College Park Water Hardness & Quality Report (2026)
Water Hardness
~120–179 mg/L
Hardestimated · not lab-verified
Source
reservoir
pH Level
8.3
neutral = 7.0
Lead
0.008 mg/L
✓ Below action level
TDS
462.7 mg/L
Est. Daily Cost
$0.40
energy & soap waste
Source: See methodology section below · 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 College Park, your appliances are currently losing 20% efficiency due to mineral buildup.
| Appliance | In College Park | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 6.8 yrs | 8.5 yrs | -20% |
| Washing Machine | 9.6 yrs | 12 yrs | -20% |
| Water Heater | 12 yrs | 15 yrs | -20% |
Regional Water Comparison
How College Park compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| ▶ College Park, Maryland | ≈ 120–179 mg/L | 10 ppt | 🟠 Hard | reservoir |
| Hyattsville, Maryland | ≈ 120–179 mg/L | 7.6 ppt | 🟠 Hard | reservoir |
| East Riverdale, Maryland | ≈ 120–179 mg/L | 8.3 ppt | 🟠 Hard | reservoir |
| Adelphi, Maryland | ≈ 120–179 mg/L | 10.5 ppt | 🟠 Hard | reservoir |
| Langley Park, Maryland | ≈ 120–179 mg/L | 4.7 ppt | 🟠 Hard | reservoir |
National Benchmark
How College Park compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ College Park | ≈ 120–179 mg/L | 🟠 Moderate |
| USA National Avg | 151 mg/L | 🟠 Moderate |
| Scarsdale Top Rated | 0.02 mg/L | 🟢 None |
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What Makes College Park's Water Unique?
Local geology and source profile
Washington Suburban Sanitary Commission (WSSC Water) provides water to College Park, Maryland, in Prince George's County, serving over 1.8 million residents across Montgomery and Prince George's counties. Primary sources include the Potomac River (70%) via the Washington Aqueduct and Patuxent River (30%) from the Brighton Dam Reservoir. Treatment occurs at the Patuxent Water Filtration Plant and Potomac Water Filtration Plant, with distribution through an extensive pipeline network covering the Washington, DC suburbs.
The Potomac and Patuxent watersheds span the Appalachian Piedmont and Coastal Plain, with limestone and dolomite in upstream Appalachian plateaus transitioning to sandy Cretaceous sediments downstream. The Piedmont's metamorphic and igneous rocks yield moderately mineralized runoff, while Coastal Plain aquifers like the Patapsco Formation (sandstones and clays) add dissolved ions from shell fragments and calcareous sands. The Patuxent Formation (unconsolidated sands and gravels) also contributes to the hard character of the supply through mineral dissolution during river flow and groundwater recharge across the Piedmont-Coastal Plain transition zone.
Hard water in this area promotes scale buildup in pipes, water heaters, dishwashers, and washing machines, reducing efficiency and lifespan. White deposits on fixtures and soap scum are common, increasing detergent use and cleaning needs. Regular vinegar descaling, installing scale inhibitors, or a water softener is recommended to mitigate effects and protect appliances. WSSC Water reports consistent compliance with EPA standards, including zero violations over 108 years, with pH typically 7.2–8.0; lead and copper levels meet action levels through corrosion control; treatment includes coagulation, sedimentation, filtration, chloramination, and fluoride addition, with occasional manganese or iron detections addressed via advanced oxidation.
Geology & Source: Potomac and Patuxent River watersheds — Piedmont-Coastal Plain transition; Patapsco Formation sandstones and clays, Patuxent Formation sands and gravels; limestone and dolomite upstream leach calcium and magnesium, producing hard supply
Other Maryland Water Reports
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Frequently Asked Questions
Is College Park's water safe to drink?
Do I need a water softener in College Park?
How does College Park compare to the USA average?
Data Sources & Methodology
Water quality data for College Park is derived from geographic and geological modelling of the surrounding region. No federal monitoring station data was available for this location.
Water Hardness
Modelled estimate based on state-level USGS geological survey data for this region. No direct USGS Water Quality Portal measurement was matched to this city — the value reflects a statistical range calibrated to the state's dominant rock types and typical source water characteristics.
pH
Estimated from regional geology and source water characteristics. pH is correlated with water hardness and local bedrock — values may differ from utility-reported figures.
TDS — Total Dissolved Solids
Estimated using a derived ratio from water hardness and regional conductance profiles. TDS in natural water correlates strongly with total mineral content including hardness ions.
PFAS — Perfluoroalkyl and Polyfluoroalkyl Substances
EPA UCMR5 (5th Unregulated Contaminant Monitoring Rule, 2023–2025) — sum of PFAS compounds detected at the public water system serving this city. A value of 0 indicates the system was sampled with no detection above reporting limits.
Lead
Modelled estimate based on the EPA Lead and Copper Rule 90th-percentile tap-sample methodology. No publicly available per-city lead dataset with sufficient national coverage exists. Values are a conservative baseline derived from city population tier and infrastructure age — all estimates are maintained below the EPA action level of 0.015 mg/L.
Appliance Lifespan
Calculated from water hardness using a linear degradation model. Baseline lifespans represent soft-water performance (kettle: 8.5 yrs, washing machine: 12.0 yrs, water heater: 15.0 yrs). Hard water mineral scale progressively reduces operational life in direct proportion to hardness concentration.