Learn About Radon
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Take a Look at the Information Regarding Radon
Radon is a radioactive, odorless, colorless, tasteless, and chemically inert gas that was first discovered in 1910. Radioactive elements in rocks find their way into the soil as they are worn down over time, and in certain instances, can migrate through soil to enter homes in quantities that are great enough to be a hazard to your health.
For these to instances to occur, there must be a source of radon, permeable soil, and a conduit into your home. Common points of entry include, but are not limited to, porous basement floors/walls, cracks in concrete floors or slabs, and openings around utility accesses. Call us today to learn more.
Certain areas are susceptible to radon accumulation as well:
- Buildings constructed in areas where the rocks contain higher than average quantities of uranium
- Buildings that are created over uranium-bearing veins and granite pegmatites
- Geographic areas containing radium contamination
- Property in areas that contain high concentrations of radon in the groundwater
- Residential or commercial buildings built on or constructed with radioactive materials such as uranium mill tailings.
Houses built in other areas of the Piedmont Province, especially those built on the zone of phyllites running through central Montgomery, western Howard, eastern Frederick, and central Carroll Counties, frequently have indoor radon values exceeding the levels considered safe by the Environmental Protection Agency.
Most sands and gravels of the Maryland Coastal Plain have been well oxidized, with the majority of the uranium leached out and carried away. Unfortunately, certain Coastal Plain sediments contain uranium-rich phosphate beds which resist oxidation, so homes built on these foundations are at risk for elevated radon values.
Call the team at Affordable Radon Reduction Inc to learn more.
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Have a question about radon that isn't answered here? Please give us a call to get an answer today or take a look at one of these additional resources.
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