Lee Water Hardness & Quality Report (2026)
Water Hardness
301+ mg/L
Very Hardestimated · not lab-verified
Source
mixed
pH Level
8.6
neutral = 7.0
Lead
0.001 mg/L
✓ Below action level
TDS
815.4 mg/L
Est. Daily Cost
£0.85
energy & soap waste
Source: DWI Data Portal · Updated 2026
0–99
mg/L
Soft
100–149
mg/L
Slightly Hard
150–199
mg/L
Moderately Hard
200–300
mg/L
Hard
300+
mg/L
Very Hard
Appliance Damage Report
In Lee, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In Lee | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 4.7 yrs | 8.5 yrs | -45% |
| Washing Machine | 6.6 yrs | 12 yrs | -45% |
| Water Heater | 8.3 yrs | 15 yrs | -45% |
Regional Water Comparison
How Lee compares to its nearest neighbours
| City | Hardness | Clark° | Risk | Source |
|---|---|---|---|---|
| ▶ Lee, Greater London | ≈ 301+ mg/L | 28.1° | 🔴 Very Hard | mixed |
| Blackheath, Greater London | 275.5 mg/L | 19.3° | 🟠 Hard | mixed |
| Kidbrooke, Greater London | ≈ 200–300 mg/L | 19.5° | 🟠 Hard | mixed |
| Ladywell, Greater London | ≈ 200–300 mg/L | 22.2° | 🟠 Hard | mixed |
| Catford, Greater London | ≈ 300+ mg/L | 19.6° | 🔴 Very Hard | mixed |
National Benchmark
How Lee compares to the United Kingdom average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ Lee | ≈ 301+ mg/L | 🔴 Very High |
| United Kingdom National Avg | 177 mg/L | 🟡 Moderate |
| Skipton Top Rated | 7.1 mg/L | 🟢 None |
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What Makes Lee's Water Unique?
Local geology and source profile
While no distinct 'Lee' supply zone with its own utility was identified, this area of Greater London is integrated into the broader water infrastructure managed by Thames Water and Anglian Water. The Lee Valley Reservoir Chain, a significant network of 13 reservoirs, forms a vital part of this system. These reservoirs are replenished by the River Lee Diversion, the River Lee Flood Relief Channel, the New River, and the Thames-Lee Water Main. Water undergoes treatment at various plants, processing both surface water from the River Lee and River Thames, and groundwater from local aquifers. The watershed itself begins in the Chiltern Hills and journeys southeast through East London to meet the River Thames.
The geology underpinning the Lee Valley is characterized by Chalk and other sedimentary rock layers typical of southeast England. These formations generally result in water that is moderately mineralized. However, the precise geological influences on the specific water chemistry for this particular supply zone remain unconfirmed without access to dedicated water quality reports. The Lee Valley watershed originates in the Chiltern Hills and flows southeast through East London to join the River Thames.
Homeowners in the Lee area may notice scale buildup on faucets and in appliances due to the mineral content of the water. This can affect the efficiency and lifespan of items like water heaters and dishwashers. Regular descaling can help mitigate these effects. If you're experiencing significant issues with scale or soap scum, a water softener might be a worthwhile consideration for your household. For precise details on water hardness, pH levels, or compliance reports specific to your address, it's best to contact Thames Water or Anglian Water directly.
Geology & Source: Chalk and sedimentary formations of southeast England; contribute to moderately mineralised water
Other Greater London Water Reports
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