Great Bend Water Hardness & Quality Report (2026)
Water Hardness
180+ mg/L
Very Hardestimated Β· not lab-verified
Source
groundwater
pH Level
8.5
neutral = 7.0
Lead
0.009 mg/L
β Below action level
TDS
1551.9 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 Great Bend, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In Great Bend | 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 Great Bend compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Great Bend, Kansas | β 180+ mg/L | 704.2 ppt | π΄ Very Hard | groundwater |
| Hays, Kansas | β 120β179 mg/L | 31.7 ppt | π Hard | groundwater |
| Hutchinson, Kansas | β 120β179 mg/L | 0 ppt | π Hard | groundwater |
| McPherson, Kansas | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Salina, Kansas | β 120β179 mg/L | 75 ppt | π Hard | reservoir |
National Benchmark
How Great Bend compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Great Bend | β 180+ mg/L | π΄ High |
| USA National Avg | 151 mg/L | π Moderate |
| Scarsdale Top Rated | 0.02 mg/L | π’ None |
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What Makes Great Bend's Water Unique?
Local geology and source profile
The City of Great Bend Water Division, located at 200 Kiowa Rd, PO Box 1168, Great Bend, KS 67530, serves the community in Barton County. This utility draws its water supply primarily from groundwater aquifers, specifically the Dakota Formation and Meade Formation. These formations are located within the Great Bend Prairie and Arkansas Valley watersheds of central Kansas. While specific treatment plant names aren't detailed, the City of Great Bend adheres to EPA standards, reporting no violations since 2023 and maintaining low lead levels. The groundwater from these Cretaceous-period sandstone and limestone aquifers is generally suitable for domestic, stock, irrigation, and public supply needs.
The water originates from sandstone and limestone aquifers within the Dakota Formation and Meade Formation, part of the Great Bend Prairie region. These Cretaceous-period formations, underlying Barton County and extending into Stafford County, are characterized by mineral-rich sedimentary rocks. As groundwater percolates through these layers, calcium and magnesium dissolve, naturally imparting a hard character to the supply. The Meade Formation, situated beneath the prairie, yields moderately hard water, though some areas in northeastern Stafford County experience higher mineralization.
Homeowners may notice accelerated scale buildup in pipes, water heaters, dishwashers, and washing machines when the water is very hard, which can reduce efficiency and shorten appliance lifespan. You might also experience diminished soap lathering and find spots on dishes. Regular descaling of appliances and vinegar soaks for fixtures can help manage this. Given the water's natural hardness, installing a water softener is strongly recommended to protect plumbing and mitigate these effects. The utility conducts frequent testing to ensure compliance with EPA standards, offering 24/7 emergency response.
Geology & Source: Dakota Formation and Meade Formation sandstone and limestone aquifers; limestone and mineral-rich rock formations dissolve calcium and magnesium, contributing to hard water
Other Kansas Water Reports
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Frequently Asked Questions
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Data Sources & Methodology
Water quality data for Great Bend 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.