Vale of Leven Water Hardness & Quality Report (2026)
Water Hardness
5.4°Clark7.8°fH4.3°dH
Source
reservoir
pH Level
7.6
neutral = 7.0
Lead
0.005 mg/L
✓ Below action level
TDS
176.7 mg/L
Est. Daily Cost
£0.18
energy & soap waste
Source: DWI Data Portal · Updated 2026
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 Vale of Leven, your appliances are currently losing 10% efficiency due to mineral buildup.
| Appliance | In Vale of Leven | Soft Water City | Efficiency 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 Vale of Leven compares to its nearest neighbours
| City | Hardness | Clark° | Risk | Source |
|---|---|---|---|---|
| ▶ Vale of Leven, Scotland | 77.5 mg/L | 5.4° | 🟡 Moderately Hard | reservoir |
| Dumbarton, Scotland | 54 mg/L | 3.8° | 🟢 Soft | reservoir |
| Port Glasgow, Scotland | 40.5 mg/L | 2.8° | 🟢 Soft | reservoir |
| Erskine, Scotland | 44 mg/L | 3.1° | 🟢 Soft | reservoir |
| Helensburgh, Scotland | 21 mg/L | 1.5° | 🟢 Soft | reservoir |
National Benchmark
How Vale of Leven compares to the United Kingdom average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ Vale of Leven | 77.5 mg/L | 🟡 Low |
| United Kingdom National Avg | 183 mg/L | 🔴 High |
| Livingston Top Rated | 8.5 mg/L | 🟢 None |
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What Makes Vale of Leven's Water Unique?
Local geology and source profile
Vale of Leven, the urban area comprising Alexandria, Renton and Bonhill on the River Leven in West Dunbartonshire between Loch Lomond and Dumbarton, is supplied by Scottish Water from local upland reservoirs in the Kilpatrick Hills and the Cardross and Loch Lomond fringe. The primary local source for the Vale of Leven supply zone is Carman Reservoir on Carman Hill above Renton — a reservoir fed by drainage from the Carboniferous basalt and dolerite sills and Devonian volcanic rocks of the Kilpatrick Hills that flank the south side of Loch Lomond. These volcanic and intrusive rocks — while calcium-poor by comparison with sedimentary limestone — weather slightly faster than the purely metamorphic Dalradian schist of Loch Lomond's Highland catchment, yielding modestly more mineralised water. At 77.5 mg/L (TDS 176.7 mg/L), the Vale of Leven supply is softer than most English water but measurably harder than the pure Loch Lomond supply at Clydebank (33.5 mg/L, TDS 61.9 mg/L), a few miles down the Leven.
The Carboniferous basalt, dolerite intrusions and Devonian volcanic rocks of the Kilpatrick Hills are mafic rocks — iron-magnesium-rich silicates — that weather slowly but contribute slightly more dissolved calcium and sodium than the purely metamorphic Dalradian schist of the central Highlands. While still producing very soft water by English standards, the Kilpatrick Hills catchment yields a distinctly more mineralised supply than Loch Lomond's Highland metamorphic catchment. Scottish Water's distribution of both the Loch Lomond and local Kilpatrick reservoir supply across West Dunbartonshire produces the characteristic variation in hardness across the Vale of Leven and Clydebank zones.
At 77.5 mg/L Vale of Leven's water is soft and limescale is rarely a significant domestic issue. Kettles need descaling only every two to three months with a brief white vinegar rinse. Shower screens remain clear for extended periods. Washing-up liquid lathers freely. Combi-boilers and white goods enjoy low scaling risk and extended lifespans. Vale of Leven's industrial heritage — Tobias Smollett was born here, and the Leven's mills once processed linen and cotton — is backed by a consistently soft west Scottish water supply.
Geology & Source: Supplied by Scottish Water from Carman Reservoir and local West Dunbartonshire upland sources — Carboniferous and Devonian volcanic catchment in the Kilpatrick Hills — produces soft water at 77.5 mg/L (5.4°Clark).