Mahler Barbara, Massei Nicolas
U.S. Geological Survey, 8027 Exchange Dr., Austin, TX 78754, United States.
J Contam Hydrol. 2007 Apr 1;91(1-2):81-106. doi: 10.1016/j.jconhyd.2006.08.010. Epub 2006 Dec 11.
Karst aquifers are uniquely vulnerable to contamination. In the Barton Springs segment of the karstic Edwards aquifer (Texas, U.S.A.), urban contaminants such as pesticides and volatile organic compounds frequently are detected in spring base flow. To determine whether contaminant concentrations change in response to storms, and if they therefore might act as tracers of focused recharge, samples were collected from Barton Springs at closely spaced intervals following three storms. Two herbicides (atrazine and simazine), two insecticides (carbaryl and diazinon), and a solvent (tetrachloroethene) described breakthrough curves over a 1-week period following one or more storms. The breakthrough curves were decomposed into two to five log-normal subcurves, which were interpreted as representing pulses of contaminants moving through the aquifer. Each subcurve could be used in the same way as an artificial tracer to determine travel time to and recovery at the spring. The contaminants have several advantages over artificial tracers: they represent the actual compounds of interest, they are injected essentially simultaneously at several points, and they are injected under those conditions when transport is of the most interest, i.e., following storms. The response of storm discharge, specific conductance, and contaminant loading at the spring depended on initial aquifer flow conditions, which varied from very low (spring discharge of 0.48 m3/s) to high (spring discharge of 2.7 m3/s): concentrations and recovery were the highest when initial aquifer flow conditions were low. This behavior provides information about aquifer structure and the influence of aquifer flow condition on transport properties.
岩溶含水层极易受到污染。在美国得克萨斯州岩溶爱德华兹含水层的巴顿泉段,泉基流中经常检测到农药和挥发性有机化合物等城市污染物。为了确定污染物浓度是否会因暴雨而变化,以及它们是否因此可作为集中补给的示踪剂,在三场暴雨后,以紧密间隔从巴顿泉采集了样本。一种除草剂(莠去津和西玛津)、两种杀虫剂(西维因和二嗪农)以及一种溶剂(四氯乙烯)描述了一场或多场暴雨后1周内的穿透曲线。穿透曲线被分解为两到五条对数正态子曲线,这些子曲线被解释为代表污染物在含水层中移动的脉冲。每条子曲线都可以像人工示踪剂一样用于确定到达泉水的时间和在泉水中的回收率。与人工示踪剂相比,这些污染物有几个优点:它们代表了实际感兴趣的化合物,它们基本上在几个点同时注入,并且它们是在最关注运移的条件下注入的,即暴雨之后。泉水处的暴雨流量、电导率和污染物负荷的响应取决于初始含水层流动条件,初始含水层流动条件从非常低(泉水流量为0.48立方米/秒)到高(泉水流量为2.7立方米/秒)不等:当初始含水层流动条件较低时,浓度和回收率最高。这种行为提供了有关含水层结构以及含水层流动条件对运移特性影响的信息。