Segovia N, Gaso M I, Armienta M A
Instituto de Geofisica, UNAM, Ciudad Universitaria, Circuito Exterior, C.U., Mexico, DF, 04510, Mexico.
Environ Geochem Health. 2007 Apr;29(2):143-53. doi: 10.1007/s10653-006-9069-6.
Radon has been determined in soil, groundwater, and air in Mexico, both indoors and outdoors, as part of geophysical studies and to estimate effective doses as a result of radon exposure. Detection of radon has mainly been performed with solid-state nuclear track detectors (SSNTD) and, occasionally, with active detection devices based on silicon detectors or ionization chambers. The liquid scintillation technique, also, has been used for determination of radon in groundwater. The adjusted geometric mean indoor radon concentration (74 Bq m-3) in urban developments, for example Mexico City, is higher than the worldwide median concentration of radon in dwellings. In some regions, particularly hilly regions of Mexico where air pollution is high, radon concentrations are higher than action levels and the effective dose for the general population has increased. Higher soil radon levels have been found in the uranium mining areas in the northern part of the country. Groundwater radon levels are, in general, low. Soil-air radon contributing to indoor atmospheres and air pollution is the main source of increased exposure of the population.
作为地球物理研究的一部分,并为了估算氡暴露导致的有效剂量,墨西哥对室内和室外的土壤、地下水及空气中的氡进行了测定。氡的检测主要使用固态核径迹探测器(SSNTD),偶尔也使用基于硅探测器或电离室的主动探测设备。液体闪烁技术也已用于测定地下水中的氡。例如在墨西哥城等城市开发区,经调整后的室内氡浓度几何平均值(74 Bq m-3)高于全球住宅氡浓度中位数。在一些地区,特别是墨西哥空气污染严重的山区,氡浓度高于行动水平,普通人群的有效剂量增加。在该国北部的铀矿区发现了较高的土壤氡水平。总体而言,地下水中的氡水平较低。导致室内大气和空气污染的土壤-空气氡是公众暴露增加的主要来源。