標(biāo)題: Titlebook: Advances in Transport Phenomena in Porous Media; Jacob Bear,M. Yavuz Corapcioglu Book 1987 Martinus Nijhoff Publishers, Dordrecht 1987 Fun [打印本頁] 作者: 民俗學(xué) 時間: 2025-3-21 18:29
書目名稱Advances in Transport Phenomena in Porous Media影響因子(影響力)
書目名稱Advances in Transport Phenomena in Porous Media影響因子(影響力)學(xué)科排名
書目名稱Advances in Transport Phenomena in Porous Media網(wǎng)絡(luò)公開度
書目名稱Advances in Transport Phenomena in Porous Media網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Advances in Transport Phenomena in Porous Media被引頻次
書目名稱Advances in Transport Phenomena in Porous Media被引頻次學(xué)科排名
書目名稱Advances in Transport Phenomena in Porous Media年度引用
書目名稱Advances in Transport Phenomena in Porous Media年度引用學(xué)科排名
書目名稱Advances in Transport Phenomena in Porous Media讀者反饋
書目名稱Advances in Transport Phenomena in Porous Media讀者反饋學(xué)科排名
作者: 隱語 時間: 2025-3-21 23:03
https://doi.org/10.1007/978-94-009-3625-6Fundament; contaminant; finite element method; groundwater; uncertainty; hydrogeology作者: Ruptured-Disk 時間: 2025-3-22 01:49 作者: 保存 時間: 2025-3-22 04:46 作者: notion 時間: 2025-3-22 08:54
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.作者: 改革運動 時間: 2025-3-22 13:54
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.作者: Chivalrous 時間: 2025-3-22 19:20
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作者: 漂泊 時間: 2025-3-23 00:39
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 t作者: VEST 時間: 2025-3-23 02:36 作者: 品牌 時間: 2025-3-23 07:37
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作者: 我怕被刺穿 時間: 2025-3-23 12:38 作者: Allure 時間: 2025-3-23 14:05 作者: Interlocking 時間: 2025-3-23 19:17 作者: Generalize 時間: 2025-3-23 22:14 作者: Spinal-Fusion 時間: 2025-3-24 06:19
Nathalie Cron,Ina Quick,Stefan Vollmerpotential sites for repositories for nuclear waste. In Sweden, research was started in 1977 to investigate the flow and transport in low permeability crystalline rocks such as granites and gneisses..About 10 different potential sites have been investigated by surface mapping and by deep (700 m) dril作者: 使成核 時間: 2025-3-24 08:22 作者: Ambulatory 時間: 2025-3-24 13:00
Trauma, Transformation, and Transcendence,ace, such as the direction of the hydraulic gradient, for hydraulic heads in an aquifer. In (10), the method of simple kriging for stationary hydrologic variables is presented. In this chapter, universal kriging and the use of generalized covariances of order k are summarized, for the estimation of 作者: 脫水 時間: 2025-3-24 16:01 作者: interlude 時間: 2025-3-24 22:26
https://doi.org/10.1057/9780230584037ng to request the statistical distributions of predicted contaminant arrival to the biosphere, so that realistic confidence intervals can be obtained for the modeling results. To meet these needs, methods are being developed to quantify uncertainty in the subsurface flow and transport analysis seque作者: Antagonism 時間: 2025-3-24 23:29
NATO Science Series E:http://image.papertrans.cn/a/image/150036.jpg作者: Invigorate 時間: 2025-3-25 03:34 作者: 商議 時間: 2025-3-25 10:11 作者: Aggregate 時間: 2025-3-25 13:28
Book 1987 objective of this meeting was to present and discuss selected topics associated with transport phenomena in porous media. By their very nature, porous media and phenomena of transport of extensive quantities that take place in them, are very complex. The solid matrix may be rigid, or deformable (el作者: Outshine 時間: 2025-3-25 17:50 作者: 鎮(zhèn)痛劑 時間: 2025-3-25 21:50 作者: –LOUS 時間: 2025-3-26 03:58 作者: 通便 時間: 2025-3-26 06:11 作者: osteopath 時間: 2025-3-26 09:32
Natural Convection in Porous Mediais review, we deal mainly with the presentation of fundamental results obtained through the study of this phenomena in dispersed saturated porous media. Beginning with the formulation of basic equations and boundary conditions, we then successively review:作者: affinity 時間: 2025-3-26 14:11 作者: tariff 時間: 2025-3-26 17:21
Theory of Filtrationsions are derived for non-Newtonian and Newtonian fluids, one dimensional cylindrical and circular leaf filters. All are governed by an analogous rate expression..Experimental data shows the effect of cake pressure drop, filter area, particle size, particulate phases, and filter cake geometry.作者: 規(guī)范要多 時間: 2025-3-26 23:22
Multiphase Flow in Fractured Reservoirsoundary conditions. Simulation of one of the experiments shows that the prediction of imbibition flow rate by simulation models is critically dependent on a well defined capillary pressure curve..An improved dual porosity model for simulation of multiphase flow in fractured reservoirs is discussed.作者: Dislocation 時間: 2025-3-27 01:35
