Assessment of the Radioactivity, Metals Content and Mineralogy of Granodiorite from Calabria, Southern Italy: A Case Study

Author:

Dattola Luigi12ORCID,Belvedere Alberto3,D’Agostino Maurizio3ORCID,Faggio Giuliana4ORCID,Majolino Domenico5ORCID,Marguccio Santina3,Messina Giacomo4,Messina Maurizio3,Mottese Antonio Francesco4,Paladini Giuseppe5ORCID,Venuti Valentina5ORCID,Caridi Francesco5ORCID

Affiliation:

1. Agenzia Regionale per la Protezione dell’Ambiente della Calabria (ARPACal)—Centro Regionale Geologia e Amianto, Via della Pace, 87050 Castrolibero, Italy

2. Dipartimento di Ingegneria dell’Ambiente (DIAm), Università della Calabria, Via Pietro Bucci, 87036 Rende, Italy

3. Agenzia Regionale per la Protezione dell’Ambiente della Calabria (ARPACal)—Dipartimento di Reggio Calabria, Via Troncovito SNC, 89135 Reggio Calabria, Italy

4. Dipartimento di Ingegneria dell’Informazione, delle Infrastrutture e dell’Energia Sostenibile (DIIES), Università “Mediterranea”, Loc. Feo di Vito, 89122 Reggio Calabria, Italy

5. Dipartimento di Scienze Matematiche e Informatiche, Scienze Fisiche e Scienze della Terra, Università degli Studi di Messina, V.le F. Stagno D’Alcontres, 31, 98166 Messina, Italy

Abstract

In this paper, an assessment of the natural radioactivity level, radon exhalation, metal contamination, and mineralogy of a granodiorite rock sample from Stilo, in the Calabria region, Southern Italy is presented as a case study. This rock was employed as a building material in the area under study. The specific activity of 226Ra, 232Th and 40K natural radioisotopes was assessed through high-purity germanium (HPGe) gamma-ray spectrometry. Then, several indices such as the absorbed gamma dose rate (D), the annual effective dose equivalent (AEDE), the activity concentration index (ACI) and the alpha index (Iα), were quantified to determine any potential radiological health risk related to radiation exposure from the analyzed rock. Furthermore, E-PERM electret ion chambers and inductively coupled plasma mass spectrometry (ICP-MS) measurements were carried out to properly quantify the radon exhalation rate and any possible metal pollution, respectively. In particular, to further address metal pollution factors, the geo-accumulation index (Igeo) was calculated to properly address the toxicity levels of the ecosystem originating from the detected metals. Finally, with the aim of successfully discriminating the provenance of such naturally occurring radionuclides, a combined approach involving X-ray diffraction (XRD) and µ-Raman spectroscopy was employed for the identification of the main radioisotope-bearing minerals characterizing the investigated granodiorite. The results achieved in this case study can be taken as the basis for further inquiries into background levels of radioactivity and chemical contamination in natural stone employed as building materials.

Publisher

MDPI AG

Reference70 articles.

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3. Radon radioactivity in groundwater from the Calabria region, south of Italy;Caridi;J. Instrum.,2016

4. 238U, 226Ra, 210Pb, 232Th and 40K activities in soil profiles of the Flysch sector (Central Spanish Pyrenees);Navas;Appl. Radiat. Isot.,2002

5. Radioactivity levels in rocks of North Karnataka, India;Kerur;Indian J. Pure Appl. Phys.,2010

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