Chalco Water Hardness & Quality Report (2026)
Water Hardness
~120–179 mg/L
Hardestimated · not lab-verified
Source
groundwater
pH Level
8.3
neutral = 7.0
Lead
0.004 mg/L
✓ Below action level
TDS
384 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 Chalco, your appliances are currently losing 20% efficiency due to mineral buildup.
| Appliance | In Chalco | 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 Chalco compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| ▶ Chalco, Nebraska | ≈ 120–179 mg/L | 3.5 ppt | 🟠 Hard | groundwater |
| Papillion, Nebraska | ≈ 120–179 mg/L | 0 ppt | 🟠 Hard | groundwater |
| La Vista, Nebraska | ≈ 120–179 mg/L | 4.9 ppt | 🟠 Hard | groundwater |
| Omaha, Nebraska | ≈ 120–179 mg/L | 5 ppt | 🟠 Hard | river |
| Bellevue, Nebraska | ≈ 120–179 mg/L | 4.7 ppt | 🟠 Hard | reservoir |
National Benchmark
How Chalco compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ Chalco | ≈ 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 Chalco's Water Unique?
Local geology and source profile
Chalco, Nebraska, an unincorporated community, receives its water supply from either the Papillion-Missouri River Natural Resources District or the City of Omaha Water Department. The primary sources are groundwater wells tapping into the Ogallala Aquifer. Treatment occurs at facilities like the Papillion Water Treatment Plant or Omaha's L Street and Platte West plants, serving residents and businesses in the Chalco area and Sarpy County. This groundwater system is part of the Missouri River Basin, specifically the Platte River sub-basin, where surface recharge supports the aquifer.
The region's water originates from groundwater within the Ogallala Aquifer, a vast formation spanning multiple states. Key geological layers include the Pleistocene Peorian Loess cap and the Miocene Ogallala Group, which consists of sands interspersed with carbonate-cemented layers. These carbonate-rich rocks, specifically limestone and dolomite, are responsible for dissolving significant amounts of calcium and magnesium ions. This geological interaction results in water that is characteristically hard, a common trait for supplies drawn from this particular carbonate-rich area of the High Plains.
This hard water can lead to scale buildup in household appliances like water heaters and dishwashers, potentially reducing their efficiency and lifespan. You might notice that faucet aerators and showerheads clog more frequently, diminishing water flow. Homeowners often find that monthly descaling with vinegar for fixtures and annual flushes for water heaters are necessary maintenance. Installing a whole-house water softener is frequently recommended in areas with water hardness averaging over 200 PPM, as it can significantly protect appliances and improve the lathering of soaps and detergents. While generally safe, occasional nitrates from agriculture are managed through blending and aeration processes, and detections of PFAS are typically below federal limits.
Geology & Source: Ogallala Aquifer; Pliocene to Pleistocene-age sands, gravels, silts, and clays overlying Tertiary sediments; limestone and dolomite layers contribute calcium and magnesium for hard water.
Other Nebraska Water Reports
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Frequently Asked Questions
Is Chalco's water safe to drink?
Do I need a water softener in Chalco?
How does Chalco compare to the USA average?
Data Sources & Methodology
Water quality data for Chalco 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.