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Bayesian approach for three-dimensional aquifer characterization at the Hanford 300 Area

机译:汉福德300区三维含水层表征的贝叶斯方法

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This study presents a stochastic, three-dimensional characterization of a heterogeneous hydraulic conductivity field within the Hanford 300 Area, Washington, USA, by assimilating large-scale, constant-rate injection test data with small-scale, three-dimensional electromagnetic borehole flowmeter (EBF) measurement data. We first inverted the injection test data to estimate the transmissivity field, using zeroth-order temporal moments of pressure buildup curves. We applied a newly developed Bayesian geostatistical inversion framework, the method of anchored distributions (MAD), to obtain a joint posterior distribution of geostatistical parameters and local log-transmissivities at multiple locations. The unique aspects of MAD that make it suitable for this purpose are its ability to integrate multi-scale, multi-type data within a Bayesian framework and to compute a nonparametric posterior distribution. After we combined the distribution of transmissivities with depth-discrete relative-conductivity profile from the EBF data, we inferred the three-dimensional geostatistical parameters of the log-conductivity field, using the Bayesian model-based geostatistics. Such consistent use of the Bayesian approach throughout the procedure enabled us to systematically incorporate data uncertainty into the final posterior distribution. The method was tested in a synthetic study and validated using the actual data that was not part of the estimation. Results showed broader and skewed posterior distributions of geostatistical parameters except for the mean, which suggests the importance of inferring the entire distribution to quantify the parameter uncertainty.
机译:这项研究通过将大规模,恒定速率的注入测试数据与小规模的三维电磁井流量计同化,提出了美国汉福德300地区内非均质水力传导率场的随机三维表征( EBF)测量数据。首先,我们使用压力累积曲线的零阶瞬时矩来反转注入测试数据,以估算透射率场。我们应用了新开发的贝叶斯地统计反演框架,即锚定分布(MAD)方法,以获得多个位置的地统计参数和局部对数透射率的联合后验分布。 MAD使其适用于此目的的独特方面是其在贝叶斯框架内集成多尺度,多类型数据并计算非参数后验分布的能力。从EBF数据中将透射率的分布与深度离散的相对电导率曲线结合起来后,我们使用基于贝叶斯模型的地统计学方法推导了对数电导率场的三维地统计参数。在整个过程中贝叶斯方法的这种一致使用使我们能够系统地将数据不确定性纳入最终的后验分布。该方法在综合研究中进行了测试,并使用不属于估算范围的实际数据进行了验证。结果表明,除均值外,地统计学参数的后验分布较宽且偏斜,这表明推断整个分布以量化参数不确定性的重要性。

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