St. Johns Water Hardness & Quality Report (2026)
Water Hardness
180+ mg/L
Very Hardestimated Β· not lab-verified
Source
groundwater
pH Level
7.8
neutral = 7.0
Lead
0.003 mg/L
β Below action level
TDS
340.7 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 St. Johns, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In St. Johns | 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 St. Johns compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ St. Johns, Florida | β 180+ mg/L | 6.8 ppt | π΄ Very Hard | groundwater |
| Fruit Cove, Florida | β 180+ mg/L | 5 ppt | π΄ Very Hard | groundwater |
| Fleming Island, Florida | β 120β179 mg/L | 10.9 ppt | π Hard | groundwater |
| Palm Valley, Florida | β 180+ mg/L | 8 ppt | π΄ Very Hard | groundwater |
| Bellair-Meadowbrook Terrace, Florida | β 120β179 mg/L | 11.7 ppt | π Hard | groundwater |
National Benchmark
How St. Johns compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ St. Johns | 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 St. Johns's Water Unique?
Local geology and source profile
St. Johns County Utility Department manages water services across multiple systems including Bartram Oaks, Eagle Creek, Fruit Cove, North Beach, Northeast Utilities, Northwest Utilities, and Ponte Vedra Utility System. The primary source is groundwater drawn via wells from the Floridan aquifer, with treatment at plants serving the Saint Johns Forest Grid and Saint Johns North Grid. There are no surface water reservoirs or rivers involved; the supply is purely groundwater for the county, including the community of Saint Johns (zip codes such as 32092).
Recharge comes from rainfall percolating into the Floridan aquifer across north and central Florida rather than from a traditional surface watershed. The aquifer consists of Eocene limestone formations β the Avon Park and Ocala groups β with extensive karst dissolution features enhancing permeability. Pleistocene marine transgression left residual saline influences in deeper sections, particularly in southeastern areas, shaping a mineral-rich profile. This limestone geology dissolves to yield a hard supply with elevated dissolved solids.
Very hard water promotes rapid scale buildup in pipes, water heaters, dishwashers, washing machines, and fixtures, reducing efficiency and lifespan. Affected appliances show white deposits, clogged aerators, and higher energy use. Regular vinegar descaling, annual heater flushing, and low-flow fixtures help mitigate these effects. A water softener is strongly recommended to prevent damage and extend appliance life. pH typically ranges 7β8; lead and copper rule compliance is met with low action levels. Naturally elevated chloride from saline intrusion is notable in southeastern areas; treatment involves disinfection with chlorine and aeration at some plants, with hardness left untreated.
Geology & Source: Upper Floridan aquifer β Eocene Avon Park and Ocala Limestones; karst dissolution features enhance permeability and release calcium and magnesium, producing hard groundwater; Pleistocene saline intrusion in southeastern areas
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Frequently Asked Questions
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Data Sources & Methodology
Water quality data for St. Johns 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.