Book 1987may be isothermal or non-isothermal, with or without phase changes. Porous medium domains in which extensive quantities, such as mass of a fluid phase, component of a fluid phase, or heat of the porous medium as a whole, are being transported occur in the practice in a variety of disciplines.作者: 牽索 時間: 2025-3-27 08:58 作者: 事物的方面 時間: 2025-3-27 12:29
Preventive Psychiatry and World Problemscting reservoir performance. This chapter describes the micromodel techniques developed at Imperial College, highlighting particularly those involving pore scale events which depend on network and pore morphology.作者: 開始沒有 時間: 2025-3-27 16:50
Davide Carneiro,Paulo Novais,José Nevese first part presents an analysis of buoyancy flow causing the tilting of the interface (thermal front) between hot and cold water. The second part describes a numerical approach that studies the thermohydraulics of an aquifer thermal energy system where all three processes are taken into account.作者: 生來 時間: 2025-3-27 21:29 作者: 裙帶關(guān)系 時間: 2025-3-27 22:50
Pore Scale Physical Modeling of Transport Phenomena in Porous Mediacting reservoir performance. This chapter describes the micromodel techniques developed at Imperial College, highlighting particularly those involving pore scale events which depend on network and pore morphology.作者: Jargon 時間: 2025-3-28 03:33 作者: conquer 時間: 2025-3-28 10:16 作者: quiet-sleep 時間: 2025-3-28 13:34
Advective and Diffusive Fluxes in Porous Media 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.作者: 茁壯成長 時間: 2025-3-28 17:24
Pore Scale Physical Modeling of Transport Phenomena in Porous Mediaysical 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作者: 四指套 時間: 2025-3-28 20:34
Natural Convection in Porous Mediad 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 t作者: Semblance 時間: 2025-3-29 01:58
Heat and Mass Transport in Geothermal Reservoirs categories: vapor-saturated, two-phase boiling, liquid-saturated and supercritical. Liquid-saturated reservoirs and liquid-dominated or vapor-dominated reservoirs of the two-phase boiling type are the most common types exploited so far. There is growing interest in submarine geothermal systems and 作者: 辭職 時間: 2025-3-29 05:45
Thermohydraulics of an Aquifer Thermal Energy Storage Systemhysical 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作者: euphoria 時間: 2025-3-29 08:59
Mechanics of Fluids in Layered Soilsewpoint of phenomena such as subsidence due to the extraction of fluids from the aquifer. Special attention is paid to the influence of permeability contrasts such as occurring in a soil system consisting of layers of clay and sand, and the relative importance of the compressibilities of the various作者: sphincter 時間: 2025-3-29 12:55
Governing Equations for Particle Transport in Porous Mediaastewater treatment, well drilling, and in various liquid-solid separation processes. In liquid waste disposal projects, suspended solids can cause the injection well to become clogged, and groundwater quality can be endangered by suspended clay and silt particles migrating to the formation adjacent作者: 富足女人 時間: 2025-3-29 16:32 作者: SPURN 時間: 2025-3-29 19:48
Transport Equations for Fractured Porous Mediak has been a topic of increasing interest. In studies to date, the means by which transport phenomena in fractured rock have been mathematically visualized has taken two distinct routes. The need for different conceptualizations of fractured rock has arisen due to the diverse nature of fracturing in作者: 敬禮 時間: 2025-3-30 00:43 作者: CON 時間: 2025-3-30 06:25 作者: 賄賂 時間: 2025-3-30 11:19 作者: 影響帶來 時間: 2025-3-30 15:13 作者: 整潔漂亮 時間: 2025-3-30 17:10
Uncertainty Assessment for Fluid Flow and Contaminant Transport Modeling in Heterogeneous Groundwateng to request the statistical distributions of predicted contaminant arrival to the biosphere, so that realistic confidence intervals can be obtained for the modeling results. To meet these needs, methods are being developed to quantify uncertainty in the subsurface flow and transport analysis seque作者: 衰弱的心 時間: 2025-3-30 23:15
Heat and Mass Transport in Geothermal Reservoirstense heat output of such fields remains problematic, unless an intimate contact between circulating fluids and hot boundary rock of the magma is maintained over the lifetime of the activity. Convective downward migration of fluid along existing fractures and water penetration by thermal cracking of作者: cipher 時間: 2025-3-31 02:37 作者: 表被動 時間: 2025-3-31 08:05
