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中尺度气象学在调节西班牙韦尔瓦(Huelva)地区(222)Rn 浓度中的作用——磷石膏堆的影响。

The role of mesoscale meteorology in modulating the (222)Rn concentrations in Huelva (Spain)--impact of phosphogypsum piles.

机构信息

European Commission, Joint Research Centre (JRC), Institute for Transuranium Elements (ITU), Ispra, VA, Italy.

Institute of Energy Technologies (INTE), Technical University of Catalonia, Barcelona, Spain.

出版信息

J Environ Radioact. 2015 Jul;145:1-9. doi: 10.1016/j.jenvrad.2015.03.023. Epub 2015 Apr 5.

Abstract

The combined analysis of (222)Rn activity concentrations and mesoscale meteorological conditions at Huelva city (Spain) was addressed in this study to understand the potential impact of phosphogypsum piles on the (222)Rn activity concentrations registered at this area. Hourly mean data from April 2012 to February 2013 registered at two sampling sites (Huelva city and in the background station of El Arenosillo, located 27 km to the south-east) have been used in the study. The results of the present study showed a large difference in mean radon concentrations between the two stations during the sampling period, 6.3 ± 0.4 Bq m(-3) at Huelva and 3.0 ± 0.2 Bq m(-3) at El Arenosillo. The analysis has demonstrated that hourly (222)Rn concentrations at Huelva city above 22 Bq m(-3), with nocturnal peaks up to 50 Bq/m(3), mainly coincided with the occurrence of a pure sea-land breeze cycle. Mesoscale circulations in this region are mainly characterized by two patterns of sea-land breeze, pure and non-pure, with the phosphosypsum piles directly upstream (south) of the city during the afternoon on pure sea-breeze days. The difference between mean (222)Rn activity concentrations at Huelva city were 9.9 ± 1.5 Bq m(-3) for the pure pattern and 3.3 ± 0.5 Bq m(-3) for the non-pure pattern, while in the background station concentrations were 3.9 ± 0.4 Bq m(-3) and 2.8 ± 0.4 Bq m(-3) respectively. Considering these large differences, a detailed analysis of composites and case studies of representative sea-land breeze cycles of both types and their impact on (222)Rn activity concentration was performed. The results suggested that the presence of the phosphogypsum piles was necessary in order to justify the high (222)Rn activity concentrations observed at Huelva compared with the background station in the afternoons on pure sea breeze days (1.5-2.0 Bq m(-3)). On the other hand, large night time differences between the two sites on these days were likely to be associated with a combination of shallow density currents travelling down the Guadalquivir valley and, again, the presence of phosphogypsum piles. The results have demonstrated a significant impact of the phosphogypsum piles on (222)Rn activity concentrations in Huelva city during the occurrence of pure sea breeze days.

摘要

本研究旨在分析乌韦亚市(西班牙)的(222)Rn 活度浓度与中尺度气象条件的综合情况,以了解磷石膏堆对该地区(222)Rn 活度浓度的潜在影响。本研究使用了 2012 年 4 月至 2013 年 2 月期间在两个采样点(乌韦亚市和位于东南 27 公里处的埃尔阿雷内罗背景站)采集的每小时平均值数据。本研究结果表明,在采样期间,两个站点之间的氡浓度均值差异较大,乌韦亚市为 6.3±0.4 Bq m-3,埃尔阿雷内罗为 3.0±0.2 Bq m-3。分析表明,乌韦亚市的(222)Rn 浓度在 22 Bq m-3 以上,夜间峰值高达 50 Bq/m3,主要与纯海陆风循环的发生有关。该地区的中尺度环流主要以纯海陆风和非纯海陆风两种模式为特征,在下午纯海风天气期间,磷石膏堆直接位于城市的上游(南部)。在纯风模式下,乌韦亚市的平均(222)Rn 活度浓度差值为 9.9±1.5 Bq m-3,非纯风模式下为 3.3±0.5 Bq m-3,而在背景站浓度分别为 3.9±0.4 Bq m-3 和 2.8±0.4 Bq m-3。考虑到这些较大的差异,对两种类型具有代表性的海陆风循环的综合分析和案例研究及其对(222)Rn 活度浓度的影响进行了分析。结果表明,在下午纯海风天气期间,与背景站相比,磷石膏堆的存在是解释乌韦亚市(222)Rn 活度浓度较高的必要条件(1.5-2.0 Bq m-3)。另一方面,这些天两个站点之间夜间的差异较大,可能与沿瓜达尔基维尔山谷下行的浅层密度流以及磷石膏堆的存在有关。研究结果表明,在纯海风天气发生期间,磷石膏堆对乌韦亚市(222)Rn 活度浓度有显著影响。

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