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Bayesian approach to quantify parameter uncertainty and impacts on predictive flow and mass transport in heterogeneous aquifer

机译:贝叶斯方法量化参数不确定性及其对非均质含水层中预测流量和质量输运的影响

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摘要

Groundwater flow and mass transport predictions are subjected to uncertainty due to heterogeneity of hydraulic conductivity, whose variability in space is considerably higher than that of other hydraulic properties relevant to groundwater flow. To characterize the distribution of hydraulic conductivity, random space function (RSF) is often used. The Bayesian approach was applied to quantitatively study the effect of parameter uncertainty in RSF on a hypothetical two-dimensional uniform groundwater flow and mass transport. Specifically, the parameter uncertainty transmitted to macrodispersion in mass transport model was also inferred. The results showed that the posterior probability distributions of parameters were updated after Bayesian inference. The numerical experiments indicated that the overall predictive uncertainty was increased with simulating time along the flow direction. As to the relative contribution of the two types of uncertainty, it indicated that parametric uncertainty was a little more important than stochastic uncertainty for the predictive uncertainty of hydraulic head. When the uncertainty of hydraulic head as well as macrodispersion was transported to mass transport model, a much bigger contribution of stochastic uncertainty was observed. Therefore, parametric uncertainty should not be neglected during the process of subsurface simulation.
机译:由于水力传导率的非均质性,地下水流量和质量输运预测存在不确定性,其空间变异性明显高于与地下水流有关的其他水力性质。为了表征水力传导率的分布,经常使用随机空间函数(RSF)。贝叶斯方法用于定量研究RSF中参数不确定性对假设的二维均匀地下水流和质量输运的影响。具体来说,还可以推断出传质模型中传递给宏观分散的参数不确定性。结果表明,经过贝叶斯推断后,参数的后验概率分布得到了更新。数值实验表明,随着时间的流逝,总的预测不确定性随模拟时间的增加而增加。关于这两种不确定性的相对贡献,表明对于液压头的预测不确定性,参数不确定性比随机不确定性更重要。当将水头和宏观分散的不确定性转移到大规模运输模型时,观察到随机不确定性的贡献更大。因此,在地下模拟过程中不应忽略参数不确定性。

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