Incorporating Super-Diffusion due to Sub-Grid Heterogeneity to Capture Non-Fickian Transport

被引:15
作者
Baeumer, Boris [1 ]
Zhang, Yong [2 ,3 ]
Schumer, Rina [4 ]
机构
[1] Univ Otago, Dept Math & Stat, Dunedin, New Zealand
[2] Univ Alabama, Dept Geol Sci, Tuscaloosa, AL 35487 USA
[3] Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210098, Jiangsu, Peoples R China
[4] Desert Res Inst, Div Hydrol Sci, Reno, NV 89512 USA
基金
美国国家科学基金会;
关键词
ADVECTION-DISPERSION EQUATION; LEVY MOTION; HYDRAULIC CONDUCTIVITY; FRACTIONAL DISPERSION; SOLUTE TRANSPORT; MODELS; MEDIA; FLIGHTS; ORDER; TIME;
D O I
10.1111/gwat.12267
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Numerical transport models based on the advection-dispersion equation (ADE) are built on the assumption that sub-grid cell transport is Fickian such that dispersive spreading around the average velocity is symmetric and without significant tailing on the front edge of a solute plume. However, anomalous diffusion in the form of super-diffusion due to preferential pathways in an aquifer has been observed in field data, challenging the assumption of Fickian dispersion at the local scale. This study develops a fully Lagrangian method to simulate sub-grid super-diffusion in a multidimensional regional-scale transport model by using a recent mathematical model allowing super-diffusion along the flow direction given by the regional model. Here, the time randomizing procedure known as subordination is applied to flow field output from MODFLOW simulations. Numerical tests check the applicability of the novel method in mapping regional-scale super-diffusive transport conditioned on local properties of multidimensional heterogeneous media.
引用
收藏
页码:699 / 708
页数:10
相关论文
共 43 条
[1]  
[Anonymous], 2000, MODFLOW 2000 US GEOL
[2]   Subordinated advection-dispersion equation for contaminant transport [J].
Baeumer, B ;
Benson, DA ;
Meerschaert, MM ;
Wheatcraft, SW .
WATER RESOURCES RESEARCH, 2001, 37 (06) :1543-1550
[3]  
Baeumer B., 2001, Fract. Calc. Appl. Anal., V4, P481
[4]   Tempered stable Levy motion and transient super-diffusion [J].
Baeumer, Boris ;
Meerschaert, Mark M. .
JOURNAL OF COMPUTATIONAL AND APPLIED MATHEMATICS, 2010, 233 (10) :2438-2448
[5]   Unbounded functional calculus for bounded groups with applications [J].
Baeumer, Boris ;
Haase, Markus ;
Kovacs, Mihaly .
JOURNAL OF EVOLUTION EQUATIONS, 2009, 9 (01) :171-195
[6]   Spatial scale effect on the upper soil effective parameters of a distributed hydrological model [J].
Barrios, M. ;
Frances, F. .
HYDROLOGICAL PROCESSES, 2012, 26 (07) :1022-1033
[7]   Models of sub-grid variability in numerical simulations of solute transport in heterogeneous porous formations: three-dimensional flow and effect of pore-scale dispersion [J].
Bellin, A ;
Lawrence, AE ;
Rubin, Y .
STOCHASTIC ENVIRONMENTAL RESEARCH AND RISK ASSESSMENT, 2004, 18 (01) :31-38
[8]   The fractional-order governing equation of Levy motion [J].
Benson, DA ;
Wheatcraft, SW ;
Meerschaert, MM .
WATER RESOURCES RESEARCH, 2000, 36 (06) :1413-1423
[9]   Application of a fractional advection-dispersion equation [J].
Benson, DA ;
Wheatcraft, SW ;
Meerschaert, MM .
WATER RESOURCES RESEARCH, 2000, 36 (06) :1403-1412
[10]   Pore-scale modeling of transverse dispersion in porous media [J].
Bijeljic, Branko ;
Blunt, Martin J. .
WATER RESOURCES RESEARCH, 2007, 43 (12)