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Appendix 1 Water Resource Zone Characteristics Contents Drought Plan 2019 Appendix 1 Water Resource Zone Characteristics Contents Water Resource Zone Characteristics 3 Area 1: Lincolnshire and Nottinghamshire 5 Central Lincolnshire 5 Bourne 7 East Lincolnshire 8 Nottinghamshire 10 South Lincolnshire 11 Area 2: Ruthamford 12 Ruthamford Central 12 Ruthamford North 13 Ruthamford South 15 Ruthamford West 17 Area 3: Fenland 18 North Fenland 18 South Fenland 19 Area 4: Norfolk 20 Happisburgh 20 North Norfolk Coast 21 North Norfolk Rural 23 Norwich and The Broads 25 South Norfolk Rural 27 Area 5: East Sufflok and Essex 28 Central Essex 28 East Suffolk 29 South Essex 31 Area 6: Cambridgeshire and West Suffolk 33 Cheveley, Ely, Newmarket, Sudbury, Ixworth, and Bury Haverhill 33 Thetford 36 Area 7: Hartlepool 37 Hartlepool 37 2 Water Resource Zone Characteristics The uneven nature of climate, drought, growth and List of WRMP 2019 WRZs, in order of discussion: environmental impacts across our region means we have developed Water Resource Zones (WRZs). WRZs Area 1: Lincolnshire and Nottinghamshire are the geographical areas used to develop forecasts Central Lincolnshire of supply and demand and supply-demand balances. Bourne The WRZ describes an area within which supply infrastructure and demand centres are linked such East Lincolnshire that customers in the WRZ experience the same risk Nottinghamshire of supply failure. These were reviewed in the Water South Lincolnshire Resources Management Plan (WRMP) 2019 and have changed since the last WRMP and Drought Plan. Area 2: Ruthamford Ruthamford Central Overall, we have increased the number of WRZs from 19 at WRMP 2015 to 28 for WRMP 2019, including Ruthamford North the addition of South Humber Bank which is a non- Ruthamford South potable WRZ that sits within Central Lincolnshire. Ruthamford West The revised list of WRZs are listed below and Area 3: Fenland shown in Figure 1. For each WRZ we describe the characteristics of the zone, details of previous North Fenland droughts experienced and current drought risk. South Fenland Through WRMP 2019 modelling, we have assessed our drought risk for each WRZ and consider the Area 4: Norfolk majority to be secure up to a 1 in 200 year event. Happisburgh There are five zones where we have identified remaining vulnerabilities and we have proposed North Norfolk Coast supply-side investment schemes in the WRMP. North Norfolk Rural These will be completed by the end of AMP7. Should Norwich and The Broads a severe drought occur before this time, we have South Norfolk Rural identified ‘interim options’, in Appendix 3. Appendix 3 also includes high level options should an extreme Area 5: East Sufflok and Essex drought (1 in 500 year event) occur, although given the unlikely and uncertain nature of such an event Central Essex these options have not been detailed at a WRZ level. East Suffolk Demand drought measures we would undertake for South Essex each WRZ to ensure security of supply are detailed in Appendix 2. Area 6: Cambridgeshire and West Suffolk Bury Haverhill Cheveley Ely Ixworth Newmarket Sudbury Thetford Area 7: Hartlepool Hartlepool 3 South West Lincolnshire Humber East Lincolnshire (WRMP (WRMP 2015) Bank 2015) split into two renamed WRZs: East Lincolnshire Nottinghamshire and Bourne Fenland (WRMP 2015) split into two WRZs: North Fenland and South Fenland. Hunstanton WRZ Nottinghamshire North (WRMP 2015) incorporated North Norfolk Coast Lincolnshire East Lincolnshire into North Fenland (WRMP 2015) split into two WRZs: North Central Norfolk Coast and Lincolnshire Happisburgh (WRMP 2015) split into three WRZs: Central South Lincolnshire, South Lincolnshire North Norfolk Happisburgh Lincolnshire and North Coast South Humber Fenland Bank Norfolk Bourne Rural (WRMP Norwich and 2015) split South the Broads North Norfolk into two Fenland Rural WRZs: North Norfolk Coast and Norfolk Thetford South Norfolk Rural Rural Ruthamford Ely North Ixworth West Suffolk Newmarket (WRMP 2015) Bury split into three Haverhill WRZs: Bury Cheveley East Haverhill, Suffolk Ixworth and Ruthamford Ruthamford Thetford West South Central Essex Ruthamford Sudbury Central South Essex Ruthamford South (WRMP 2015) split into three WRZs: Ruthamford West, Central and South 4 Area 1: Lincolnshire and Nottinghamshire Central Lincolnshire Characteristics The Central Lincolnshire WRZ covers an area of 2072km2 and extends south from the Humber. It includes groundwater abstraction from the Lincolnshire Limestone and a surface water abstraction from the River Trent. It is based on the supply systems for Scunthorpe and Lincoln. The new Hall WTW was opened in July 2014, which will treat water abstracted directly from the River Trent for supply to customers in Lincoln. Source details Approximate % groundwater/ Water Treatment Source surface water WRZ split WRZ Water source Works type % groundwater % surface water Branston Booths GW Confined Lincs Limestone Dunston GW Confined Lincs Limestone Hall SW River Trent Newton GW Sherwood Sandstone Central Waddingham GW Confined Lincs Limestone 83 17 Lincs Welton