以局部尺度弥散为特征的异质介质中的放大传输:流道、宏观阻滞和参数预测

IF 4 2区 环境科学与生态学 Q1 WATER RESOURCES
Lian Zhou, Scott K. Hansen
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引用次数: 0

摘要

许多关于异质达西流输运的理论研究只考虑了平流。当忽略局部尺度弥散时,通量加权会随着时间的推移而持续存在;拉格朗日和欧拉平均流速分布彼此简单相关,并与底层水力传导场的方差相关。局部尺度色散会使这种关系复杂化,可能导致最初通量加权的溶质经历低速区域,以及由于相邻流线之间的溶质横向移动而产生泰勒型宏观色散。为了研究局部尺度色散与电导率对数方差、相关长度和各向异性之间的相互作用,我们在大尺度、高分辨率多变量高斯随机电导率场中对空间周期性二维达西流的流动和平流-色散传输进行了蒙特卡罗研究。我们在所有异质性水平上都观察到了流动通道,并对其程度进行了量化。我们发现在放大系统中存在大量有效迟滞的证据,这与流动通道的增加有关,并观察到有限的泰勒型宏观分散,我们对此进行了物理解释。在释放后的短距离内,拉格朗日速度达到了准恒定,这就允许使用我们之前提出的简化连续时间随机行走(CTRW)模型,其中过渡时间分布被理解为无流动异质性的等效系统中单位时间的时间映射。数值数据集就是用这样的 CTRW 模型建立的;我们展示了定义 CTRW 过渡时间分布的无量纲参数是如何通过无量纲异质性统计进行预测的,并为此提供了经验方程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Upscaling transport in heterogeneous media featuring local-scale dispersion: Flow channeling, macro-retardation and parameter prediction
Many theoretical treatments of transport in heterogeneous Darcy flows consider advection only. When local-scale dispersion is neglected, flux weighting persists over time; mean Lagrangian and Eulerian flow velocity distributions relate simply to each other and to the variance of the underlying hydraulic conductivity field. Local-scale dispersion complicates this relationship, potentially causing initially flux-weighted solute to experience lower-velocity regions as well as Taylor-type macrodispersion due to transverse solute movement between adjacent streamlines. To investigate the interplay of local-scale dispersion with conductivity log-variance, correlation length, and anisotropy, we perform a Monte Carlo study of flow and advective-dispersive transport in spatially-periodic 2D Darcy flows in large-scale, high-resolution multivariate Gaussian random conductivity fields. We observe flow channeling at all heterogeneity levels and quantify its extent. We find evidence for substantial effective retardation in the upscaled system, associated with increased flow channeling, and observe limited Taylor-type macrodispersion, which we physically explain. A quasi-constant Lagrangian velocity is achieved within a short distance of release, allowing usage of a simplified continuous-time random walk (CTRW) model we previously proposed in which the transition time distribution is understood as a temporal mapping of unit time in an equivalent system with no flow heterogeneity. The numerical data set is modeled with such a CTRW; we show how dimensionless parameters defining the CTRW transition time distribution are predicted by dimensionless heterogeneity statistics and provide empirical equations for this purpose.
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来源期刊
Advances in Water Resources
Advances in Water Resources 环境科学-水资源
CiteScore
9.40
自引率
6.40%
发文量
171
审稿时长
36 days
期刊介绍: Advances in Water Resources provides a forum for the presentation of fundamental scientific advances in the understanding of water resources systems. The scope of Advances in Water Resources includes any combination of theoretical, computational, and experimental approaches used to advance fundamental understanding of surface or subsurface water resources systems or the interaction of these systems with the atmosphere, geosphere, biosphere, and human societies. Manuscripts involving case studies that do not attempt to reach broader conclusions, research on engineering design, applied hydraulics, or water quality and treatment, as well as applications of existing knowledge that do not advance fundamental understanding of hydrological processes, are not appropriate for Advances in Water Resources. Examples of appropriate topical areas that will be considered include the following: • Surface and subsurface hydrology • Hydrometeorology • Environmental fluid dynamics • Ecohydrology and ecohydrodynamics • Multiphase transport phenomena in porous media • Fluid flow and species transport and reaction processes
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