民俗学 发表于 2025-3-21 18:29:30
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https://doi.org/10.1007/978-94-009-3625-6Fundament; contaminant; finite element method; groundwater; uncertainty; hydrogeologyRuptured-Disk 发表于 2025-3-22 01:49:37
http://reply.papertrans.cn/16/1501/150036/150036_3.png保存 发表于 2025-3-22 04:46:45
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On the Concept and Size of a Representative Elementary Volume (Rev)This chapter discusses the concept of the Representative Elementary Volume (REV) that serves as a cornerstone in the continuum modeling of transport phenomena in porous media (4). Following the presentation of the concept, quantitative criteria are presented for the selection of the size of the REV.改革运动 发表于 2025-3-22 13:54:06
Conflict and Conflict Resolution in Families transported in a porous medium domain (2). The objective of this chapter is to develop expressions for the macroscopic advective and diffusive fluxes of mass and heat in terms of macroscopic state variables.Chivalrous 发表于 2025-3-22 19:20:34
Preventive Psychiatry and World Problemsysical modeling using visual techniques can give some of the necessary descriptions leading to the proper formulation of mathematical models for predicting reservoir performance. This chapter describes the micromodel techniques developed at Imperial College, highlighting particularly those involving漂泊 发表于 2025-3-23 00:39:04
Davide Carneiro,Paulo Novais,José Nevesd free or natural convective movements, these flows depend on density differences due to temperature gradients and boundary conditions. Generally speaking, convective movements which tend to homogenize the whole fluid volume where they take place have two main effects: produce a non-uniform insitu tVEST 发表于 2025-3-23 02:36:57
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Davide Carneiro,Paulo Novais,José Neveshysical processes: (1) buoyancy flow, (2) forced convection, (3) thermal conduction and thermal dispersion. This chapter is divided into two parts. The first part presents an analysis of buoyancy flow causing the tilting of the interface (thermal front) between hot and cold water. The second part de