Water in the UK is devolved, which means there is no single UK water system. There are four, with different regulators, different ownership and different charging arrangements — and comparing them is one of the more informative natural experiments available in the sector.

The four systems
RowEnglandScotlandWalesNorthern Ireland
OwnershipPrivate regional monopoliesPublicly owned corporationCompany limited by guarantee, no shareholdersGovernment-owned company
Economic regulatorOfwatWICSOfwatUtility Regulator
Quality regulatorDWIDWQRDWIDWI NI
Environment regulatorEnvironment AgencySEPANatural Resources WalesNIEA
Household chargingSeparate water billCollected with council taxSeparate water billNo separate household charge
Number of companies16 water and/or sewerage companiesOneTwoOne

The rainfall problem

Scotland receives roughly twice the rainfall of England. Wales receives nearly as much. The population is concentrated in the south and east, which is the driest part.

Average annual rainfall by UK nation
1991–2020 Met Office baseline. Scotland receives nearly twice England’s rainfall.
Average annual rainfall by UK nationWales: 1,446 mm. Scotland: 1,391 mm. Northern Ireland: 1,106 mm. United Kingdom: 1,061 mm. England: 798 mm05001,0001,500mmWalesWales: 1,446 mm1,446ScotlandScotland: 1,391 mm1,391Northern IrelandNorthern Ireland: 1,106 mm1,106United KingdomUnited Kingdom: 1,061 mm1,061EnglandEngland: 798 mm797.7

Annual totals for different countries are not comparable as a measure of water availability. A large arid country and a small wet one can have similar national average rainfall while having entirely different renewable water resources per person. Gauge networks also differ in density, and mountain precipitation is systematically under-measured.

View the data behind this chart
SubjectValue (mm)Notes
Wales1,446
Scotland1,391
Northern Ireland1,106
United Kingdom1,061
England798

Parts of Essex and Cambridgeshire receive under 600 mm a year — comparable with parts of Spain, and less than Jerusalem. Combine that with the highest population density in the UK and you get the central fact of English water resources: the water is in the wrong place relative to the people.

Where UK water comes from

  • England: roughly a third groundwater, mostly chalk and sandstone, with the remainder from reservoirs and river abstraction. The south east is groundwater-dominated
  • Scotland: overwhelmingly upland surface water and reservoirs, generally soft and often coloured by peat
  • Wales: upland reservoirs and rivers, with significant transfer to England through the Elan Valley and Lake Vyrnwy aqueducts
  • Northern Ireland: Lough Neagh and upland reservoirs

Why hardness varies so much

Where hardness comes from

Hardness is geology written into water. Rain is soft everywhere; what it flows over decides what it becomes.

Where hardness comes fromRain falls with almost no dissolved minerals. Where it flows over granite, sandstone or peat, little dissolves and the water stays soft. Where it percolates through chalk, limestone or dolomite, carbonic acid dissolves calcium and magnesium carbonate, and the water becomes hard. The result is that hardness maps closely onto underlying geology rather than onto anything about the water supplier.Rainnaturally softGranite / sandstonelittle dissolvesPeat moorlandorganic acidsChalk / limestoneCaCO₃ dissolvesDolomiteadds magnesiumSoft water<50 mg/l as CaCO₃Hard water>200 mg/l as CaCO₃
Scotland and Wales
Predominantly hard igneous and metamorphic rock, so water is generally soft.
South east England
Chalk and limestone, so water is generally very hard.
What it means for you
Hardness has no adverse health effect. It affects scaling, soap use and taste, and it is set by the rock, not by the water company.

UK water hardness maps almost exactly onto geology. The chalk and limestone of southern and eastern England produce very hard water; the granite, sandstone and peat of Scotland, Wales, Cornwall and the Pennines produce soft water. This has nothing to do with the water company and cannot be changed by them.

Sources

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