標(biāo)題: Titlebook: Dispersion in Heterogeneous Geological Formations; Brian Berkowitz Book 2002 Springer Science+Business Media Dordrecht 2002 contaminant.co [打印本頁(yè)] 作者: 味覺沒有 時(shí)間: 2025-3-21 19:08
書目名稱Dispersion in Heterogeneous Geological Formations影響因子(影響力)
書目名稱Dispersion in Heterogeneous Geological Formations影響因子(影響力)學(xué)科排名
書目名稱Dispersion in Heterogeneous Geological Formations網(wǎng)絡(luò)公開度
書目名稱Dispersion in Heterogeneous Geological Formations網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Dispersion in Heterogeneous Geological Formations被引頻次
書目名稱Dispersion in Heterogeneous Geological Formations被引頻次學(xué)科排名
書目名稱Dispersion in Heterogeneous Geological Formations年度引用
書目名稱Dispersion in Heterogeneous Geological Formations年度引用學(xué)科排名
書目名稱Dispersion in Heterogeneous Geological Formations讀者反饋
書目名稱Dispersion in Heterogeneous Geological Formations讀者反饋學(xué)科排名
作者: abduction 時(shí)間: 2025-3-21 23:13
On Perturbative Expansions to the Stochastic Flow Problem,sum of an average plus a stochastic fluctuation. To make the problem tractable, the log conductivity fluctuation, ., about the mean log conductivity, 1nK., is assumed to have finite variance, σ.. Historically, perturbation schemes have involved the assumption that σ. <1. Here it is shown that . may 作者: 送秋波 時(shí)間: 2025-3-22 02:31
Recursive Conditional Moment Equations for Advective Transport in Randomly Heterogeneous Velocity Fquantities that can be assigned unique values at each point in space-time. Yet in practice these parameters can be deduced from measurements only at selected locations where their values depend on the scale (support volume) and mode (instruments and procedure) of measurement. Quite often, the suppor作者: irradicable 時(shí)間: 2025-3-22 07:08
The Relative Dispersion and Mixing of Passive Solutes in Transport in Geologic Media,serve two major contributions of the fluctuating velocity field in the contaminant movement: (i) the spreading caused by velocity variations of scales lesser than that of the plume size, which we will call ‘relative’ spreading, and (ii) the meander-like movement of the plume as a whole caused by vel作者: Neuralgia 時(shí)間: 2025-3-22 10:53 作者: Protein 時(shí)間: 2025-3-22 16:05
Large-Time Spatial Covariance of Concentration of Conservative Solute and Application to the Cape C Lagrangian methodology to develop an analytical expression for the spatial covariance of the concentration, based on the central limit theorem and applicable to large times after injection. We use this expression to analyze the conservative tracer test data from the natural gradient experiment cond作者: Protein 時(shí)間: 2025-3-22 20:29 作者: ALIBI 時(shí)間: 2025-3-22 21:38
Role of Molecular Diffusion in Contaminant Migration and Recovery in an Alluvial Aquifer System, diffusion in the migration and recovery of a conservative solute. Heterogeneity is resolved to the hydrofacies scale with a discretization of 10.0, 5.0 and 0.5 m in the strike, dip and vertical directions of the alluvial-fan system. Transport simulations rely on recently developed random-walk techn作者: 五行打油詩(shī) 時(shí)間: 2025-3-23 02:08
Methods of Quantum Field Theory in the Physics of Subsurface Solute Transport,, resulting in new calculations of the solute macrodispersion tensor that derive from the solving Dyson equation with a subsequent renormalization group analysis. In this paper, we offer a critical evaluation of these techniques as they relate specifically to the derivation of a field-scale advectio作者: 教唆 時(shí)間: 2025-3-23 06:43 作者: 埋伏 時(shí)間: 2025-3-23 11:41 作者: nonchalance 時(shí)間: 2025-3-23 14:14 作者: outer-ear 時(shí)間: 2025-3-23 19:56
http://image.papertrans.cn/e/image/281517.jpg作者: 拔出 時(shí)間: 2025-3-24 01:25 作者: 易彎曲 時(shí)間: 2025-3-24 03:45
