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Monitoring Strategies at Phreatic Wellfields: A 3D Travel Time Approach

机译:潜水井场的监控策略:3D行程时间方法

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摘要

Ground water quality networks for monitoring phreatic drinking water wellfields are generally established for two main purposes: (1) the short-term safeguarding of public water supply and (2) signaling and predicting future quality changes in the extracted ground water. Six monitoring configurations with different well locations and different screen depths and lengths were evaluated using a numerical model of the 3D ground water flow toward a partially penetrating pumping well in a phreatic aquifer. Travel times and breakthrough curves for observation and pumping wells were used to judge the effectiveness of different design configurations for three monitoring objectives: (1) early warning; (2) prediction of future quality changes; and (3) evaluation of protection measures inside a protection zone. Effectiveness was tested for scenarios with advective transport, first-order degradation, and linear sorption. It is shown that the location and especially the depth of the observation wells should be carefully chosen, taking into account the residence time from the surface to the observation well, the residual transit times to the extraction well, and the transformation and retardation rates. Shallow monitoring was most functional for a variety of objectives and conditions. The larger the degradation rates or retardation, the shallower should the monitoring be for effective early warning and prediction of future ground water quality. The general approach followed in the current study is applicable for many geohydrological situations, tuning specific monitoring objectives with residence times and residual transit times obtained from a site-specific ground water flow model.
机译:通常建立用于监测潜水饮用水井场的地下水质量网络主要有两个目的:(1)短期维护公共供水;(2)发出信号并预测提取的地下水的未来质量变化。使用3D地下水流向潜水含水层中部分穿透的抽水井的数值模型,对具有不同井位,不同筛网深度和长度的六种监测配置进行了评估。观察和抽水井的行进时间和穿透曲线用于判断三个监测目标的不同设计配置的有效性:(1)预警; (2)预测未来质量变化; (3)评价保护区内的保护措施。测试了对流运输,一级降解和线性吸附的情景的有效性。结果表明,应该仔细选择观察井的位置,特别是深度,要考虑到从地面到观察井的停留时间,到萃取井的残留迁移时间以及转化率和滞后率。浅层监视对于各种目标和条件最有效。退化率或滞后性越大,对有效的预警和对未来地下水水质预测的监测范围就越浅。当前研究中采用的一般方法适用于许多地质水文情况,可以通过从特定地点的地下水流模型中获得的停留时间和剩余通过时间来调整特定的监测目标。

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