地下水模拟不确定性量化的高效计算方法

H. Kunstmann
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引用次数: 2

摘要

当必须在水管理问题上作出保守的决定时,对不确定性进行量化是必要的。蒙特卡罗技术适合这种分析,但通常需要大量的计算工作。另一种计算效率高的方法是一阶二阶矩法(FOSM),它将参数不确定性直接传播到结果中。我们将FOSM方法应用于地下水流动和溶质输运方程。它显示了基于测量的水头和浓度的校准如何产生相互不确定度原理,该原理与可行透过率和补给率的不确定度相关。该方法用于计算稳态头和稳态溶质浓度的不确定度。该方法以半干旱的博茨瓦纳的帕拉路含水层为例进行了说明,其中地下水补给的不确定性范围的量化是主要的兴趣。FOSM法得到的不确定性界与蒙特卡罗法得到的结果吻合较好。结果表明,在计划抽水量下,超采超过帕拉路含水层自然补给量的概率为30%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Computationally efficient methods for the quantification of uncertainties in groundwater modelling
When conservative decisions have to be made in water management questions, the quantification of uncertainties is necessary. Monte Carlo techniques are suited for this analysis but usually require a huge computational effort. An alternative and computationally efficient approach is the First Order Second Moment (FOSM) method which directly propagates the uncertainty originating from parameter uncertainty into the result. We apply the FOSM method to both the groundwater flow and solute transport equations. It is shown how calibration on the basis of measured heads and concentrations yield the Principle of Interdependent Uncertainty that correlates the uncertainties of feasible transmissivities and recharge rates. The method is used to compute the uncertainty of steady state heads and of steady state solute concentrations. The method is illustrated by application to the Palla Road aquifer in semiarid Botswana, for which the quantification of the uncertainty range of groundwater recharge is of prime interest. The uncertainty bounds obtained by the FOSM method correspond well with the results obtained by the Monte Carlo method. It is shown that at the planned abstraction rate the probability of exceeding the natural replenishment of the Palla Road aquifer by overpumping is 30%.
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