Pregled bibliografske jedinice broj: 1108840
The influence of geological formations on geogenic radon potential and/or indoor radon Croatia
The influence of geological formations on geogenic radon potential and/or indoor radon Croatia // JRC Conference and Workshop reports Book of Abstract 2nd International Workshop on the European Atlas of Natural Radiation / Tollefsen, Tore ; Cinelli, Giorgia ; De Cort ; Marc (ur.).
Lahti: Publications Office of the European Union,, 2017. str. 46-46 doi:10.2760/7074 (predavanje, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 1108840 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
The influence of geological formations on geogenic
radon potential and/or indoor radon Croatia
Autori
Radolić, Vanja ; Poje Sovilj, Marina ; Miklavčić, Igor ; Stanić, Denis ; Vuković, Branko
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
JRC Conference and Workshop reports Book of Abstract 2nd International Workshop on the European Atlas of Natural Radiation
/ Tollefsen, Tore ; Cinelli, Giorgia ; De Cort ; Marc - Lahti : Publications Office of the European Union,, 2017, 46-46
ISBN
978-92-79-74130-2
Skup
2nd International Workshop on the European Atlas of Natural Radiation
Mjesto i datum
Verbania, Italija, 06.11.2017. - 09.11.2017
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
geological structures ; radon concentration ; soil permeability
Sažetak
In the last few years, the targeted surveys of indoor radon in homes as well as in public buildings with high occupancy (kindergartens and schools) were performed in several counties in Croatia with different geological formations. In the southern part of Croatia, geological structure mainly consists of a limestone plateau and dolomites formed in the Jurassic and Late Cretaceous while carbonate rocks, especially flysch, during Paleogene period. The northern part consists geologically mainly of sandstones and soft clay formed during the Neogene and Quaternary periods. Sediments are of gravels, loess and silts and are all the products of mostly continental environments and alluvial fans. Differences in geological structures of these two areas inevitable suppose to have, as a consequence, very different geogenic radon potential (GRP). Indoor radon was measured by track etched detectors which were randomly distributed in homes, schools and kindergartens across the whole geographic areas and the number of detectors dependend on population densities of the investigated areas. Radon concentrations in soil gas in Croatia were measured with the AlphaGUARD and RM-2 measuring systems while soil permeability was measured by Radon-JOK permeameter. A detailed GRP map based on in-field soil gas radon and soil gas permeability measurements was carried out using “Neznal’s” approach. The relationship between geological formations and GRPs or indoor radon were examined. According to the obtained results, the criteria for identification of “radon prone area”, as part of the future National Action Plan, for radon is proposed and discussed.
Izvorni jezik
Engleski
Znanstvena područja
Fizika
POVEZANOST RADA
Ustanove:
Sveučilište u Osijeku - Odjel za fiziku
Profili:
Denis Stanić
(autor)
Igor Miklavčić
(autor)
Marina Poje Sovilj
(autor)
Branko Vukovic
(autor)
Vanja Radolić
(autor)