Autotrol Uranium & Radium System

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What Happens When Uranium-Radium Is Left Untreated Over Time

Radium-226, part of the uranium-radium family, is naturally present in groundwater sourced from deep aquifers like Chesterfield County’s 211MDDF. While detections here have remained below federal safety thresholds, prolonged exposure in untreated water can lead to issues associated with gradual accumulation. The primary concern is not immediate safety but ensuring levels remain controlled to meet long-term health guidelines that regulate radionuclides in drinking water.

Distinguishing Uranium-Radium from Other Commonly Confused Water Concerns

Uranium-radium’s identification differs significantly from common water issues such as iron or manganese staining or microbial contamination. Unlike these physical or biological concerns, uranium-radium is a naturally occurring radioactive element. It does not cause taste or odor problems and is only measurable through specialized laboratory analysis, not by normal visual inspection or household testing kits.

How Uranium-Radium Enters Groundwater in Chesterfield County

The uranium-radium detected in Chesterfield County’s aquifer 211MDDF derives from natural geologic sources within the rock formations at depths ranging from approximately 220 to 458 feet. Radioactive decay of uranium-rich minerals releases radium into groundwater over long timescales. This process is consistent across wells sampled in the area and is not a result of surface pollution or man-made contamination.

Differences in Water Quality After Treatment With the Autotrol Uranium & Radium System

The Autotrol Uranium & Radium System removes radium from household water by targeting the dissolved radioactive particles through a treatment media designed specifically for this purpose. Treated water at the tap typically shows significantly reduced radionuclide levels, providing peace of mind that concentrations remain well within safe federal standards. The system ships ready to configure without needing specialized infrastructure beyond routine household plumbing connections.

How Sampling Depth and Well Characteristics Affect What You Should Expect

Samples taken from wells 220 to 458 feet deep in the Chesterfield County aquifer show a range of radium-226 levels from 0.0 to 6.0 pCi/L, with a median near 0.9 pCi/L. Shallow wells or surface water sources generally do not exhibit these radionuclide profiles. Understanding your well depth and water source is important because shallower or different geologic formations may have very different water chemistry and require alternative or no treatment.

Interpreting Certified Laboratory Tests for Uranium-Radium

Testing for radium-226 in water requires certified laboratories using precise measurement techniques. Laboratory reports provide concentrations in picocuries per liter (pCi/L), indicating the radioactivity level from radium decay. In Chesterfield County’s aquifer, none of the 29 tested results from 11 wells exceeded federal maximum contaminant levels. A laboratory report helps determine if treatment with specialized equipment like the Autotrol System is advisable based on your actual well water conditions rather than area averages.

Government sampling in Chesterfield County’s 211MDDF aquifer from 2011 to 2014 documented radium-226 presence in all tested wells, never exceeding legal limits. For detailed data, visit the U.S. Geological Survey water monitoring site covering this area.

Where this information comes from

Source: USGS groundwater sampling. Sampled 2014-01-21. 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-226 in the 211MDDF aquifer (Chesterfield County): 29 results from 11 wells, median 0.9 pCi/L, range 0.0-6.0 pCi/L; none above any federal threshold