Where does the radon gas come from?
Radon is a colourless and very volatile radioactive gas coming from the nuclear decay of radium, generated by the decay of uranium, naturally present in the soil and rocks, above all of volcanic origin, in water, in tombs and in the materials used in construction. In confined environments, it can accumulate, reaching concentrations such as to become a significant source of health risk.
On the basis of numerous epidemiological studies, radon has been classified by the International Agency for Research on Cancer (IARC-WHO) as a Group 1 human carcinogen, representing the second cause of lung cancer immediately after tobacco. For most people, the main exposure to radon occurs at home, in the workplace and in schools, as it spreads from the ground or building materials and reaches the interior of the building through cracks, attacks of walls to the floor, the passages of various electrical, thermal or hydraulic systems.
Radon levels vary according to the time of day and year, so long-term measures are needed to obtain an average of time fluctuations. In confined working environments or with people in the basement and underground (e.g. laboratories, kitchens, taverns, wine bars, meeting rooms, gyms), gas tends to accumulate until it reaches concentrations that can pose a major health risk. The buildings most at risk are those built on soils of volcanic origin, highly permeable or built with materials such as tuff, pozzolane, granite. Italy is a country at risk, especially in historic centers, where it is easy to meet local places directly on the ground without any barrier.
The mapping of radon risk areas is entrusted to ARPA (Regional Environmental Protection Agencies).


