College Water Hardness & Quality Report (2026)
Water Hardness
~0–59 mg/L
Softestimated · not lab-verified
Source
reservoir
pH Level
7.2
neutral = 7.0
Lead
0.002 mg/L
✓ Below action level
TDS
32.6 mg/L
Est. Daily Cost
$0.08
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, your appliances are currently losing 4% efficiency due to mineral buildup.
| Appliance | In College | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 8.2 yrs | 8.5 yrs | -4% |
| Washing Machine | 11.5 yrs | 12 yrs | -4% |
| Water Heater | 14.4 yrs | 15 yrs | -4% |
Regional Water Comparison
How College compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| ▶ College, Alaska | ≈ 0–59 mg/L | 0.5 ppt | 🟢 Soft | reservoir |
| Fairbanks, Alaska | ≈ 120–179 mg/L | 26.2 ppt | 🟠 Hard | groundwater |
| Badger, Alaska | ≈ 120–179 mg/L | 0.4 ppt | 🟠 Hard | reservoir |
| Knik-Fairview, Alaska | ≈ 120–179 mg/L | 1.1 ppt | 🟠 Hard | reservoir |
| Eagle River, Alaska | ≈ 120–179 mg/L | 1 ppt | 🟠 Hard | groundwater |
National Benchmark
How College compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ College | ≈ 0–59 mg/L | 🟢 None |
| USA National Avg | 151 mg/L | 🟠 Moderate |
| Scarsdale Top Rated | 0.02 mg/L | 🟢 None |
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What Makes College's Water Unique?
Local geology and source profile
College Utilities Corporation supplies drinking water to roughly 27,000 people in College and neighboring parts of the Fairbanks North Star Borough, Alaska. Their primary water source is groundwater drawn from local aquifers within the Tanana River valley. Water treatment takes place at the CUC water treatment plant, where the raw water is filtered, disinfected using chlorination, and subjected to other necessary processes to satisfy EPA standards, as outlined in their 2025 Consumer Confidence Report. The watershed covers the Tanana River lowlands, with groundwater replenishment coming from surface waters and precipitation in this subarctic region.
Geologically, the area is characterized by Quaternary glacial till, alluvial sands, gravels, and silts, with some influence from Tertiary coal-bearing sediments. Crucially, there are no significant limestone or dolomite formations present. This geological makeup means the aquifers deliver water containing very few dissolved minerals, leading to its naturally soft quality and limited buffering capacity. The lack of hard minerals contributes to the water's soft profile.
Homeowners often notice that this soft water means less scale buildup inside pipes, water heaters, and various appliances. This can reduce maintenance requirements and potentially extend the lifespan of your equipment. You might find that dishwashers and coffee makers operate more efficiently, and you'll likely use less soap and detergent. A water softener generally isn't needed and could even add unnecessary sodium to the supply; instead, regular filter cleaning and using pH-balanced cleaning products are good practices. The 2025 CCR confirms all contaminants are within health guidelines, with no reported violations for lead, copper, or PFAS.
Geology & Source: Quaternary glacial and alluvial deposits; low mineral dissolution due to limited contact with carbonate rocks results in soft water
Other Alaska Water Reports
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Frequently Asked Questions
Is College's water safe to drink?
Do I need a water softener in College?
How does College compare to the USA average?
Data Sources & Methodology
Water quality data for College 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.