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首页> 外文期刊>Journal of Hydrology >Three-dimensional imaging of aquifer and aquitard heterogeneity via transient hydraulic tomography at a highly heterogeneous field site
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Three-dimensional imaging of aquifer and aquitard heterogeneity via transient hydraulic tomography at a highly heterogeneous field site

机译:高度异质田地现场瞬态水力层析术的含水层和水流工异质性的三维成像

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Previous studies have shown that geostatistics-based transient hydraulic tomography (THT) is robust for subsurface heterogeneity characterization through the joint inverse modeling of multiple pumping tests. However, the hydraulic conductivity (K) and specific storage (S-s) estimates can be smooth or even erroneous for areas where pumping/observation densities are low. This renders the imaging of interlayer and intralayer heterogeneity of highly contrasting materials including their unit boundaries difficult. In this study, we further test the performance of THT by utilizing existing and newly collected pumping test data of longer durations that showed drawdown responses in both aquifer and aquitard units at a field site underlain by a highly heterogeneous glaciofluvial deposit. The robust performance of the THT is highlighted through the comparison of different degrees of model parameterization including: (1) the effective parameter approach; (2) the geological zonation approach relying on borehole logs; and (3) the geostatistical inversion approach considering different prior information (with/without geological data). Results reveal that the simultaneous analysis of eight pumping tests with the geostatistical inverse model yields the best results in terms of model calibration and validation. We also find that the joint interpretation of long-term drawdown data from aquifer and aquitard units is necessary in mapping their full heterogeneous patterns including intralayer variabilities. Moreover, as geological data are included as prior information in the geostatistics-based THT analysis, the estimated K values increasingly reflect the vertical distribution patterns of permeameter-estimated K in both aquifer and aquitard units. Finally, the comparison of various THT approaches reveals that differences in the estimated K and S-s tomograms result in significantly different transient drawdown predictions at observation ports. (C) 2018 Elsevier B.V. All rights reserved.
机译:以前的研究表明,基于地统计学的瞬态液压断层摄影(THT)通过多个泵送测试的联合逆建模,对地下异质性表征具有鲁棒性。然而,液压导电性(k)和特定储存(S-S)估计对于泵送/观察密度低的区域来说是光滑的甚至错误的。这使得具有高对比度材料的层间和体内异质性的成像,包括其单位边界。在这项研究中,我们进一步通过利用现有和新收集的泵送测试数据来测试THT的性能,并通过高度异质的甘草流沉积物在现场出现的含水层和水流工部件中显示出含水层和水流工部件的绘制响应。通过比较不同程度的模型参数化的比较突出了THT的稳健性能,包括:(1)有效参数方法; (2)地质区划方法依赖于钻孔原木; (3)考虑不同先前信息的地质统计反演方法(有/没有地质数据)。结果表明,与地质统计逆模型的8个泵送测试同时分析,在模型校准和验证方面产生了最佳结果。我们还发现,在绘制其全相容模式,包括含水层和水流工单位的长期缩减数据的联合解释是必要的,包括intoralayer可变性。此外,随着基于地质数据的基于地质数据的先前信息包括地质数据,估计的k值越来越多地反映了含水层和水流单元中估计型估计k的垂直分布模式。最后,各种THT方法的比较揭示了估计的K和S-S断层照片的差异导致观察端口的显着不同的瞬态缩减预测。 (c)2018年elestvier b.v.保留所有权利。

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