Hythe Water Hardness & Quality Report (2026)
Water Hardness
24.7°Clark35.3°fH19.7°dH
Source
mixed
pH Level
8.5
neutral = 7.0
Lead
0.005 mg/L
✓ Below action level
TDS
1007.8 mg/L
Est. Daily Cost
£0.80
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 Hythe, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In Hythe | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 1.5 yrs | 8.5 yrs | -82% |
| Washing Machine | 3 yrs | 12 yrs | -75% |
| Water Heater | 5 yrs | 15 yrs | -67% |
Regional Water Comparison
How Hythe compares to its nearest neighbours
| City | Hardness | Clark° | Risk | Source |
|---|---|---|---|---|
| ▶ Hythe, South East | 352.5 mg/L | 24.7° | 🔴 Very Hard | mixed |
| Folkestone, South East | 372.5 mg/L | 26.1° | 🔴 Very Hard | mixed |
| Canterbury, South East | 336.5 mg/L | 23.6° | 🔴 Very Hard | mixed |
| Ashford, South East | 364 mg/L | 25.5° | 🔴 Very Hard | mixed |
| Dover, South East | 327.5 mg/L | 23° | 🔴 Very Hard | mixed |
National Benchmark
How Hythe compares to the United Kingdom average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ Hythe | 352.5 mg/L | 🔴 High |
| United Kingdom National Avg | 183 mg/L | 🔴 High |
| Livingston Top Rated | 8.5 mg/L | 🟢 None |
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What Makes Hythe's Water Unique?
Local geology and source profile
South East Water supplies Hythe, the Cinque Port town on the Kent coast between Folkestone and Dymchurch at the seaward edge of the Romney Marsh, from deeply confined North Downs Chalk boreholes where the chalk plunges beneath Weald Clay and Romney Marsh marine deposits in east Kent, treated at regional east Kent chalk works. At 352.5 mg/L (24.7°Clark) and a TDS of 1007.8 mg/L, Hythe's water is the hardest in this entire UK dataset — driven by the extreme mineral saturation of the deeply confined East Kent Chalk aquifer, where groundwater residence times spanning millennia allow calcium bicarbonate dissolution to reach absolute saturation.
Hythe sits immediately at the foot of the North Downs chalk escarpment where it meets the Romney Marsh lowland — the chalk dips steeply here and disappears beneath up to 20 metres of Romney Marsh alluvium, Weald Clay, and Lower Greensand to the south. This confinement creates an artesian chalk aquifer of exceptional saturation, where groundwater is under considerable hydrostatic pressure and has had many thousands of years to dissolve calcium carbonate to near-equilibrium saturation. The TDS exceeding 1000 mg/L at Hythe is consistent with this geological context — the same geological regime that produces Swanscombe's 1031.7 mg/L TDS from the Northfleet confined chalk — and places Hythe at the absolute extreme of natural groundwater mineralisation in England.
At 352.5 mg/L, limescale causes extreme and relentless damage to all household appliances and plumbing in Hythe. Kettles must be descaled at least weekly to prevent near-immediate element failure. The combi-boiler faces near-certain premature breakdown without a properly fitted, regularly replaced scale inhibitor and very frequent professional heat exchanger servicing. Washing-up liquid requires very large quantities to produce any meaningful lather. Taps, shower screens, and all plumbing must be descaled weekly with white vinegar or a proprietary product to prevent permanent chalk encrustation. A whole-house water softener is essentially essential rather than merely recommended to protect all appliances in this, the hardest tap water community measured in Great Britain.
Geology & Source: Supplied by South East Water from deeply confined North Downs Chalk boreholes in the Kent Downs at the Romney Marsh fringe — treated at regional east Kent chalk works — produces extremely hard water at 352.5 mg/L (24.7°Clark).