Sycamore Water Hardness & Quality Report (2026)
Water Hardness
180+ mg/L
Very Hardestimated Β· not lab-verified
Source
groundwater
pH Level
7.9
neutral = 7.0
Lead
0.004 mg/L
β Below action level
TDS
302.5 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 Sycamore, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In Sycamore | 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 Sycamore compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Sycamore, Illinois | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| DeKalb, Illinois | β 120β179 mg/L | 0 ppt | π Hard | groundwater |
| Wasco, Illinois | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Village of Campton Hills, Illinois | β 180+ mg/L | 5.9 ppt | π΄ Very Hard | river |
| Huntley, Illinois | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
National Benchmark
How Sycamore compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Sycamore | 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 Sycamore's Water Unique?
Local geology and source profile
The City of Sycamore Water Division serves approximately 17,600 residents in DeKalb County, Illinois. The utility operates five deep wells that access sandstone aquifers, with no surface water component. The Water Division office is located at 202 E. Page Street, Sycamore, IL 60178 (815-895-3545). According to the city's official FAQ, the water supply is classified as very hard, exceeding 180 mg/L of mineral hardness. The utility reports full compliance with all EPA drinking water requirements and sampling and testing standards.
Sycamore's groundwater originates from Paleozoic-age sandstone formations typical of northern Illinois, characteristic of the Illinois Basin. These deep aquifers have undergone extensive contact with mineral-rich sedimentary rock over geological timescales, resulting in elevated dissolved calcium and magnesiumβthe primary drivers of hardness. Thick sequences of sandstone and limestone create naturally mineralized groundwater, explaining the very hard supply and the region's widespread need for water treatment.
At the very hard classification, residents experience significant scale buildup on fixtures, reduced soap effectiveness, and accelerated wear on water heaters and appliances. The city recommends water softening systems to extend appliance lifespan. The utility applies a phosphate blend corrosion control treatment at individual well sites to manage lead and copper leaching in the distribution system, though source groundwater is lead-free. Third-party analyses have flagged contaminants including Di(2-ethylhexyl) adipate, m-Xylene, 1,1,2-Trichloroethane, and Monochloroacetic acid above EPA health-based guidelines; the city maintains regular testing and publishes results.
Geology & Source: Five municipal wells tap Paleozoic-age sandstone aquifers in northern Illinois; thick sedimentary strata with prolonged water-rock contact dissolve high concentrations of calcium and magnesium carbonates, producing very hard supply
Other Illinois Water Reports
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Frequently Asked Questions
Is Sycamore's water safe to drink?
Do I need a water softener in Sycamore?
How does Sycamore compare to the USA average?
Data Sources & Methodology
Water quality data for Sycamore 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.