Miami Water Hardness & Quality Report (2026)
Water Hardness
8 grains per gallon
Source
groundwater
pH Level
7.6
neutral = 7.0
Lead
0.003 mg/L
β Below action level
TDS
215 mg/L
Est. Daily Cost
$0.37
energy & soap waste
Source: USGS Water Quality Portal 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 Miami, your appliances are currently losing 18% efficiency due to mineral buildup.
| Appliance | In Miami | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 5.1 yrs | 8.5 yrs | -40% |
| Washing Machine | 8.5 yrs | 12 yrs | -29% |
| Water Heater | 10.1 yrs | 15 yrs | -33% |
Regional Water Comparison
How Miami compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Miami, Florida | 137 mg/L | 6.9 ppt | π Hard | groundwater |
| Little Havana, Florida | 185.5 mg/L | 8.4 ppt | π΄ Very Hard | groundwater |
| Allapattah, Florida | 318 mg/L | 12.6 ppt | π΄ Very Hard | groundwater |
| Miami Beach, Florida | 85.5 mg/L | 5.3 ppt | π‘ Moderately Hard | groundwater |
| Brownsville, Florida | 127.5 mg/L | 6.6 ppt | π Hard | groundwater |
National Benchmark
How Miami compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Miami | 137 mg/L | π Moderate |
| USA National Avg | 150 mg/L | π Moderate |
| Badger Top Rated | 8.5 mg/L | π’ None |
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What Makes Miami's Water Unique?
Local geology and source profile
Miami's water is supplied by Miami-Dade Water and Sewer Department (WASD), drawing entirely from the Biscayne Aquifer β one of the most productive surficial aquifers in the United States and the sole source of drinking water for most of Miami-Dade County. The aquifer is accessed through a network of well fields across Miami-Dade County, with the largest being the Northwest Wellfield, Hialeah-Preston, and Alexander Orr Jr. Wellfield systems. The Alexander Orr Jr. Water Treatment Plant and the Hialeah and John E. Preston Water Treatment Plants treat groundwater before distribution. Miami-Dade's water system is one of the largest groundwater-based systems in the United States, serving over 2.3 million customers with no surface reservoir dependency.
Miami's moderate hardness of 137 mg/L is a product of the Biscayne Aquifer's unique geological character. The aquifer is contained within the Miami Limestone (Pleistocene age) and the underlying Fort Thompson Formation β porous, vuggy carbonate rocks formed from ancient coral reef and marine shell deposits laid down 125,000β500,000 years ago when sea level stood higher than today. Rainwater percolating through these highly porous limestone formations dissolves calcium carbonate at moderate rates, producing water of intermediate hardness typical of Florida coastal aquifer systems. The Biscayne Aquifer's shallow depth and high porosity also mean it is highly vulnerable to saltwater intrusion from Biscayne Bay, which WASD manages through careful well field operations.
Miami's moderately hard water is manageable in daily household use. White mineral deposits form gradually on showerheads and faucets, soap and detergent perform reasonably well, and glassware develops mild spotting over time without rinse-aid. The tropical climate means evaporation can concentrate minerals rapidly on outdoor fixtures and pool surrounds. Descaling showerheads and coffee machines every 2β3 months is standard practice, and dishwasher rinse-aid effectively eliminates glassware filming. A basic carbon-block filter also addresses any taste variation from the treatment process, which Miami residents occasionally notice during seasonal wellfield switching.
Geology & Source: Biscayne Aquifer over porous Miami Limestone and Fort Thompson formation β moderate hardness from coral rock