Hampton Water Hardness & Quality Report (2026)

Hampton, Virginia is served by a municipal water utility operating two distinct source systems providing drinking water to residents throughout the city. Surface water is drawn from the Chickahominy River, and supplementary groundwater is pumped from wells in the Lee Hall area. The utility owns and operates five reservoirs that store and supply water to treatment plants throughout the service area. Both source waters are treated separately at dedicated facilities, then blended together prior to distribution, ensuring consistent water quality is delivered to customers across Hampton's full service area.

The Chickahominy River watershed flows through Virginia's Coastal Plain, a region characterized by unconsolidated sediments, clays, and sands with limited carbonate rock formations. The groundwater supply from Lee Hall wells taps into sedimentary aquifers that naturally contain dissolved minerals. This geological setting — shallow marine deposits with minimal carbonate rock — produces a moderately hard blended water supply typical of the region's hydrogeology.

At moderately hard levels, Hampton residents may notice mineral scale buildup on fixtures and reduced efficiency of water heaters, with slight aesthetic effects such as soap residue. Most household appliances function adequately without treatment, though a water softener may be considered if scale becomes problematic; regular water heater maintenance and periodic descaling of fixtures is advised. Hampton's drinking water contains notable contaminants: lead measures around 1 ppb at the 90th percentile; chromium-6 has been detected at approximately 90 ppt — nearly five times the concentration considered negligible cancer risk; and PFAS contamination near Langley Air Force Base has reached 26,000–220,000 ppt. The utility treats both source waters separately before blending to manage these contaminants.