Sidle W C, Shanklin D, Lee P Y, Roose D L
United States Environmental Protection Agency, Isotope Hydrology Laboratory, 5995 Center Hill Ave., Cincinnati, OH 45224, USA.
J Environ Radioact. 2001;55(1):29-46. doi: 10.1016/s0265-931x(00)00183-1.
Background radioactivity is elevated in many agricultural drainage ponds and also constructed wetland ponds in the Kankakee watershed. During 1995-1999, gross-alpha and -beta activities were measured up to 455 and 1650 mBq L-1, respectively. 226Ra and 228Ra averaged 139 and 192 mBq L-1 in controlled drainage ponds compared to 53 and 58 mBq L-1 for 226Ra and 228Ra, respectively, in native wetland ponds. Analyses of applied ammonium phosphate fertilizers near both native and controlled ponds indicate comparable 226Ra/228Ra and 228Ra/232Th activity ratios with only the surface waters in the controlled ponds. For example, 226Ra/228Ra activity ratios in controlled ponds ranged from 0.791 to 0.91 and group with a local fertilizer batch containing FL phosphate compounds with 226Ra/228Ra activity ratios of 0.831-1.04. Local soils of the Kankakee watershed have 226Ra/228Ra activity ratios of 0.541-0.70. Calculated Ra fluxes of waters, in drainage ditches associated with these controlled ponds, for 226Ra ranged from 0.77 to 9.00 mBq cm-2 d-1 and for 228Ra ranged from 1.22 to 8.43 mBq cm-2 d-1. Ra activity gradients were measured beneath these controlled ponds both in agricultural landscapes and in constructed wetlands, all being associated with drainage ditches. Ra had infiltrated to the local water table but was below regulatory maximum contaminant limits. Still, measurable Ra activity was measured downgradient of even the constructed wetlands in the Kankakee watershed, suggesting that the attenuation of Ra was low. However, no Ra excess was observed in the riparian zone or the Kankakee River downgradient of the native wetland ponds.
许多农业排水池塘以及坎卡基河流域的人工湿地池塘的本底放射性均有所升高。在1995年至1999年期间,总α和总β活度分别测得高达455和1650毫贝克勒尔每升。在受控排水池塘中,226镭和228镭的平均活度分别为139和192毫贝克勒尔每升,而在天然湿地池塘中,226镭和228镭的平均活度分别为53和58毫贝克勒尔每升。对天然池塘和受控池塘附近施用的磷酸铵肥料进行分析表明,只有受控池塘的地表水具有可比的226镭/228镭和228镭/232钍活度比。例如,受控池塘中的226镭/228镭活度比范围为0.791至0.91,与含有佛罗里达磷酸盐化合物的当地肥料批次归为一组,其226镭/228镭活度比为0.831至1.04。坎卡基河流域的当地土壤的226镭/228镭活度比为0.541至0.70。与这些受控池塘相关的排水渠中水体的镭通量计算值,226镭范围为0.77至9.00毫贝克勒尔每平方厘米每天,228镭范围为1.22至8.43毫贝克勒尔每平方厘米每天。在农业景观和人工湿地中的这些受控池塘下方均测量到了镭活度梯度,所有这些都与排水渠相关。镭已渗入当地地下水位,但低于监管的最大污染物限值。尽管如此,在坎卡基河流域即使是人工湿地的下游仍测量到了可测量的镭活度,这表明镭的衰减程度较低。然而,在天然湿地池塘下游的河岸带或坎卡基河中未观察到镭超标现象。