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Nashua Water Hardness & Quality Report (2026)

Water Hardness

77.5mg/L
Moderately Hard

4.5 grains per gallon

Source

reservoir

pH Level

7.7

neutral = 7.0

Lead

0.008 mg/L

✓ Below action level

TDS

199.7 mg/L

Est. Daily Cost

$0.21

energy & soap waste

Source: USGS Water Quality Portal · Updated 2026

77.5mg/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 Nashua, your appliances are currently losing 10% efficiency due to mineral buildup.

ApplianceIn NashuaSoft 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%
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Regional Water Comparison

How Nashua compares to its nearest neighbours

CityHardnessPFAS (ppt)RiskSource
Nashua, New Hampshire77.5 mg/L8.5 ppt🟡 Moderately Hardreservoir
Merrimack, New Hampshire61.5 mg/L7.3 ppt🟡 Moderately Hardreservoir
Pelham, New Hampshire29 mg/L4.7 ppt🟢 Softreservoir
Windham, New Hampshire66.5 mg/L7.7 ppt🟡 Moderately Hardreservoir
Derry, New Hampshire18 mg/L3.9 ppt🟢 Softreservoir

National Benchmark

How Nashua compares to the USA average

BenchmarkHardnessAppliance Risk
Nashua77.5 mg/L🟡 Low
USA National Avg150 mg/L🟠 Moderate
Badger Top Rated8.5 mg/L🟢 None

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What Makes Nashua's Water Unique?

Local geology and source profile

Source: ReservoirTDS: 199.7 mg/LpH: 7.7

Nashua, New Hampshire — the second-largest city in New Hampshire in Hillsborough County on the Massachusetts border — draws its municipal water supply from the Pennichuck Water Works (a public water utility), sourcing from Pennichuck Pond and Pennichuck Brook watershed in Nashua and Merrimack, plus the Merrimack River via the Nashua Water Treatment Plant (a supplemental surface water source). Pennichuck Water Works has served Nashua since 1853. Water hardness measures 77.5 mg/L — classified as moderately soft.

Nashua's moderately soft supply reflects the Pennichuck watershed's New Hampshire granite geology. The Pennichuck Pond drainage basin is underlain by the Precambrian–Ordovician Milford–Concord Granite (the pink Milford Granite used widely in New England monuments) and associated Merrimack Belt metamorphic rocks (Ordovician Smalls Falls Formation, Berwick Formation). These ancient New Hampshire Paleozoic granites and metamorphics — like other New England crystalline basement rocks — contribute negligible dissolved calcium to watershed drainage, producing naturally soft water. The Merrimack River component at Nashua adds slightly more mineral content from its diverse upper watershed, but the overall supply remains moderately soft.

With hardness at 77.5 mg/L, Nashua residents experience minimal to moderate scale challenges. Faucet aerators and showerheads develop deposits slowly — bi-monthly cleaning with citric acid solution is sufficient. Dishwashers produce clean glassware. Pennichuck Water Works consistently delivers water meeting all New Hampshire DES and EPA Safe Drinking Water Act requirements.

Geology & Source: Mixed supply from the Pennichuck Brook and Pennichuck Pond watershed and the Merrimack River via the Pennichuck Water Works — the Southern New Hampshire Precambrian Milford–Concord granite, Fitchburg–Concord intrusive complex; the Nashua–Pennichuck watershed on the Precambrian granite terrain produces moderately soft supply at 77.5 mg/L in Hillsborough County.

Other New Hampshire Water Reports

Frequently Asked Questions

Is Nashua's water safe to drink?
Yes. Nashua's water meets all federal safety standards. The hardness is 77.5 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 Nashua?
Nashua's water is moderately hard at 77.5 mg/L. A water softener is generally not necessary, though a carbon filter can improve taste and remove any remaining chlorine.
How does Nashua compare to the USA average?
The USA national average is 150 mg/L. Nashua at 77.5 mg/L is 72 mg/L below the national average. The softest major city is Badger at just 8.5 mg/L.
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