A continuous time random walk (CTRW) integro-differential equation with chemical interaction

被引:11
作者
Ben -Zvi, Rami [1 ]
Nissan, Alon [1 ]
Scher, Harvey [1 ]
Berkowitz, Brian [1 ]
机构
[1] Weizmann Inst Sci, Dept Earth & Planetary Sci, IL-7610001 Rehovot, Israel
基金
以色列科学基金会;
关键词
SOLUTE TRANSPORT; POROUS-MEDIA; HETEROGENEOUS MEDIA; REACTIVE TRANSPORT; DISPERSION; FORMULATIONS;
D O I
10.1140/epjb/e2017-80417-8
中图分类号
O469 [凝聚态物理学];
学科分类号
070205 ;
摘要
A nonlocal-in-time integro-differential equation is introduced that accounts for close coupling between transport and chemical reaction terms. The structure of the equation contains these terms in a single convolution with a memory function M(t), which includes the source of non-Fickian (anomalous) behavior, within the framework of a continuous time random walk (CTRW). The interaction is non-linear and second -order, relevant for a bimolecular reaction A + B -> C. The interaction term Gamma P-A (s, t)PB (s, t) is symmetric in the concentrations of A and B (i.e. P-A and P-B); thus the source terms in the equations for A, B and C are similar, but with a change in sign for that of C. Here, the chemical rate coefficient, Gamma, is constant. The fully coupled equations are solved numerically using a finite element method (FEM) with a judicious representation of M(t) that eschews the need for the entire time history, instead using only values at the former time step. To begin to validate the equations, the FEM solution is compared, in lieu of experimental data, to a particle tracking method (CTRW-PT); the results from the two approaches, particularly for the C profiles, are in agreement. The FEM solution, for a range of initial and boundary conditions, can provide a good model for reactive transport in disordered media.
引用
收藏
页数:8
相关论文
共 30 条
[11]   Computing "Anomalous" contaminant transport in porous media: The CTRW MATLAB toolbox [J].
Cortis, A ;
Berkowitz, B .
GROUND WATER, 2005, 43 (06) :947-950
[12]   Time behavior of solute transport in heterogeneous media: transition from anomalous to normal transport [J].
Dentz, M ;
Cortis, A ;
Scher, H ;
Berkowitz, B .
ADVANCES IN WATER RESOURCES, 2004, 27 (02) :155-173
[13]   Anomalous reactive transport in porous media: Experiments and modeling [J].
Edery, Yaniv ;
Dror, Ishai ;
Scher, Harvey ;
Berkowitz, Brian .
PHYSICAL REVIEW E, 2015, 91 (05)
[14]   Reactive transport in disordered media: Role of fluctuations in interpretation of laboratory experiments [J].
Edery, Yaniv ;
Guadagnini, Alberto ;
Scher, Harvey ;
Berkowitz, Brian .
ADVANCES IN WATER RESOURCES, 2013, 51 :86-103
[15]   Dissolution and precipitation dynamics during dedolomitization [J].
Edery, Yaniv ;
Scher, Harvey ;
Berkowitz, Brian .
WATER RESOURCES RESEARCH, 2011, 47
[16]   Particle tracking model of bimolecular reactive transport in porous media [J].
Edery, Yaniv ;
Scher, Harvey ;
Berkowitz, Brian .
WATER RESOURCES RESEARCH, 2010, 46
[17]   Continuous-time random walks with internal dynamics and subdiffusive reaction-diffusion equations [J].
Eule, S. ;
Friedrich, R. ;
Jenko, F. ;
Sokolov, I. M. .
PHYSICAL REVIEW E, 2008, 78 (06)
[18]   A FAST ALGORITHM FOR THE EVALUATION OF HEAT POTENTIALS [J].
GREENGARD, L ;
STRAIN, J .
COMMUNICATIONS ON PURE AND APPLIED MATHEMATICS, 1990, 43 (08) :949-963
[19]   Integrodifferential formulations of the continuous-time random walk for solute transport subject to bimolecular A plus B → 0 reactions: From micro- to mesoscopic [J].
Hansen, Scott K. ;
Berkowitz, Brian .
PHYSICAL REVIEW E, 2015, 91 (03)
[20]  
Jiang SD, 2004, COMPUT MATH APPL, V47, P955, DOI 10.1016/j.camwa.2003.04.004