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亚历山大市室内氡水平与土壤氡析出率的对比研究。

A comparative study of the indoor radon level with the radon exhalation rate from soil in Alexandria city.

作者信息

Abd El-Zaher Mohamed

机构信息

Department of Basic and Applied Science, Faculty of Engineering, Arab Academy for Science & Technology, Alexandria, Egypt.

出版信息

Radiat Prot Dosimetry. 2013 May;154(4):490-6. doi: 10.1093/rpd/ncs267. Epub 2012 Oct 15.

Abstract

The assessment of the radiological risk related to the inhalation of radon and radon its progeny is based mainly on the integrated measurement of radon in both indoor and outdoor environments. The exhalation of radon from the earth's crust and building materials forms the main source of radon in the indoor environment. This study has been undertaken for the purpose of health risk assessment. In this comparative study, the indoor radon level, radium content, radon exhalation rate and concentration of soil radon are measured using the Can Technique. Soil samples were collected simultaneously from different geological formations of the same area for laboratory measurement of the radon exhalation rate. The radon exhalation rate was measured in the laboratory using LR-115 type II plastic track detectors. The indoor radon concentrations in this study area were found to vary from 44±9 to 132±31 Bq m(-3) with an average of 72±29 Bq m(-3). The seasonal variations of the indoor radon reveal the maximum values in the winter and in summer in different dwellings of Alexandria city. The annual effective dose varies from 0.75 to 2.2 mSv with an average value of 1.34 mSv. The radon exhalation rate was found to vary in the ranges 8.31-233.70×10(-3) Bq kg(-1) h(-1), 0.48-15.37 Bq m(-2) h(-1) with an average 47.97×10(-3) Bq kg(-1) h(-1), (3.14 Bq m(-2) h(-1)). The radium content in soil varies from 3.14 to 39.60 Bq kg(-1) with an average of 11.55 Bq kg(-1). The significance of this study is discussed in details from the point of view of radiation protection.

摘要

对与吸入氡及其子体相关的放射风险评估主要基于室内和室外环境中氡的综合测量。地壳和建筑材料中氡的析出是室内环境中氡的主要来源。本研究旨在进行健康风险评估。在这项对比研究中,使用罐技术测量室内氡水平、镭含量、氡析出率和土壤氡浓度。从同一地区不同地质构造同时采集土壤样本,用于实验室测量氡析出率。在实验室中使用LR - 115 II型塑料径迹探测器测量氡析出率。本研究区域内的室内氡浓度在44±9至132±31 Bq m(-3)之间变化,平均为72±29 Bq m(-3)。室内氡的季节变化显示,在亚历山大市不同住宅中,冬季和夏季出现最大值。年有效剂量在0.75至2.2 mSv之间变化,平均值为1.34 mSv。发现氡析出率在8.31 - 233.70×10(-3) Bq kg(-1) h(-1)、0.48 - 15.37 Bq m(-2) h(-1)范围内变化,平均为47.97×10(-3) Bq kg(-1) h(-1),(3.14 Bq m(-2) h(-1))。土壤中的镭含量在3.14至39.60 Bq kg(-1)之间变化,平均为11.55 Bq kg(-1)。从辐射防护的角度详细讨论了本研究的意义。

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