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首页> 外文期刊>Journal of Environmental Protection >An Indoor Radon Survey in Three Different Climate Regions in Mexico, and the Influence of Climate in the Obtained Values
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An Indoor Radon Survey in Three Different Climate Regions in Mexico, and the Influence of Climate in the Obtained Values

机译:墨西哥三个不同气候区域的室内Rad调查以及气候对获得值的影响

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摘要

In this paper we present the results of a survey of indoor radon concentration levels in Mexico. In order to investigate whether differences in climate translate into significant differences in indoor radon concentrations, the country was divided into three climate regions: the northern semi-desert region, the central semitropical region and the southern tropical region. The survey was carried out using nuclear track methodology. The dosimeters employed for the survey were based on the passive closed-end cup device, developed at the Physics Institute of the National Autonomous University of Mexico, and used PADC as detector material. A well-established protocol for chemically etching and reading the detectors was followed. Average annual temperatures differ between regions (from 15℃ to 28℃) but vary relatively little within each region. Atmospheric temperature is one of the most important factors which need to be considered when carrying out a survey of indoor radon concentrations because temperature largely determines building ventilation habits, and ventilation habits are known to have significant effects on indoor radon concentrations. Other factors, including building construction materials, architectural styles, geological and hydrological characteristics, and seismicity, vary from region to region and within each region. In each of the three regions low levels of indoor radon (from 37 to 179 Bq·m-3) were found.
机译:在本文中,我们介绍了墨西哥室内ra浓度水平调查的结果。为了调查气候差异是否转化为室内ra浓度的显着差异,该国被划分为三个气候区域:北部半沙漠地区,中亚热带地区和南部热带地区。这项调查是使用核轨道方法进行的。用于调查的剂量计基于墨西哥国立自治大学物理研究所开发的无源封闭杯装置,并使用PADC作为检测器材料。遵循了用于化学蚀刻和读取检测器的公认方案。不同地区之间的年平均气温有所不同(从15℃到28℃),但每个地区之间的平均变化相对较小。大气温度是进行室内ra浓度调查时需要考虑的最重要因素之一,因为温度在很大程度上决定了建筑物的通风习惯,并且已知通风习惯会对室内ra浓度产生重大影响。其他因素,包括建筑物的建筑材料,建筑风格,地质和水文特征以及地震活动性,在不同地区之间以及每个地区内都不同。在这三个区域的每一个中,室内ra水平较低(从37到179 Bq·m-3)。

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