Lincoln Water Hardness & Quality Report (2026)
Water Hardness
180+ mg/L
Very Hardestimated Β· not lab-verified
Source
groundwater
pH Level
8
neutral = 7.0
Lead
0.002 mg/L
β Below action level
TDS
583 mg/L
Est. Daily Cost
$0.91
energy & soap waste
Source: See methodology section below 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 Lincoln, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In Lincoln | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 4.7 yrs | 8.5 yrs | -45% |
| Washing Machine | 6.6 yrs | 12 yrs | -45% |
| Water Heater | 8.3 yrs | 15 yrs | -45% |
Regional Water Comparison
How Lincoln compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Lincoln, Illinois | β 180+ mg/L | 4.7 ppt | π΄ Very Hard | groundwater |
| Springfield, Illinois | β 120β179 mg/L | 6 ppt | π Hard | reservoir |
| Morton, Illinois | 128.5 mg/L | 0 ppt | π Hard | groundwater |
| Bloomington, Illinois | β 120β179 mg/L | 5.2 ppt | π Hard | river |
| Pekin, Illinois | 470 mg/L | 6.2 ppt | π΄ Very Hard | groundwater |
National Benchmark
How Lincoln compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Lincoln | β 180+ mg/L | π΄ High |
| USA National Avg | 151 mg/L | π Moderate |
| Scarsdale Top Rated | 0.02 mg/L | π’ None |
Bring Scarsdale-quality water to your Lincoln home
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What Makes Lincoln's Water Unique?
Local geology and source profile
Illinois American Water - Lincoln District supplies roughly 15,000 residents in Logan County, including the city of Lincoln and nearby areas. Their water comes entirely from wells that draw from the Mahomet-Teays Valley Aquifer, a deep aquifer composed of glacial sand and gravel. The Lincoln Water Treatment Plant is where this groundwater is treated. Disinfection is applied, and zinc orthophosphate is added to help control corrosion. For more information, you can contact Heather Weekley, Water Quality Superintendent, at 309-419-0985.
The water originates from the Mahomet-Teays buried valley aquifer system, which stretches across central Illinois. This system is fed by sand and gravel deposits from Pleistocene glacial outwash, situated above Pennsylvanian bedrock. Because it's a confined aquifer, it gets recharge from distant areas and has little surface interaction. This results in a very hard water supply that's rich in minerals. The geology includes glacial deposits packed with carbonates and formations influenced by limestone, which dissolve significant amounts of calcium and magnesium. This leads to water with high dissolved solids and a hardness that can increase corrosivity when combined with chlorides and sulfates.
This very hard water can lead to substantial scale buildup in your home's pipes, water heaters, dishwashers, and washing machines, which not only reduces their efficiency but also shortens their lifespan. Hot water systems are particularly vulnerable to deposits of calcium carbonate. You might also notice that soap doesn't lather well, leaving a sticky residue on your skin, hair, and clothes. To manage this, regularly descale fixtures and appliances. Installing a whole-house water softener is highly recommended for homes in this area. It will help prevent spotting on glassware, extend the life of your appliances, and make cleaning more effective. Illinois American Water uses zinc orthophosphate for corrosion control, as recommended by the Illinois EPA, and has kept lead and copper levels below action thresholds.
Geology & Source: Mahomet-Teays Valley Aquifer; Pleistocene unconsolidated sands and gravels overlying Pennsylvanian bedrock; limestone and dolomite-rich glacial tills and bedrock impart very high hardness
Other Illinois Water Reports
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Frequently Asked Questions
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Data Sources & Methodology
Water quality data for Lincoln 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 β 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 β values may differ from utility-reported figures.
TDS β 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 β Perfluoroalkyl and Polyfluoroalkyl Substances
EPA UCMR5 (5th Unregulated Contaminant Monitoring Rule, 2023β2025) β 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 β 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.