Soil gas radon mapping of Muzaffarabad city, Pakistan

Soil-based radon investigations are of value in correlating radon production and its transportation into buildings through the processes of convection and diffusion. Such studies can help in identifying land areas that pose special concerns. We present preliminary results of soil radon gas...

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Main Authors: Tareen Aleem Dad Khan, Rafique Muhammad, Kearfot Kimberlee J.T., Basharat Muhammad, Shafique Bilal
Format: Article
Language:English
Published: VINCA Institute of Nuclear Sciences 2016-01-01
Series:Nuclear Technology and Radiation Protection
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/1451-3994/2016/1451-39941603291T.pdf
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spelling doaj-792642a209d74963a2e0c376c17fbac42020-11-24T23:38:30ZengVINCA Institute of Nuclear SciencesNuclear Technology and Radiation Protection1451-39941452-81852016-01-0131329129810.2298/NTRP1603291T1451-39941603291TSoil gas radon mapping of Muzaffarabad city, PakistanTareen Aleem Dad Khan0Rafique Muhammad1Kearfot Kimberlee J.T.2Basharat Muhammad3Shafique Bilal4The University of Azad Jammu & Kashmir, Muzaffarbad, Department of Physics, Azad Kashmir, PakistanThe University of Azad Jammu & Kashmir, Muzaffarbad, Department of Physics, Azad Kashmir, PakistanUniversity of Michigan, Department of Nuclear Engineering and Radiological Sciences, Ann Arbor, Mich., USAThe University of Azad Jammu & Kashmir, Institute of Geology, Muzaffarabad, Azad Kashmir, PakistanThe University of Azad Jammu & Kashmir, Muzaffarbad, Department of Physics, Azad Kashmir, PakistanSoil-based radon investigations are of value in correlating radon production and its transportation into buildings through the processes of convection and diffusion. Such studies can help in identifying land areas that pose special concerns. We present preliminary results of soil radon gas measurements at 60 different locations in an attempt to map out the geohazard zone of the city of Muzaffarabad. The seismic geohazard microzonation for the area includes five microzones based on different hazard parameters: a very high hazard zone, a high hazard zone, a moderate hazard zone, a low hazard zone, and a safe zone. Measurements were taken with an active radon monitoring system at the depths of 30, 40, 50, and 60 cm below the ground surface. The results obtained were explained by the lithology of the area. Average soil radon gas concentrations were correlated with the depth from the ground surface and indoor radon values for the study area. No significant correlation was found between soil radon gas and meteorological parameters, however soil radon gas increases as the depth from the surface of the ground grows. The results showed a linear relation between soil radon concentrations with depth from ground surface (R2 = 0.9577). The minimum soil radon concentration (68.5 Bq/m3) was found at a depth of 30 cm in the very high hazard zone, the maximum value (53.300 Bq/m3) at a depth of 60 cm in the seismically safe zone. Measured soil gas radon concentrations at depths of 30, 40, 50, and 60 cm were mapped for high, moderate, and low radon concentrations. Elevated soil radon gas concentrations were found in the safe zone, otherwise considered to be suitable for any type of construction.http://www.doiserbia.nb.rs/img/doi/1451-3994/2016/1451-39941603291T.pdfradonsoil gasgeohazard zonelithologymeteorological parameter
collection DOAJ
language English
format Article
sources DOAJ
author Tareen Aleem Dad Khan
Rafique Muhammad
Kearfot Kimberlee J.T.
Basharat Muhammad
Shafique Bilal
spellingShingle Tareen Aleem Dad Khan
Rafique Muhammad
Kearfot Kimberlee J.T.
Basharat Muhammad
Shafique Bilal
Soil gas radon mapping of Muzaffarabad city, Pakistan
Nuclear Technology and Radiation Protection
radon
soil gas
geohazard zone
lithology
meteorological parameter
author_facet Tareen Aleem Dad Khan
Rafique Muhammad
Kearfot Kimberlee J.T.
Basharat Muhammad
Shafique Bilal
author_sort Tareen Aleem Dad Khan
title Soil gas radon mapping of Muzaffarabad city, Pakistan
title_short Soil gas radon mapping of Muzaffarabad city, Pakistan
title_full Soil gas radon mapping of Muzaffarabad city, Pakistan
title_fullStr Soil gas radon mapping of Muzaffarabad city, Pakistan
title_full_unstemmed Soil gas radon mapping of Muzaffarabad city, Pakistan
title_sort soil gas radon mapping of muzaffarabad city, pakistan
publisher VINCA Institute of Nuclear Sciences
series Nuclear Technology and Radiation Protection
issn 1451-3994
1452-8185
publishDate 2016-01-01
description Soil-based radon investigations are of value in correlating radon production and its transportation into buildings through the processes of convection and diffusion. Such studies can help in identifying land areas that pose special concerns. We present preliminary results of soil radon gas measurements at 60 different locations in an attempt to map out the geohazard zone of the city of Muzaffarabad. The seismic geohazard microzonation for the area includes five microzones based on different hazard parameters: a very high hazard zone, a high hazard zone, a moderate hazard zone, a low hazard zone, and a safe zone. Measurements were taken with an active radon monitoring system at the depths of 30, 40, 50, and 60 cm below the ground surface. The results obtained were explained by the lithology of the area. Average soil radon gas concentrations were correlated with the depth from the ground surface and indoor radon values for the study area. No significant correlation was found between soil radon gas and meteorological parameters, however soil radon gas increases as the depth from the surface of the ground grows. The results showed a linear relation between soil radon concentrations with depth from ground surface (R2 = 0.9577). The minimum soil radon concentration (68.5 Bq/m3) was found at a depth of 30 cm in the very high hazard zone, the maximum value (53.300 Bq/m3) at a depth of 60 cm in the seismically safe zone. Measured soil gas radon concentrations at depths of 30, 40, 50, and 60 cm were mapped for high, moderate, and low radon concentrations. Elevated soil radon gas concentrations were found in the safe zone, otherwise considered to be suitable for any type of construction.
topic radon
soil gas
geohazard zone
lithology
meteorological parameter
url http://www.doiserbia.nb.rs/img/doi/1451-3994/2016/1451-39941603291T.pdf
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