Reading Water Hardness & Quality Report (2026)
Water Hardness
8.9 grains per gallon
Source
reservoir
pH Level
8
neutral = 7.0
Lead
0.005 mg/L
β Below action level
TDS
322.3 mg/L
Est. Daily Cost
$0.41
energy & soap waste
Source: USGS Water Quality Portal Β· Updated 2026
0β60
mg/L
Soft
61β120
mg/L
Moderately Hard
121β180
mg/L
Hard
180+
mg/L
Very Hard
Appliance Damage Report
In Reading, your appliances are currently losing 20% efficiency due to mineral buildup.
| Appliance | In Reading | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 4.6 yrs | 8.5 yrs | -46% |
| Washing Machine | 7.9 yrs | 12 yrs | -34% |
| Water Heater | 9.5 yrs | 15 yrs | -37% |
Regional Water Comparison
How Reading compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Reading, Pennsylvania | 153 mg/L | 7.8 ppt | π Hard | reservoir |
| Pottstown, Pennsylvania | 118.5 mg/L | 6 ppt | π‘ Moderately Hard | reservoir |
| Ephrata, Pennsylvania | 108 mg/L | 5.5 ppt | π‘ Moderately Hard | reservoir |
| Coatesville, Pennsylvania | 140 mg/L | 7.2 ppt | π Hard | reservoir |
| Limerick, Pennsylvania | 186.5 mg/L | 9.6 ppt | π΄ Very Hard | reservoir |
National Benchmark
How Reading compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Reading | 153 mg/L | π Moderate |
| USA National Avg | 150 mg/L | π Moderate |
| Badger Top Rated | 8.5 mg/L | π’ None |
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What Makes Reading's Water Unique?
Local geology and source profile
Reading, Pennsylvania β the Berks County seat in the Schuylkill Valley β draws its municipal water supply from the Schuylkill River via the Reading Area Water Authority (RAWA), operating a raw water intake on the Schuylkill River in Berks County. The Schuylkill River at Reading has drained the northeastern Pennsylvania anthracite region and the Great Valley carbonate zone above the city. Water hardness measures 153 mg/L β classified as hard.
Reading's hard supply reflects the Schuylkill River's significant carbonate mineral accumulation at the Berks County reach. The Schuylkill River watershed above Reading includes: the Pennsylvania Great Valley (South Mountain zone β Cambrian Chickies Quartzite and Ordovician carbonate thrust sheets, Silurian Juniata Formation); the Appalachian anthracite region (Pennsylvanian Pottsville Conglomerate and anthracite coal measures β acidic drainage partially offset by downstream neutralisation); and the Great Valley carbonate formation (the CambrianβOrdovician Great Valley limestone and dolomite belt, part of the Appalachian Valley and Ridge calcareous zone). The Valley and Ridge limestone belt's drainage significantly contributes dissolved calcium, producing the moderately hard to hard supply at Reading's Schuylkill intake.
At 153 mg/L, Reading residents face regular hard water challenges. Scale deposits form on faucet aerators, showerheads, and appliances within weeks β monthly descaling with citric acid solution is standard maintenance. Dishwashers require rinse-aid, and water heaters benefit from annual inspection. Reading Area Water Authority consistently delivers water meeting all Pennsylvania DEP and EPA Safe Drinking Water Act requirements.
Geology & Source: River supply from the Schuylkill River via the Reading Area Water Authority (RAWA) β the Schuylkill River at the Reading reach drains the Pennsylvania Great Valley Silurian Tuscarora Sandstone, Ordovician Reedsville Formation, and the Pennsylvanian anthracite fields calcareous formations; the Schuylkill Valley produces moderately hard supply at 153 mg/L in Berks County.