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班加罗尔市及其周边地区氡及其子体的浓度。

Concentrations of radon and its daughter products in and around Bangalore city.

作者信息

Ningappa C, Sannappa J, Chandrashekara M S, Paramesh L

机构信息

Department of Physics, Vidya Vikas Institute of Engineering and Technology, Mysore 570010, India.

出版信息

Radiat Prot Dosimetry. 2008;130(4):459-65. doi: 10.1093/rpd/ncn091. Epub 2008 Apr 1.

Abstract

Indoor radon and its progeny levels were measured during 2005-06 in Bangalore rural district and in Bangalore City by using Solid State Nuclear Track Detector (SSNTD)-based twin cup dosemeters, and the activity of radium present in soils and rocks was measured by using HPGe detector. Fifty dwellings of different types were chosen for the measurement. The dosimeters containing the detector (LR-115 Type II Film) used in each house were fixed 2 m above the floor. After an exposure time of 90 days, films were etched to reveal tracks. From the track density, the concentrations of radon were evaluated. The value of radon concentration in the indoor air near granite quarries varies from 55 to 300 Bq.m(-3) with a median of 155 Bq.m(-3) and its progeny varies from 0.24 to 19.6 mWL with a median of 8.4 mWL. In Bangalore City, the concentration of radon varies from 18.4 to 110 Bq.m(-3) with a median of 45 Bq.m(-3) and its progeny varies from 1.62 to 11.24 mWL with a median of 4.15 mWL. Higher concentrations of radon and its progeny were observed in granite quarries compared with Bangalore City. The main reason for the higher indoor radon and its progeny concentration is due to the mining activity and the types of the bedrock. The concentration of radon mainly depends on the activity of radium present in soils and rocks and the types of building materials used. The activity of radium varies in granitic regions of Bangalore rural district from 42.0 to 163.6 Bq.kg(-1) with a median of 112.8 Bq.kg(-1). The concentrations of indoor radon and its daughter products and equivalent effective dose are discussed.

摘要

2005年至2006年期间,在班加罗尔农村地区和班加罗尔市,使用基于固体核径迹探测器(SSNTD)的双杯剂量计测量了室内氡及其子体水平,并使用高纯锗探测器测量了土壤和岩石中镭的活度。选择了50栋不同类型的住宅进行测量。每个房屋中使用的装有探测器(LR - 115 II型胶片)的剂量计固定在离地面2米高处。经过90天的暴露时间后,对胶片进行蚀刻以显示径迹。根据径迹密度评估氡的浓度。花岗岩采石场附近室内空气中氡的浓度在55至300 Bq·m⁻³之间变化,中位数为155 Bq·m⁻³,其子体浓度在0.24至19.6 mWL之间变化,中位数为8.4 mWL。在班加罗尔市,氡的浓度在18.4至110 Bq·m⁻³之间变化,中位数为45 Bq·m⁻³,其子体浓度在1.62至11.24 mWL之间变化,中位数为4.15 mWL。与班加罗尔市相比,花岗岩采石场中观察到更高浓度的氡及其子体。室内氡及其子体浓度较高的主要原因是采矿活动和基岩类型。氡的浓度主要取决于土壤和岩石中镭的活度以及所使用的建筑材料类型。班加罗尔农村地区花岗岩区域中镭的活度在42.0至163.6 Bq·kg⁻¹之间变化,中位数为112.8 Bq·kg⁻¹。文中讨论了室内氡及其子产物的浓度以及等效有效剂量。

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