made woodlands in Europe. The scheme was planned in the late 1960s to satisfy an expected rise in demand for water to support a booming UK industrial economy.
The Massachusetts Water Resources Authority (MWRA) is a public authority in the Commonwealth of Massachusetts that provides wholesale drinking water and sewage services to 3.1 million people in sixty-one municipalities and more than 5,500 large industrial users in the eastern and central parts of the state, primarily in the Boston area.
The Derwent Reservoir is a reservoir on the River Derwent, on the border between County Durham and Northumberland, in England. It is west of Consett. It is 3.5 miles (5.6 km) long) and covers an area of 4 km2 and has a maximum depth of 100 ft (30m) and when full, holds 11,000 million gallons (50,000,000m³).
Waskerley is a village in County Durham, England. It is situated six miles to the southwest of Consett and three miles southwest of Castleside and the A68. Stanhope in the Durham Dales is a further six miles to the southwest and the Derwent Reservoir and the village of Edmundbyers is approximately five miles to the north. The village of Muggleswick is three miles to the north.
Burnhope Reservoir is a reservoir above the village of Wearhead, County Durham, England.
Hallington Reservoirs are located near the small village of Colwell, Northumberland, England on the B6342 road off the A68 road, and 7 miles (11 km) north of Corbridge. Hallington is actually two small reservoirs: Hallington Reservoir West and Hallington Reservoir East, which are separated by a dam.
The Rede is a river in Northumberland, England. The river rises on Carter Fell on the Anglo-Scottish border feeding Catcleugh Reservoir and joins the River North Tyne below the village of Redesmouth. The Rede is one of only two rivers in the North East of England that has the freshwater pearl mussel in its waters.
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.
The Knight Reservoir is a large pumped storage reservoir located in the Borough of Elmbridge in Surrey. It was inaugurated in 1907 and stores up to 2,180 million litres of raw water abstracted from the River Thames prior to its treatment and supply to London and north Surrey. It is located south of the River Thames, west of West Molesey, and between Hurst Road (A3050) and Walton Road (B369). It is adjacent to, and west of, its twin Bessborough Reservoir.
Bakethin Reservoir is a reservoir immediately upstream of Kielder Water, in Northumberland, England, close to the border with Scotland. It is fed by the River North Tyne and lies southeast of Kielder village.
Severn Trent Water Authority was one of ten regional water authorities established in 1974. Its area of operation was the catchments of the River Trent and River Severn. It assumed the powers and responsibilities of existing water supply authorities in those catchment areas, the Severn River Authority, the Trent River Authority and the sewage and sewage disposal responsibilities of the councils within its area.
The City of Nottingham Water Department (1912–1974), formerly the Nottingham Corporation Water Department (1880–1912), was responsible for the supply of water to Nottingham from 1880 to 1974. The first water supply company in the town was the Nottingham Waterworks Company, established in 1696, which took water from the River Leen, and later from springs at Scotholme, when the river became polluted. Other companies were set up in the late 18th century and in 1824, while in 1826 the Trent Water Company was established. They employed Thomas Hawksley as their engineer, who became one of the great water engineers of the period, and Nottingham had the first constant pressurised water supply system in the country. The various companies amalgamated in 1845, and Hawksley remained as the consulting engineer until 1879.
Tunstall Reservoir was a water supply storage reservoir completed in 1879, and now used solely to maintain minimum regulatory flows on the River Wear in northeast England. It is situated in the north Pennines of the United Kingdom, and lies 3.5 km north of the village of Wolsingham, in Weardale, County Durham. The earthen embankment dam, which impounds the reservoir, is recognized as the location where pressure grouting with cement grout was first utilized in 1876 by engineer Thomas Hawksley, to reduce leakage within the rock foundation under an earth dam. Pressure grouting has since become normal practice for construction and remediation at dams and related water resource projects.
Waskerley Reservoir is the largest of a group of three reservoirs located on Muggleswick Common, County Durham, the others being Smiddy Shaw and Hisehope Reservoirs.
Smiddy Shaw Reservoir is one of a group of three reservoirs located on Muggleswick Common, County Durham, the others being Waskerley and Hisehope Reservoirs.
Hisehope Reservoir is the smallest of a group of three reservoirs located on Muggleswick Common, County Durham, the others being Waskerley and Smiddy Shaw Reservoirs.
Essex and Suffolk Water is a water supply company in the United Kingdom. It operates in two geographically distinct areas, one serving parts of Norfolk and Suffolk, and the other serving parts of Essex and Greater London. The total population served is 1.8 million. Essex and Suffolk is a 'water only' supplier, with sewerage services provided by Anglian Water and Thames Water within its areas of supply. It is part of the Northumbrian Water Group.
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