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radon

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radon
Number86
CategoryNoble gas

radon. It is a radioactive, colorless, odorless, and tasteless noble gas, formed naturally from the decay of uranium and thorium in the Earth's crust. Its most stable isotope, radon-222, has a half-life of 3.8 days and decays into a series of solid radioactive progeny, including polonium-218 and lead-214. Due to its radioactivity and gaseous nature, it can accumulate indoors, posing a significant public health risk as the second leading cause of lung cancer after tobacco smoking.

Properties and characteristics

Radon is a member of the noble gas group in the periodic table, sharing this classification with elements like helium, neon, and argon. It is the densest known gas under standard conditions and is chemically inert, though it can form fleeting compounds such as radon fluoride. The element is intensely radioactive, with all its isotopes being unstable; radon-222, a decay product of radium-226 in the uranium-238 decay chain, is the most common and epidemiologically significant. Other isotopes like radon-220, also called thoron, originates from the thorium-232 decay series and has a much shorter half-life of 55 seconds. The decay of these isotopes emits alpha particles, which are a type of high-energy, high-mass radiation consisting of two protons and two neutrons.

Occurrence and sources

Radon is generated continuously in rocks and soils from the radioactive decay of trace amounts of uranium and thorium, elements found in granitic rock, shale, phosphate rock, and certain types of sandstone. Its concentration in the outdoor atmosphere is typically very low, as it readily disperses, but it can accumulate to dangerous levels inside buildings, entering through cracks in foundations, gaps around pipes, sump pits, and construction joints. Geographically, areas underlain by uranium-rich bedrock, such as parts of Cornwall, the Appalachian Mountains, and the Canadian Shield, often have higher natural background levels. It is also found in some groundwater supplies, particularly from deep wells drilled into rock with high radium content, and can be released into indoor air during activities like showering. The element was first isolated and identified in 1900 by the German physicist Friedrich Ernst Dorn while studying the decay chain of radium.

Health effects and risks

Inhalation of radon decay products is a established cause of lung cancer, as recognized by major health agencies including the World Health Organization, the United States Environmental Protection Agency, and the International Agency for Research on Cancer. Once inhaled, the solid radioactive decay products, such as polonium-218, can deposit on the bronchial epithelium and emit alpha particles that damage cellular DNA. This risk is significantly amplified by concurrent exposure to tobacco smoke, with smokers facing a much higher synergistic risk. The Surgeon General of the United States has warned that it is the second leading cause of lung cancer nationally, resulting in thousands of deaths annually. Studies of underground miners, such as those who worked in the Schneeberg mines and the Port Radium site, provided the first definitive epidemiological evidence linking prolonged exposure to increased cancer incidence.

Measurement and mitigation

Concentrations are measured in becquerels per cubic meter (Bq/m³) or picocuries per liter (pCi/L), typically using passive detection devices like alpha-track detectors, charcoal canisters, or electret ion chambers. Short-term testing kits are available for initial screening, but long-term testing over at least three months is recommended for an accurate assessment of average exposure. If elevated levels are found, mitigation techniques include sub-slab depressurization, which uses a fan and piping system to draw the gas from beneath the building's foundation and vent it outdoors above the roofline. Other methods involve sealing major entry routes, improving basement ventilation, and installing vapor barriers. The American Society of Heating, Refrigerating and Air-Conditioning Engineers provides standards for mitigation in new construction, while many national radon programs offer guidance for existing homes.

Regulation and guidelines

Many countries and international bodies have established action levels and guidelines for concentration in indoor air and drinking water. The World Health Organization recommends a reference level of 100 Bq/m³, below which mitigation should be considered. In the United States, the Environmental Protection Agency sets an action level of 148 Bq/m³ (4 pCi/L) for homes and schools, and radon-resistant construction techniques are incorporated into building codes in many high-risk areas. The European Union has issued a directive that sets a national reference level for member states, not to exceed 300 Bq/m³ for existing dwellings. For public water supplies, the EPA has proposed a maximum contaminant level, while some states like New Jersey and Maine have implemented their own stringent regulations. Occupational exposure limits for workers, such as in mines, are enforced by agencies like the Occupational Safety and Health Administration and the Mine Safety and Health Administration.

Category:Chemical elements Category:Noble gases Category:Radioactivity