Fleck Uranium & Radium System

Fleck Uranium & Radium System

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Distinguishing Uranium-Radium from Other Water Quality Issues

In Gloucester County's aquifer 121CKKD, U.S. Geological Survey groundwater samples from 31 wells show detectable levels of radium-224 between 0.03 and 16.8 pCi/L, with a median of 1.865 pCi/L. Importantly, none exceeded federal thresholds. This measurement differs from common water quality concerns like iron or hardness, which affect water clarity and taste but do not involve radioactive elements. Uranium-radium radiological counts relate to specific radioactive isotopes naturally present in the geology and are monitored for regulatory compliance rather than aesthetic impacts.

Impact of Plumbing Materials and Age Separate from Source Water

While source water carries uranium-radium, household plumbing components do not contribute to these isotopes. Old or new pipes, regardless of material, neither add nor remove uranium-radium from water. Therefore, the levels measured in the area's aquifer reflect natural groundwater conditions rather than changes from plumbing corrosion or leaching. This separation means treatment decisions focus on source water quality, not plumbing system characteristics.

Additional Considerations for Commercial or Industrial Operators versus Households

Commercial and industrial users face added scrutiny regarding uranium and radium concentrations due to higher water volumes and regulatory reporting requirements. Such operators often need detailed isotopic profiling, continuous monitoring, and compliance documentation. In contrast, households primarily require confirmation of levels through localized testing and selection of appropriate treatment capacity based on typical daily water usage. The larger scale and complexity in commercial contexts necessitate approaches that extend beyond standard residential equipment capabilities.

Water Changes at the Tap After Using the Fleck Uranium & Radium System

The Fleck Uranium & Radium System utilizes specialized ion exchange technology to reduce uranium and radium concentrations from groundwater before it reaches household taps. Post-treatment water typically shows significantly lowered levels of these isotopes, improving peace of mind and maintaining compliance with safety standards. The system ships ready to configure and provides a grain capacity of 32,000, sufficient for many residential point-of-entry applications. Users can expect no adverse changes in water color, taste, or odor directly related to this treatment.

How Uranium and Radium Enter Gloucester County Groundwater

In Gloucester County, uranium and radium occur naturally in the soil and rock comprising aquifer 121CKKD. Groundwater flows through these mineral formations, dissolving trace amounts of radium-224 detectable in well samples. This process is influenced by geologic composition and groundwater movement but not by human activity such as plumbing infrastructure. Understanding this natural origin clarifies why uranium-radium presence is a source water issue addressed at the point of use rather than through municipal treatment or distribution changes.

What Not to Conclude from Area Sampling Data

It is important to remember that the reported radium-224 levels represent aggregated results from multiple area wells during 2010 to 2018; they do not specify any individual household’s water quality. Detection alone is not a violation of safety standards, nor does it confirm unsafe water. Testing your own well water is the only way to establish the specific uranium and radium levels present. Area data should guide awareness and treatment consideration but not create assumptions about your home’s water condition.

Where this information comes from

Source: USGS groundwater sampling. Sampled 2018-09-04. These figures describe groundwater sampled in this area. They are not a test of any individual private well - only a test of that well can establish its own water.

On record: U.S. Geological Survey sampling of Radium-224 in the 121CKKD aquifer (Gloucester County): 38 results from 31 wells, median 1.865 pCi/L, range 0.03-16.8 pCi/L; none above any federal threshold

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