Time behavior of solute transport in heterogeneous media: transition from anomalous to normal transport

被引:350
作者
Dentz, M [1 ]
Cortis, A [1 ]
Scher, H [1 ]
Berkowitz, B [1 ]
机构
[1] Weizmann Inst Sci, Dept Environm Sci & Energy Res, IL-76100 Rehovot, Israel
基金
以色列科学基金会;
关键词
continuous time random walks; non-fickian transport;
D O I
10.1016/j.advwatres.2003.11.002
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
We study the time behavior of solute transport in a heterogeneous medium. We consider a spatially biased continuous time random walk (CTRW) governed by psi(s, t), the joint probability density for an event-displacement s with an event-time t. In this effective transport framework the concentration distribution of a solute is given by a generalized master equation (GME). We present results detailing the time dependence for the resident and flux concentrations, the center of mass velocity and the macroscopic dispersion coefficients of the solute plume. The Laplace transform of the GME is converted to a spatial differential equation resembling the advection dispersion equation (ADE), with Laplace space dependent coefficients though, and can then be solved explicitly in Laplace space. The transport behavior of the solute is then determined by accurate numerical inverse Laplace transforms. The confirmation of the accuracy of our methods is demonstrated by the excellent agreement with efficient random walk simulations based on the same psi(s, t). The psi(s, t) is given by the product of a Gaussian distribution for s and a truncated power-law distribution for t. This particular choice allows for a systematic study of the time regimes of anomalous and normal transport behavior and the transition from normal to anomalous behavior. The presented results show new aspects for the modeling of solute transport in heterogeneous media, in particular the effect of the system "memory" on plume patterns at asymptotically long times. In a specific application we solve for the contaminant flux entering a stream from a point injection of tracer in a catchment. The results are discussed as an independent test of a model of fractal stream chemistry in catchments. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:155 / 173
页数:19
相关论文
共 47 条
[1]  
Abramowitz M., 1970, HDB MATH FUNCTIONS
[2]  
[Anonymous], MATLAB FUNCTION NUME
[3]   Temporal behaviour of a solute cloud in a chemically heterogeneous porous medium [J].
Attinger, S ;
Dentz, M ;
Kinzelbach, H ;
Kinzelbach, W .
JOURNAL OF FLUID MECHANICS, 1999, 386 :77-104
[4]   Fractional Fokker-Planck equation, solution, and application [J].
Barkai, E .
PHYSICAL REVIEW E, 2001, 63 (04)
[5]   ON CHARACTERIZATION OF ANOMALOUS-DISPERSION IN POROUS AND FRACTURED MEDIA [J].
BERKOWITZ, B ;
SCHER, H .
WATER RESOURCES RESEARCH, 1995, 31 (06) :1461-1466
[6]   Anomalous transport in laboratory-scale, heterogeneous porous media [J].
Berkowitz, B ;
Scher, H ;
Silliman, SE .
WATER RESOURCES RESEARCH, 2000, 36 (01) :149-158
[7]   Anomalous transport in laboratory-scale, heterogeneous porous media (vol 36, pg 149, 2000) [J].
Berkowitz, B ;
Scher, H ;
Silliman, SE .
WATER RESOURCES RESEARCH, 2000, 36 (05) :1371-1371
[8]   Theory of anomalous chemical transport in random fracture networks [J].
Berkowitz, B ;
Scher, H .
PHYSICAL REVIEW E, 1998, 57 (05) :5858-5869
[9]   Physical pictures of transport in heterogeneous media: Advection-dispersion, random-walk, and fractional derivative formulations [J].
Berkowitz, B ;
Klafter, J ;
Metzler, R ;
Scher, H .
WATER RESOURCES RESEARCH, 2002, 38 (10)
[10]   Application of continuous time random walk theory to tracer test measurements in fractured and heterogeneous porous media [J].
Berkowitz, B ;
Kosakowski, G ;
Margolin, G ;
Scher, H .
GROUND WATER, 2001, 39 (04) :593-604