Gascó C, Antón M P, Pozuelo M, Clemente L, Rodríguez A, Yañez C, González A, Meral J
Centro de Investigaciones Energéticas, Medioambientales y Tecnológicas, CIEMAT, Departamento de Medio Ambiente, Avda. Complutense 22, Madrid 28040, Spain.
J Environ Radioact. 2006;89(2):159-71. doi: 10.1016/j.jenvrad.2006.05.004. Epub 2006 Jun 27.
Within an extensive multinational and multidisciplinary project carried out in Doñana National Park (Spain) to investigate its preservation and regeneration, the filling velocity of the salt marshes has been evaluated through the calculation of their average sediment accumulation rates. (239+240)Pu and (137)Cs from weapons testing fallout and total (210)Pb distribution profiles and inventories have been determined in some of the most characteristic zones of the park, namely, the ponds (or "lucios") and the waterjets (or "caños"). Plutonium inventories range from 16 to 101 Bq m(-2), (137)Cs values fluctuate between 514 and 3,758 Bq m(-2) and unsupported (210)Pb values comprise between 124 and 9398 Bq m(-2). Average sedimentation rates range from 3 to 5 mm y(-1) (1952-2002). These data are higher than those obtained by carbon dating for the period 6,500 AD-present, estimated as 1.5-2 mm y(-1), suggesting an increase in the accumulation of sediments and the alteration of the park's hydrodynamics caused by the re-channeling of the major rivers feeding the salt marshes.
在西班牙多尼亚纳国家公园开展的一项广泛的跨国多学科项目中,为了研究其保护和恢复情况,通过计算盐沼的平均沉积物积累速率来评估其填充速度。在该公园一些最具代表性的区域,即池塘(或“lucios”)和喷水口(或“caños”),测定了武器试验沉降物中的钚-239和钚-240、铯-137以及总铅-210的分布剖面和存量。钚存量范围为16至101贝克勒尔每平方米,铯-137值在514至3758贝克勒尔每平方米之间波动,非支持性铅-210值在124至9398贝克勒尔每平方米之间。平均沉积速率范围为3至5毫米每年(1952 - 2002年)。这些数据高于通过碳年代测定法获得的公元6500年至今期间的数据,后者估计为1.5至2毫米每年,这表明沉积物积累增加,以及为盐沼供水的主要河流改道导致公园水动力发生改变。