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樓主: 根深蒂固
51#
發(fā)表于 2025-3-30 11:56:24 | 只看該作者
52#
發(fā)表于 2025-3-30 16:21:08 | 只看該作者
Evaluation of Reactive Transport Processes in a Heterogeneous Porous Aquifer Within a Non-Parametricperiments. Multiple realizations of the K and R fields are generated to simulate the observed tracer transport stochastically. According to the results, the stochastic transport model seems suitable for highly heterogeneous aquifers such as at the ‘Horkheimer Insel’ test site.
53#
發(fā)表于 2025-3-30 18:52:21 | 只看該作者
Rational Use of Colour in Presentations,Groundwater modelling has become a reliable tool for solving groundwater budgeting and contamination problems. It has long been recognized, however, that the degree of reliability of this tool varies in proportion to the amount of information available on the heterogeneity of the flow system.
54#
發(fā)表于 2025-3-30 23:50:51 | 只看該作者
A Model of Aquifer HeterogeneityGroundwater modelling has become a reliable tool for solving groundwater budgeting and contamination problems. It has long been recognized, however, that the degree of reliability of this tool varies in proportion to the amount of information available on the heterogeneity of the flow system.
55#
發(fā)表于 2025-3-31 03:53:23 | 只看該作者
https://doi.org/10.1007/978-3-319-67870-2nd piezometric heads of a semi-confined fractured aquifer located in the North-eastern region of Portugal, based on the methodology presented in Rubin et al. (1990), for the Rio Maior aquifer, in Portugal, and in the study published by Lobo-Ferreira and Leit?o (1991) for the Bagueixe aquifer.
56#
發(fā)表于 2025-3-31 07:13:58 | 只看該作者
57#
發(fā)表于 2025-3-31 10:04:48 | 只看該作者
58#
發(fā)表于 2025-3-31 17:17:11 | 只看該作者
59#
發(fā)表于 2025-3-31 19:33:57 | 只看該作者
60#
發(fā)表于 2025-3-31 22:49:54 | 只看該作者
https://doi.org/10.1007/978-3-642-47472-9f their distance from the well. We find that this is indeed the case, although our second-order terms differ from that of Desbarats. We conclude with a highly heterogeneous example that illustrates the relative ranges over which the empirical formula and our second order expansion are accurate.
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