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Dalserf Water Hardness & Quality Report (2026)

Water Hardness

78mg/L
Moderately Hard

5.5°Clark7.8°fH4.4°dH

Source

reservoir

pH Level

7.6

neutral = 7.0

Lead

0.005 mg/L

✓ Below action level

TDS

178.2 mg/L

Est. Daily Cost

£0.18

energy & soap waste

Source: DWI Data Portal · Updated 2026

78mg/L as CaCO₃Moderately Hard

0–60

mg/L

Soft

61–120

mg/L

Moderately Hard

121–180

mg/L

Hard

180+

mg/L

Very Hard

Appliance Damage Report

In Dalserf, your appliances are currently losing 10% efficiency due to mineral buildup.

ApplianceIn DalserfSoft Water CityEfficiency Loss
Kettle
7 yrs
8.5 yrs-18%
Washing Machine
10.7 yrs
12 yrs-11%
Water Heater
12.5 yrs
15 yrs-17%

Regional Water Comparison

How Dalserf compares to its nearest neighbours

CityHardnessClark°RiskSource
Dalserf, Scotland78 mg/L5.5°🟡 Moderately Hardreservoir
Wishaw, Scotland86.5 mg/L6.1°🟡 Moderately Hardreservoir
Larkhall, Scotland29 mg/L2°🟢 Softreservoir
Carluke, Scotland66 mg/L4.6°🟡 Moderately Hardreservoir
Motherwell, Scotland24.5 mg/L1.7°🟢 Softreservoir

National Benchmark

How Dalserf compares to the United Kingdom average

BenchmarkHardnessAppliance Risk
Dalserf78 mg/L🟡 Low
United Kingdom National Avg183 mg/L🔴 High
Livingston Top Rated8.5 mg/L🟢 None

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What Makes Dalserf's Water Unique?

Local geology and source profile

Source: ReservoirTDS: 178.2 mg/LpH: 7.6

Scottish Water supplies Dalserf in South Lanarkshire, a rural parish in the Clyde Valley between Hamilton and Lanark. Supply is drawn from Daer Reservoir on the upper River Clyde in the Southern Uplands and from Camps Reservoir on the Medwin Water, treated at Daer Water Treatment Works before distribution across south Lanarkshire and the Clyde Valley. At 78 mg/L (5.5°Clark), Dalserf's water is soft, characteristic of the ancient Southern Uplands igneous and metamorphic geology that produces naturally low-mineralisation runoff into the upper Clyde catchment.

The Southern Uplands above Daer Reservoir are underlain by Lower Palaeozoic greywackes, mudstones, and Silurian volcanic rocks — chemically resistant formations with very little calcium carbonate. Rainfall on the upland moors and blanket bogs of the upper Clyde headwaters flows over these inert rocks with minimal mineral dissolution, producing naturally soft water with low TDS. The modest hardness at 78 mg/L reflects some calcium input from Carboniferous sedimentary rocks in the lower Clyde Valley distribution zone and from pH-correction treatment that slightly elevates dissolved mineral content above the very soft upland reservoir baseline.

At 78 mg/L, Dalserf's soft water is comfortable for all domestic uses. Limescale accumulates slowly; descaling the kettle every two to three months is typically adequate. The combi-boiler benefits from a basic scale inhibitor as a precaution, though calcium build-up is not a pressing concern. Washing-up liquid lathers generously at normal quantities. Taps and shower heads remain clean for extended periods with only occasional maintenance needed. Soft water in the Clyde Valley is characteristic of Scottish Water's southern supply zones and means household appliances generally enjoy extended working lives.

Geology & Source: Supplied by Scottish Water from Daer Reservoir and Camps Reservoir in the Southern Uplands — treated at Daer Water Treatment Works — produces soft water at 78 mg/L (5.5°Clark).

Other Scotland Water Reports

Frequently Asked Questions

Is Dalserf's water safe to drink?
Yes. Dalserf's water meets all federal safety standards. The hardness is 78 mg/L (Moderately Hard), which is safe to drink. High hardness affects appliances and taste, but poses no health risk.
Do I need a water softener in Dalserf?
Dalserf's water is moderately hard at 78 mg/L. A water softener is generally not necessary, though a carbon filter can improve taste and remove any remaining chlorine.
How does Dalserf compare to the United Kingdom average?
The United Kingdom national average is 183 mg/L. Dalserf at 78 mg/L is 105 mg/L below the national average. The softest major city is Livingston at just 8.5 mg/L.