https://doi.org/10.1007/978-3-642-55227-4ns remain severely limited. While transport theories that treat ‘homogeneous’ porous media are mathematically convenient, such homogeneity rarely, if ever, exists in the field. The heterogeneity of natural geological formations at a wide range of scales necessitates consideration of more sophisticated transport theories.作者: habile 時(shí)間: 2025-3-24 06:51 作者: 昆蟲 時(shí)間: 2025-3-24 14:07
978-90-481-5638-2Springer Science+Business Media Dordrecht 2002作者: TATE 時(shí)間: 2025-3-24 17:50
https://doi.org/10.1007/978-3-642-55227-4ns remain severely limited. While transport theories that treat ‘homogeneous’ porous media are mathematically convenient, such homogeneity rarely, if ever, exists in the field. The heterogeneity of natural geological formations at a wide range of scales necessitates consideration of more sophisticat作者: capsaicin 時(shí)間: 2025-3-24 19:31
https://doi.org/10.1007/978-3-642-55227-4sum of an average plus a stochastic fluctuation. To make the problem tractable, the log conductivity fluctuation, ., about the mean log conductivity, 1nK., is assumed to have finite variance, σ.. Historically, perturbation schemes have involved the assumption that σ. <1. Here it is shown that . may 作者: Picks-Disease 時(shí)間: 2025-3-25 02:45
https://doi.org/10.1007/978-3-642-55227-4quantities that can be assigned unique values at each point in space-time. Yet in practice these parameters can be deduced from measurements only at selected locations where their values depend on the scale (support volume) and mode (instruments and procedure) of measurement. Quite often, the suppor作者: 包裹 時(shí)間: 2025-3-25 05:24
https://doi.org/10.1007/978-3-642-55227-4serve two major contributions of the fluctuating velocity field in the contaminant movement: (i) the spreading caused by velocity variations of scales lesser than that of the plume size, which we will call ‘relative’ spreading, and (ii) the meander-like movement of the plume as a whole caused by vel作者: GRUEL 時(shí)間: 2025-3-25 10:59 作者: CODE 時(shí)間: 2025-3-25 15:36
https://doi.org/10.1007/978-3-642-55227-4 Lagrangian methodology to develop an analytical expression for the spatial covariance of the concentration, based on the central limit theorem and applicable to large times after injection. We use this expression to analyze the conservative tracer test data from the natural gradient experiment cond作者: 尾巴 時(shí)間: 2025-3-25 16:25
https://doi.org/10.1007/978-3-642-55227-4ller-scale velocity variability must be accounted for indirectly, usually by increasing the magnitude of the dispersivity tensor (i.e. by introducing a so-called macrodispersivity). Most macrodispersion theories tacitly assume that a macrodispersivity tensor which works well when there is only small作者: Pericarditis 時(shí)間: 2025-3-25 20:03 作者: 繁忙 時(shí)間: 2025-3-26 02:00
https://doi.org/10.1007/978-3-642-55227-4, resulting in new calculations of the solute macrodispersion tensor that derive from the solving Dyson equation with a subsequent renormalization group analysis. In this paper, we offer a critical evaluation of these techniques as they relate specifically to the derivation of a field-scale advectio作者: 容易生皺紋 時(shí)間: 2025-3-26 07:42
https://doi.org/10.1007/978-3-642-55227-4sed. Because of hydrodynamic dispersion, tracer particles which sample different regions of the reservoir tend to arrive at different times, and the resulting distribution encodes information about the flow and the large-scale geometry of the reservoir in a simple way. In particular, the transit-tim作者: 西瓜 時(shí)間: 2025-3-26 12:27
https://doi.org/10.1007/978-3-642-55227-4he basic assumptions of local second-order theories. A governing equation that describes particles that undergo Lévy motion, rather than Brownian motion, readily describes the highly skewed and heavy-tailed plume development at the MADE site. The new governing equation is based on a fractional, rath作者: 一瞥 時(shí)間: 2025-3-26 13:46 作者: AER 時(shí)間: 2025-3-26 20:45
