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Analyzing the effects of geological and parameter uncertainty on prediction of groundwater head and travel time

机译:分析地质和参数不确定性对预测地下水位和移动时间的影响

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Uncertainty of groundwater model predictions has in the past mostly beenrelated to uncertainty in the hydraulic parameters, whereas uncertainty inthe geological structure has not been considered to the same extent. Recentdevelopments in theoretical methods for quantifying geological uncertaintyhave made it possible to consider this factor in groundwater modeling. Inthis study we have applied the multiple-point geostatistical method (MPS)integrated in the Stanford Geostatistical Modeling Software (SGeMS) forexploring the impact of geological uncertainty on groundwater flow patternsfor a site in Denmark. Realizations from the geostatistical model were usedas input to a groundwater model developed from Modular three-dimensionalfinite-difference ground-water model (MODFLOW) within the Groundwater Modeling System(GMS) modeling environment. The uncertainty analysis was carried out in threescenarios involving simulation of groundwater head distribution and traveltime. The first scenario implied 100 stochastic geological models allassigning the same hydraulic parameters for the same geological units. Inthe second scenario the same 100 geological models were subjected to modeloptimization, where the hydraulic parameters for each of them were estimatedby calibration against observations of hydraulic head and stream discharge.In the third scenario each geological model was run with 216 randomized setsof parameters. The analysis documented that the uncertainty on theconceptual geological model was as significant as the uncertainty related tothe embedded hydraulic parameters.
机译:过去,地下水模型预测的不确定性主要与水力参数的不确定性有关,而地质结构的不确定性却没有得到同等程度的考虑。量化地质不确定性的理论方法的最新发展使得在地下水建模中考虑这一因素成为可能。在这项研究中,我们应用了集成在斯坦福地统计学模型软件(SGeMS)中的多点地统计学方法(MPS)来探索地质不确定性对丹麦某地地下水流动模式的影响。地统计学模型的实现被用作在地下水建模系统(GMS)建模环境中从模块化三维有限差分地下水模型(MODFLOW)开发的地下水模型的输入。在三种情况下进行了不确定性分析,包括模拟地下水水位分布和旅行时间。第一种情况意味着100个随机地质模型都为相同的地质单元分配了相同的水力参数。在第二种情况下,对相同的100个地质模型进行了模型优化,其中每个模型的水力参数都是通过对水头和水流流量的观测值进行标定来估算的;在第三种情况下,每个地质模型都使用216个随机参数集运行。分析表明,概念性地质模型的不确定性与嵌入式水力参数的不确定性一样重要。

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