Reading Water Hardness & Quality Report (2026)
Water Hardness
1.2 grains per gallon
Source
reservoir
pH Level
7.1
neutral = 7.0
Lead
0.001 mg/L
β Below action level
TDS
31.4 mg/L
Est. Daily Cost
$0.05
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 Reading, your appliances are currently losing 3% efficiency due to mineral buildup.
| Appliance | In Reading | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 8.9 yrs | 8.5 yrs | β |
| Washing Machine | 12.8 yrs | 12 yrs | β |
| Water Heater | 14.8 yrs | 15 yrs | -1% |
Regional Water Comparison
How Reading compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Reading, Massachusetts | 20.5 mg/L | 4.5 ppt | π’ Soft | reservoir |
| Wakefield, Massachusetts | 47.5 mg/L | 6.4 ppt | π’ Soft | reservoir |
| Stoneham, Massachusetts | 65.5 mg/L | 7.6 ppt | π‘ Moderately Hard | reservoir |
| North Reading, Massachusetts | 121.5 mg/L | 11.6 ppt | π Hard | reservoir |
| Melrose, Massachusetts | 36 mg/L | 5.6 ppt | π’ Soft | reservoir |
National Benchmark
How Reading compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Reading | 20.5 mg/L | π’ None |
| USA National Avg | 150 mg/L | π Moderate |
| Badger Top Rated | 8.5 mg/L | π’ None |
Bring Badger-quality water to your Reading home
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What Makes Reading's Water Unique?
Local geology and source profile
Reading, Massachusetts, in Middlesex County north of Boston, receives its municipal water from the Reading Water Division, which draws from local surface water reservoirs in the Ipswich River headwaters watershed and supplementary supply from the Massachusetts Water Resources Authority (MWRA) metropolitan system. Reading's local reservoirs β including Birch Meadow Reservoir and associated impoundments β collect surface runoff and shallow groundwater from the glaciated Essex-Middlesex upland north of Boston. The MWRA connection provides backup capacity from Quabbin Reservoir during peak demand periods.
The extraordinarily soft 20.5 mg/L hardness and ultra-low TDS of 31.4 mg/L place Reading among the softest municipal supplies in the United States. The Reading watershed drains across Precambrian Andover Granite and Paleozoic metasedimentary rocks β ancient crystalline igneous and metamorphic formations with absolutely no soluble carbonate mineral content. New England's Precambrian basement rock (granites, gneisses, metavolcanics) and overlying thin glacial soils produce naturally ultra-soft rainwater runoff with almost no dissolved mineral accumulation. Quabbin Reservoir water adds similarly ultra-soft supply from the Central Highland watershed.
At 20.5 mg/L, Reading has exceptionally soft water β essentially zero scale formation under any household conditions. Soap lathers cloud-like, appliances need descaling at most once a year under normal use, and glassware emerges spotless from the dishwasher without any rinse aid. The primary consideration with Reading's ultra-soft supply is its aggressive corrosive chemistry β at this very low hardness, the water can slowly leach trace copper or lead from household plumbing, particularly in older homes. Reading DPW manages pH carefully to reduce corrosivity, but residents in pre-1986 homes should flush cold taps for 30 seconds before drinking any first-draw water. The PFAS level of 4.5 ppt is worth noting for a community this close to the Route 128 technology corridor.
Geology & Source: Reading in Middlesex County draws from Reading's Local Reservoir System on the Ipswich River watershed headwaters and supplementary MWRA supply β the drainage area overlies Precambrian Andover Granite and Paleozoic metasedimentary rocks with essentially zero carbonate mineral content β ancient crystalline New England bedrock produces exceptionally soft water at just 20.5 mg/L with TDS of only 31.4 mg/L.