Dueñas C, Liger E, Cañete S, Pérez M, Bolívar J P
Department of Applied Physics I, University of Málaga, Campus de Teatinos, 29071 Málaga, Spain.
J Environ Radioact. 2007;95(2-3):63-74. doi: 10.1016/j.jenvrad.2007.01.012. Epub 2007 Mar 26.
Phosphogypsum (PG) is a waste product of the phosphoric acid production process and contains, generally, high activity concentrations of uranium series radionuclides. It is stored in piles formed over the last 40 years close to the town of Huelva (Southwest of Spain). The very broad expanse of the PG piles (about 1200 ha) produces a local, but unambiguous, radioactive impact to their surroundings. In 1992, the regional government of Andalusia restored an area of 400 ha by covering it with a 25-cm thick layer of natural soil and, currently, there is an additional zone of 400 ha in course of restoration (unrestored) and the same area of active PG stacks. Due to the high activity concentration of (226)Ra in active PG stacks (average 647 Bq kg(-1)), a significant exhalation of (222)Rn could be produced from the surface of the piles. Measurements have been made of (222)Rn exhalation from active PG stacks and from restored and unrestored zones. The (222)Rn exhalation from unrestored zones is half of that of the active PG stacks. Following restoration, the (222)Rn exhalation is approximately eight times lower than the active PG stacks. The activity concentrations of natural radionuclides ((226)Ra, (40)K, (232)Th) in the mentioned zones have been determined. This study was also conducted to determine the effect of (226)Ra activity concentration on the (222)Rn exhalation, and a good correlation was obtained between the (222)Rn exhalation and (226)Ra activity, porosity and density of soil.
磷石膏(PG)是磷酸生产过程中的一种废弃物,通常含有高活性浓度的铀系放射性核素。它被储存在过去40年里在韦尔瓦镇(西班牙西南部)附近形成的堆中。磷石膏堆的面积非常广阔(约1200公顷),对其周围环境产生了局部但明显的放射性影响。1992年,安达卢西亚自治区政府通过在400公顷的区域覆盖一层25厘米厚的天然土壤进行了修复,目前,还有一个400公顷的区域正在进行修复(未修复),以及相同面积的正在使用的磷石膏堆。由于正在使用的磷石膏堆中镭 - 226的活性浓度很高(平均647贝克勒尔/千克),堆表面可能会产生大量的氡 - 222析出。已经对正在使用的磷石膏堆以及已修复和未修复区域的氡 - 222析出情况进行了测量。未修复区域的氡 - 222析出量是正在使用的磷石膏堆的一半。修复后,氡 - 222析出量比正在使用的磷石膏堆低约八倍。已测定了上述区域中天然放射性核素(镭 - 226、钾 - 40、钍 - 232)的活性浓度。本研究还旨在确定镭 - 226活性浓度对氡 - 222析出的影响,并且在氡 - 222析出与镭 - 226活性、土壤孔隙率和密度之间获得了良好的相关性。