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Patchogue Water Hardness & Quality Report (2026)

Water Hardness

138.5mg/L
Hard

8.1 grains per gallon

Source

reservoir

pH Level

7.9

neutral = 7.0

Lead

0.006 mg/L

βœ“ Below action level

TDS

314.5 mg/L

Est. Daily Cost

$0.37

energy & soap waste

Source: USGS Water Quality Portal Β· Updated 2026

138.5mg/L as CaCO₃Hard

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 Patchogue, your appliances are currently losing 18% efficiency due to mineral buildup.

ApplianceIn PatchogueSoft Water CityEfficiency Loss
Kettle
5 yrs
8.5 yrs-41%
Washing Machine
8.5 yrs
12 yrs-29%
Water Heater
10.1 yrs
15 yrs-33%
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Regional Water Comparison

How Patchogue compares to its nearest neighbours

CityHardnessPFAS (ppt)RiskSource
β–Ά Patchogue, New York138.5 mg/L6.6 ppt🟠 Hardreservoir
East Patchogue, New York174.5 mg/L8.3 ppt🟠 Hardreservoir
Medford, New York68 mg/L3.3 ppt🟑 Moderately Hardreservoir
Holtsville, New York174.5 mg/L8.3 ppt🟠 Hardreservoir
Farmingville, New York101 mg/L4.9 ppt🟑 Moderately Hardreservoir

National Benchmark

How Patchogue compares to the USA average

BenchmarkHardnessAppliance Risk
β–Ά Patchogue138.5 mg/L🟠 Moderate
USA National Avg150 mg/L🟠 Moderate
Badger Top Rated8.5 mg/L🟒 None

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What Makes Patchogue's Water Unique?

Local geology and source profile

Source: ReservoirTDS: 314.5 mg/LpH: 7.9

Patchogue, New York, in Suffolk County β€” a Suffolk County village adjacent to Medford and Brookhaven on the south shore of Long Island β€” receives its water from the Suffolk County Water Authority, drawing from the Long Island aquifer (Suffolk County) through the south-central Long Island distribution.

The hard 138.5 mg/L hardness and TDS of 314.5 mg/L reflect the south-central Long Island Suffolk County aquifer supply's moderate calcareous character β€” the Pleistocene Ronkonkoma Aquifer slightly calcareous glacial sands produce moderate water, with TDS elevated by the coastal position and marine intrusion risk typical of south Long Island communities (compare Wawarsing NY: 70.5/169 in Ulster County on the Catskill Aqueduct far softer; Patchogue harder from the coastal Long Island glacial aquifer). The Long Island aquifer at Suffolk County β€” Pleistocene Ronkonkoma Aquifer (slightly calcareous β€” primary hardness contributor), Miocene Gardiners Clay (insoluble β€” dilutant), and Holocene coastal marine contact (chloride β€” TDS contributor).

At 138.5 mg/L with TDS 315, Patchogue's water is hard β€” scale builds in kettles and appliances over months, dishwashers benefit from rinse aid, and faucet aerators need periodic cleaning. Quarterly descaling is appropriate. The PFAS level of 6.6 ppt warrants a certified drinking water filter β€” the Suffolk County Long Island industrial and military corridor contribute to Patchogue's elevated readings.

Geology & Source: Patchogue in Suffolk County draws from the Suffolk County Water Authority on the Long Island aquifer (Suffolk County, south-central Long Island, New York) β€” the Long Island aquifer at Suffolk County is developed in Pleistocene Ronkonkoma Aquifer (slightly calcareous) and Miocene Gardiners Clay (insoluble) β€” New York Suffolk County Long Island aquifer Pleistocene coastal plain supply produces hard water at 138.5 mg/L with TDS 314.5 mg/L.

Other New York Water Reports

Frequently Asked Questions

Is Patchogue's water safe to drink?
Yes. Patchogue's water meets all federal safety standards. The hardness is 138.5 mg/L (Hard), which is safe to drink. High hardness affects appliances and taste, but poses no health risk.
Do I need a water softener in Patchogue?
At 138.5 mg/L (Hard), Patchogue's water will cause significant limescale on kettles, washing machines, and water heaters. A water softener or descaler is strongly recommended to extend appliance lifespan and reduce energy bills by up to 18%.
How does Patchogue compare to the USA average?
The USA national average is 150 mg/L. Patchogue at 138.5 mg/L is 11 mg/L below the national average. The softest major city is Badger at just 8.5 mg/L.
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