Using a scale model room to assess the contribution of building material of volcanic origin to indoor radon

Abstract

In the frame of Radon rEal time monitoring System and Proactive Indoor Remediation (RESPIRE), a LIFE 2016 project funded by the European Commission, the contribution of building materials of volcanic origin to indoor radon concentration was investigated. First, total gamma radiation and related outdoor dose rates of geological materials in the Caprarola area (Central Italy) were measured to defi ne main sources of radiation. Second, Rn-222 and Rn-220 exhalation rates of these rocks used as building materials were measured using an accumulation chamber connected in a closed loop with a RAD7 radon monitor. Among others, the very porous “Tufo di Gallese” ignimbrite provided the highest values. This material was then used to construct a scale model room of 62 cm × 50 cm × 35 cm (inner length × width × height, respectively) to assess experimental radon and thoron activity concentration at equilibrium and study the effects of climatic conditions and different coatings on radon levels. A fi rst test was carried out at ambient temperature to determine experimental Rn-222 and Rn-220 equilibrium activities in the model room, not covered with plaster or other coating materials. Experimental Rn-222 equilibrium was recorded in just two days demonstrating that the room “breaths”, exchanging air with the outdoor environment. This determines a dilution of indoor radon concentration. Other experiments showed that inner covers (such as plasterboard and different kinds of paints) partially infl uence Rn-222 but entirely cut the short-lived Rn-220. Finally, decreases in ambient temperature reduce radon exhalation from building material and, in turn, indoor activity concentration.