A new geostatistical tool for the analysis of the geographical variability of the indoor radon activity
The population is continuously exposed to a background level of ionizing radiation due to the natural radioactivity and, in particular, with radon (222Rn). Radon gas has been classified as the second leading cause of lung cancer after tobacco smoke [1]. In the confined environment, radon concentrati...
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doaj-7277a5aabba84b4bb3ab6cfbba9f94be2021-09-06T19:22:40ZengSciendoNukleonika0029-59222020-06-016529910410.2478/nuka-2020-0015A new geostatistical tool for the analysis of the geographical variability of the indoor radon activityLoffredo Filomena0Scala Antonio1Adinolfi Guido Maria2Savino Federica3Quarto Maria4Advanced Biomedical Science Department, University of Naples, Federico II, Corso Umberto I, 40-80138 Naples, Italy, and National Institute of Nuclear Physics (INFN), Strada Comunale Cinthia, 80126, Naples, ItalyDepartment of Physics, “E. Pancini”, University of Naples, Federico II, Corso Umberto I, 40-80138 Naples, ItalyDepartment of Physics, “E. Pancini”, University of Naples, Federico II, Corso Umberto I, 40-80138 Naples, ItalyAdvanced Biomedical Science Department, University of Naples, Federico II, Corso Umberto I, 40-80138 Naples, ItalyAdvanced Biomedical Science Department, University of Naples, Federico II, Corso Umberto I, 40-80138 Naples, Italy, and National Institute of Nuclear Physics (INFN), Strada Comunale Cinthia, 80126, Naples, ItalyThe population is continuously exposed to a background level of ionizing radiation due to the natural radioactivity and, in particular, with radon (222Rn). Radon gas has been classified as the second leading cause of lung cancer after tobacco smoke [1]. In the confined environment, radon concentration can reach harmful level and vary accordingly to many factors. Since the primary source of radon in dwellings is the subsurface, the risk assessment and reduction cannot disregard the identification of the local geology and the environmental predisposing factors. In this article, we propose a new methodology, based on the computation of the Gini coefficients at different spatial scales, to estimate the spatial correlation and the geographical variability of radon concentrations. This variability can be interpreted as a signature of the different subsurface geological conditions. The Gini coefficient computation is a statistical tool widely used to determine the degree of inhomogeneity of different kinds of distributions. We generated several simulated radon distributions, and the proposed tool has been validated by comparing the variograms based on the semi-variance computation with those ones based on the Gini coefficient. The Gini coefficient variogram is shown to be a good estimator of the inhomogeneity degree of radon concentration. Indeed, it allows to better constrain the critical distance below which the radon geological source can be considered as uniform at least for the investigated length scales of variability; it also better discriminates the fluctuations due to the environmental predisposing factors from those ones due to the random spatially uncorrelated noise.https://doi.org/10.2478/nuka-2020-0015geographical variabilitygeostatisticsgini coefficientlorenz curveradon concentrationvariogram |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Loffredo Filomena Scala Antonio Adinolfi Guido Maria Savino Federica Quarto Maria |
spellingShingle |
Loffredo Filomena Scala Antonio Adinolfi Guido Maria Savino Federica Quarto Maria A new geostatistical tool for the analysis of the geographical variability of the indoor radon activity Nukleonika geographical variability geostatistics gini coefficient lorenz curve radon concentration variogram |
author_facet |
Loffredo Filomena Scala Antonio Adinolfi Guido Maria Savino Federica Quarto Maria |
author_sort |
Loffredo Filomena |
title |
A new geostatistical tool for the analysis of the geographical variability of the indoor radon activity |
title_short |
A new geostatistical tool for the analysis of the geographical variability of the indoor radon activity |
title_full |
A new geostatistical tool for the analysis of the geographical variability of the indoor radon activity |
title_fullStr |
A new geostatistical tool for the analysis of the geographical variability of the indoor radon activity |
title_full_unstemmed |
A new geostatistical tool for the analysis of the geographical variability of the indoor radon activity |
title_sort |
new geostatistical tool for the analysis of the geographical variability of the indoor radon activity |
publisher |
Sciendo |
series |
Nukleonika |
issn |
0029-5922 |
publishDate |
2020-06-01 |
description |
The population is continuously exposed to a background level of ionizing radiation due to the natural radioactivity and, in particular, with radon (222Rn). Radon gas has been classified as the second leading cause of lung cancer after tobacco smoke [1]. In the confined environment, radon concentration can reach harmful level and vary accordingly to many factors. Since the primary source of radon in dwellings is the subsurface, the risk assessment and reduction cannot disregard the identification of the local geology and the environmental predisposing factors. In this article, we propose a new methodology, based on the computation of the Gini coefficients at different spatial scales, to estimate the spatial correlation and the geographical variability of radon concentrations. This variability can be interpreted as a signature of the different subsurface geological conditions. The Gini coefficient computation is a statistical tool widely used to determine the degree of inhomogeneity of different kinds of distributions. We generated several simulated radon distributions, and the proposed tool has been validated by comparing the variograms based on the semi-variance computation with those ones based on the Gini coefficient. The Gini coefficient variogram is shown to be a good estimator of the inhomogeneity degree of radon concentration. Indeed, it allows to better constrain the critical distance below which the radon geological source can be considered as uniform at least for the investigated length scales of variability; it also better discriminates the fluctuations due to the environmental predisposing factors from those ones due to the random spatially uncorrelated noise. |
topic |
geographical variability geostatistics gini coefficient lorenz curve radon concentration variogram |
url |
https://doi.org/10.2478/nuka-2020-0015 |
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