Centro de Investigación, Tecnología e Innovación, Universidad de Sevilla CITIUS, Av. Reina Mercedes 4B, E41012-Sevilla, Spain.
Sci Total Environ. 2009 Dec 15;408(1):69-77. doi: 10.1016/j.scitotenv.2009.09.028. Epub 2009 Oct 12.
The Huelva Estuary in Huelva, Spain, has been one of the most studied environmental compartments in the past years from the point of view of naturally occurring radioactive material (NORM) releases. It has been historically affected by waste releases, enriched in radionuclides from the U-decay series, from factories located in the area devoted to the production of phosphoric acid and phosphate fertilizers. Nevertheless, changes in national regulations forced a new waste management practice in 1998, prohibiting releases of phosphogypsum into the rivers. The input of natural radionuclides from phosphate factories to rivers was drastically reduced. Because of this there was a unique opportunity for the study of the response of a contaminated environmental compartment, specifically an estuary affected by tidal influences, after the cessation of the contaminant releases to, in this case, the Huelva Estuary (henceforth referred to as the Estuary). To investigate the environmental response to this new discharge regime, the specific activities of radionuclides 226Ra and 210Pb in water and sediment samples collected in four campaigns (from 1999 to 2005) were determined and compared with pre-1998 values. From this study it is possible to infer the most effective mechanisms of decontamination for the Estuary. Decontamination rates of 210Pb and 226Ra in the sediments and water have been calculated using exponential fittings and corresponding half-lives have been deduced from them. The cleaning half-life in the whole area of the Estuary is about 6 and 3.5 years for 226Ra and 210Pb respectively. The observed trend clearly shows that contamination of the Estuary by natural radionuclides is now decreasing and radioactive levels in waters and sediments are approaching the natural background references. This work attempts to evaluate whether it can be expected that the decontamination of the enhanced levels of natural radioactivity in the Estuary can be performed via natural processes.
西班牙韦尔瓦河口(Huelva Estuary in Huelva)多年来一直是从天然放射性物质(NORM)释放的角度研究环境的最热门领域之一。该地区历史上曾受到放射性核素释放的影响,这些放射性核素来自该地区生产磷酸和磷酸盐肥料的工厂。然而,国家法规的变化迫使 1998 年实施了新的废物管理实践,禁止将磷石膏排放到河流中。从磷酸盐工厂输入到河流中的天然放射性核素数量大大减少。正因为如此,在河流中停止排放污染物后,为研究受污染环境的响应提供了一个独特的机会,特别是在潮汐影响下的河口,就像本案例中的韦尔瓦河口(下文简称河口)。为了研究这种新的排放制度对环境的响应,对在四个时期(1999 年至 2005 年)收集的水和沉积物样本中的放射性核素 226Ra 和 210Pb 的比活度进行了测定,并与 1998 年之前的数据进行了比较。通过这项研究,可以推断出河口最有效的净化机制。利用指数拟合计算了沉积物和水中 210Pb 和 226Ra 的净化率,并由此推断出它们的半衰期。整个河口地区的净化半衰期分别约为 6 年和 3.5 年,对应于 226Ra 和 210Pb。观察到的趋势清楚地表明,河口受天然放射性核素的污染正在减少,水和沉积物中的放射性水平正在接近天然背景参考值。本研究试图评估是否可以预期通过自然过程来消除河口天然放射性增强的水平。