On Perturbative Expansions to the Stochastic Flow Problem,n V . are necessary. In particular, when the two point correlation function for the conductivity is assumed to be exponential or Gaussian, it is possible to estimate the magnitude of . in terms of . and various length scales. The ratio of the integral scale in the main direction of flow (A,) to the 作者: 打折 時(shí)間: 2025-3-26 22:11 作者: 沒有希望 時(shí)間: 2025-3-27 03:49
The Relative Dispersion and Mixing of Passive Solutes in Transport in Geologic Media,pressions for the relative mean concentration and its variance are presented. Then, the methodology is applied to the regional transport problem, where the influence of the size of the plume and the pore-scale dispersion are quantitatively assessed.作者: lesion 時(shí)間: 2025-3-27 06:16 作者: savage 時(shí)間: 2025-3-27 12:47 作者: JAMB 時(shí)間: 2025-3-27 14:18
Macrodispersivity and Large-scale Hydrogeologic Variability,city field includes both small and large-scale components, the macrodispersivity term does not appear to be able to capture all of the effects of small-scale variability. In this case the predicted plume is more well mixed and consistently underestimates peak solute concentrations at all times. We b作者: travail 時(shí)間: 2025-3-27 21:13
Role of Molecular Diffusion in Contaminant Migration and Recovery in an Alluvial Aquifer System,cted hold back of solute mass near source locations during ambient migration and pump-and-treat remediation is consistent with observations at LLNL, and reminiscent of observations at the MADE site of Columbus Air Force Base, Mississippi. Results confirm the important role of diffusion in low-conduc作者: Isometric 時(shí)間: 2025-3-28 01:23
Methods of Quantum Field Theory in the Physics of Subsurface Solute Transport,on-dispersion equation. Similarly, renormalization group analysis of the macrodispersion tensor has not yet provided results that go beyond what is available currently from the cumulant expansion approach.作者: 啤酒 時(shí)間: 2025-3-28 03:13
,Fractional Dispersion, Lévy Motion, and the MADE Tracer Tests,ants based only on the aquifer hydraulic properties. This supports the idea that the correct governing equation can be accurately determined before, or after, a contamin-ation event. While the traditional ADE fails to model a conservative tracer in the MADE aquifer, the fractional equation predicts 作者: temperate 時(shí)間: 2025-3-28 09:52
The Role of Probabilistic Approaches to Transport Theory in Heterogeneous Media,ion and breakthrough curves is advanced as a more useful characterization of the transport than the dispersion tensor, which is based on moments of the plume. The role of probabilistic approaches, such as CTRW, is appraised in the context of the interplay of spatial scales and levels of uncertainty.作者: agenda 時(shí)間: 2025-3-28 13:03
Book 2002tributions are intended to be as accessible aspossible to a wide readership of academics and professionals withdiverse backgrounds such as earth sciences, subsurface hydrology,petroleum engineering, and soil physics.作者: 交響樂 時(shí)間: 2025-3-28 16:53 作者: irradicable 時(shí)間: 2025-3-28 19:51 作者: NEG 時(shí)間: 2025-3-28 23:06 作者: 基因組 時(shí)間: 2025-3-29 03:53 作者: 旅行路線 時(shí)間: 2025-3-29 10:52 作者: Mortar 時(shí)間: 2025-3-29 11:46 作者: 圣人 時(shí)間: 2025-3-29 17:20 作者: 高興一回 時(shí)間: 2025-3-29 20:02 作者: 震驚 時(shí)間: 2025-3-30 03:47
https://doi.org/10.1007/978-3-642-55227-4on-dispersion equation. Similarly, renormalization group analysis of the macrodispersion tensor has not yet provided results that go beyond what is available currently from the cumulant expansion approach.作者: 禁止 時(shí)間: 2025-3-30 04:17 作者: Fsh238 時(shí)間: 2025-3-30 09:51
