West and East Lealman Water Hardness & Quality Report (2026)
Water Hardness
180+ mg/L
Very Hardestimated Β· not lab-verified
Source
groundwater
pH Level
8.1
neutral = 7.0
Lead
0.004 mg/L
β Below action level
TDS
480.5 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 West and East Lealman, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In West and East Lealman | 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 West and East Lealman compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ West and East Lealman, Florida | β 180+ mg/L | 8.2 ppt | π΄ Very Hard | groundwater |
| Lealman, Florida | β 120β179 mg/L | 5.7 ppt | π Hard | groundwater |
| Pinellas Park, Florida | 207 mg/L | 10.4 ppt | π΄ Very Hard | reservoir |
| St. Petersburg, Florida | β 120β179 mg/L | 12 ppt | π Hard | reservoir |
| Gulfport, Florida | β 180+ mg/L | 18 ppt | π΄ Very Hard | reservoir |
National Benchmark
How West and East Lealman compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ West and East Lealman | 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 West and East Lealman home
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What Makes West and East Lealman's Water Unique?
Local geology and source profile
West and East Lealman receive drinking water from Pinellas County Utilities, which serves more than 700,000 residents across the county, including nearby St. Petersburg and Pinellas Park. Supply is drawn primarily from the Floridan Aquifer through 20 production wells and treated at facilities including the Gulfport Water Treatment Plant and the Lealman Advanced Water Treatment Plant. Water is pumped from roughly 400 to 1,000 feet, then aerated, filtered through multimedia beds, and disinfected with chloramines before entering more than 3,600 miles of distribution pipe for homes and businesses.
The source is the Floridan Aquifer system, recharged by rainfall moving through sands into underlying carbonate rock. In this area, the aquifer includes limestone units such as Suwannee Limestone, Avon Park Formation, and Ocala Limestone, with extensive karst development and solution channels. These Paleogene carbonate formations are rich in calcium carbonate, so groundwater picks up dissolved bicarbonates, calcium, and magnesium during subsurface flow. High porosity and permeability increase water-rock interaction, which is why the local supply trends hard compared with waters from less reactive siliceous settings.
With very hard water, scale buildup is a practical issue for pipes, water heaters, dishwashers, and coffee makers, and appliance life can drop, including earlier heater failure. Residents often see stubborn fixture deposits, stiffer laundry, and weaker soap lather. Useful maintenance includes regular vinegar rinses, periodic descaling, and detergent boosters, while a whole-house water softener is strongly recommended for homes prioritizing appliance longevity and cleaning performance. Pinellas County Utilities reports EPA compliance in recent CCRs, including safe lead, copper, and PFAS findings, with treatment controls for disinfection byproducts.
Geology & Source: Floridan Aquifer System karst limestone (Eocene-Oligocene); Avon Park Formation and Ocala Limestone calcium carbonate dissolves during recharge, adding calcium and magnesium; high porosity and permeability drive hard groundwater
Other Florida Water Reports
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Frequently Asked Questions
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How does West and East Lealman compare to the USA average?
Data Sources & Methodology
Water quality data for West and East Lealman 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.