Puckett Larry J, Hughes W Brian
US Geological Survey, Reston, VA 20192, USA.
J Environ Qual. 2005 Nov 7;34(6):2278-92. doi: 10.2134/jeq2005.0109. Print 2005 Nov-Dec.
There is continuing concern over potential impacts of widespread application of nutrients and pesticides on ground- and surface-water quality. Transport and fate of nitrate and pesticides were investigated in a shallow aquifer and adjacent stream, Cow Castle Creek, in Orangeburg County, South Carolina. Pesticide and pesticide degradate concentrations were detected in ground water with greatest frequency and largest concentrations directly beneath and downgradient from the corn (Zea mays L.) field where they were applied. In almost all samples in which they were detected, concentrations of pesticide degradates greatly exceeded those of parent compounds, and were still present in ground waters that were recharged during the previous 18 yr. The absence of both parent and degradate compounds in samples collected from deeper in the aquifer suggests that this persistence is limited or that the ground water had recharged before use of the pesticide. Concentrations of NO(-)(3) in ground water decreased with increasing depth and age, but denitrification was not a dominant controlling factor. Hydrologic and chemical data indicated that ground water discharges to the creek and chemical exchange takes place within the upper 0.7 m of the streambed. Ground water had its greatest influence on surface-water chemistry during low-flow periods, causing a decrease in concentrations of Cl(-), NO(-)(3), pesticides, and pesticide degradates. Conversely, shallow subsurface drainage dominates stream chemistry during high-flow periods, increasing stream concentrations of Cl(-), NO(-)(3), pesticides, and pesticide degradates. These results point out the importance of understanding the hydrogeologic setting when investigating transport and fate of contaminants in ground water and surface water.
营养物质和农药的广泛应用对地下水和地表水水质的潜在影响一直备受关注。在南卡罗来纳州奥兰治堡县的一个浅层含水层及相邻的考城堡溪中,对硝酸盐和农药的迁移及归宿进行了研究。在施用农药的玉米(Zea mays L.)田地下方及其下游的地下水中,农药和农药降解产物的浓度检测频率最高且浓度最大。在几乎所有检测到它们的样品中,农药降解产物的浓度大大超过母体化合物的浓度,并且在前18年补给的地下水中仍然存在。从含水层较深处采集的样品中既没有母体化合物也没有降解产物,这表明这种持久性是有限的,或者是在使用农药之前地下水就已经得到了补给。地下水中NO(-)(3)的浓度随深度和年龄的增加而降低,但反硝化作用不是主要的控制因素。水文和化学数据表明,地下水排入溪流,并且在河床上部0.7米范围内发生化学交换。在低流量时期,地下水对地表水化学性质的影响最大,导致Cl(-)、NO(-)(3)、农药和农药降解产物的浓度降低。相反,在高流量时期,浅层地下排水主导着溪流化学性质,增加了溪流中Cl(-)、NO(-)(3)、农药和农药降解产物的浓度。这些结果指出了在研究地下水和地表水中污染物的迁移及归宿时了解水文地质环境的重要性。