GW Confined Lincs Limestone Barrow GW Lincs Chalk River Ancholme / Elsham (Potable) GW/SW Lincs Chalk Winterton GW Confined Lincs Limestone 5 Drought risk Drought risk has been assessed for up to a 1 in 200 year drought event as part of our WRMP 2019. This identified the Hall surface water intake on the River Trent as being vulnerable to a drought of this severity. There are three classified drought vulnerable boreholes (Tier 1): Goxhill, Welton and Winterton Holmes. We have also reviewed our risk to a 1 in 500 year extreme drought. This identified additional vulnerability is likely to be seen at the River Trent intake, and the groundwater sources of; Barrow, Barton, Ulceby, Branston Booths, Glentham, Hibaldstow Bridge, Redbourne, Spridlington, Waddingham. Drought Plan Management Actions There is an interim option proposed for Central Lincs to mitigate modelled vulnerability to a severe drought in this zone. This option is a drought permit on the River Trent at our Hall WTW intake to lower the minimum residual flow to allow increased abstraction in times of low flows. To ensure security of supply is maintained at the drought vulnerable boreholes, we can increase abstraction from less vulnerable sources within the zone and have also invested in a new borehole at Winterton to maintain supply. Cadney direct intake is reliant on augmentation of the flow of the River Ancholme by the Environment Agency’s Trent-Witham-Ancholme (TWA) transfer scheme during lower summer flows. The TWA scheme is managed by the Environment Agency under a Section 20 agreement. Analysis shows this intake is secure against the worst historic and modelled 1 in 200 year droughts1. 1 Atkins (2017) Trent Witham Ancholme Assessment Memo 6 Bourne Characteristics The Bourne WRZ covers an area of 1087km2 and lies to the south west of the Wash. It is based on the supply systems for Bourne, Spalding and Stamford. Water is abstracted from groundwater sources in the Southern Lincolnshire Limestone aquifer. Source details Approximate % groundwater/ Water Treatment Source surface water WRZ split WRZ Water source Works type % groundwater % surface water Bourne GW Confined Lincs Limestone Etton GW Confined Lincs Limestone Bourne Pilsgate GW Confined Lincs Limestone 100 0 Tallington GW Confined Lincs Limestone Wilsthorpe GW Confined Lincs Limestone The need for river support in the lower reaches identified that this zone as not being vulnerable to a of the River Glen was addressed through the drought of this severity. commissioning of the Gwash-Glen transfer scheme in 1991. The scheme is operated by the Environment We have also reviewed our risk to a 1 in 500 year Agency through a Section 20 Agreement with Anglian extreme drought. This identified additional Water by which water is released from Rutland vulnerability is likely to be seen at; Bourne, Pilsgate, Water on request. This secures an increased level of Tallington, and Wilsthorpe. abstraction from the Southern Limestone aquifer. Drought Plan Management Actions Drought risk There are no specific drought measures other than Drought risk has been assessed for up to a 1 in 200 demand management actions. year drought event as part of our WRMP 2019. This 7 East Lincolnshire Characteristics The East Lincolnshire WRZ covers an area of 2783km2, extending from Humber to the Wash and is based on the supply systems for Grimsby, Louth, Skegness, and Boston. The supplies are primarily groundwater abstractions from the Lincolnshire Chalk, Lincolnshire Limestone and Spilsby Sandstone. There is also surface water abstraction from the Louth Canal into Covenham pumped storage reservoir. Source details Approximate % groundwater/ Water Treatment Source surface water WRZ split WRZ Water source Works type % groundwater % surface water Confined Spilsby Candlesby GW Sandstone Confined Spilsby Driby GW Sandstone Fordington GW Spilsby Sandstone Fulstow GW Lincs Chalk Lincs Chalk / Spilsby Maltby le Marsh GW Sandstone East 67 33 Lincs Manby GW Spilsby Sandstone Lincs Chalk / Spilsby Mumby GW Sandstone Raithby GW Spilsby Sandstone West Pinchbeck GW Confined Lincs Limestone Barnoldby GW Lincs Chalk Covenham GW Louth Canal 8 Approximate % groundwater/ Water Treatment Source surface water WRZ split WRZ Water source Works type % groundwater % surface water Habrough GW Lincs Chalk Healing GW Lincs Chalk Little Coates GW Lincs Chalk East 67 33 Lincs Little London GW Lincs Chalk Tetney GW Lincs Chalk Weelsby GW Lincs Chalk A Section 20 Water Resource Management Drought Risk Agreement with the Environment Agency serves to protect and limit the use of the Northern Lincolnshire Drought risk has been assessed for up to a 1 in 200 Chalk aquifer during periods of naturally low year drought event as part of our WRMP 2019. This groundwater levels, which can result in low spring identified that this zone as not being vulnerable to a flows from the Lincolnshire Wolds and saline intrusion drought of this severity. along the south bank of the Humber Estuary. We have also reviewed our risk to a 1 in 500 year We abstract from the Louth Canal to fill Covenham extreme drought.
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