Modeling mixed retention and early arrivals in multidimensional heterogeneous media using an explicit Lagrangian scheme

被引:55
作者
Zhang, Yong [1 ]
Meerschaert, Mark M. [2 ]
Baeumer, Boris [3 ]
LaBolle, Eric M. [4 ]
机构
[1] Univ Alabama, Dept Geol Sci, Tuscaloosa, AL 35487 USA
[2] Michigan State Univ, Dept Stat & Probabil, E Lansing, MI 48824 USA
[3] Univ Otago, Dept Math & Stat, Dunedin, New Zealand
[4] Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA
基金
美国国家科学基金会;
关键词
NON-FICKIAN TRANSPORT; ADVECTION-DISPERSION EQUATION; WALK PARTICLE TRACKING; SOLUTE TRANSPORT; MASS-TRANSFER; ANOMALOUS TRANSPORT; FRACTIONAL DISPERSION; MACRODISPERSION EXPERIMENT; HYDRAULIC CONDUCTIVITY; BREAKTHROUGH CURVES;
D O I
10.1002/2015WR016902
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study develops an explicit two-step Lagrangian scheme based on the renewal-reward process to capture transient anomalous diffusion with mixed retention and early arrivals in multidimensional media. The resulting 3-D anomalous transport simulator provides a flexible platform for modeling transport. The first step explicitly models retention due to mass exchange between one mobile zone and any number of parallel immobile zones. The mobile component of the renewal process can be calculated as either an exponential random variable or a preassigned time step, and the subsequent random immobile time follows a Hyper-exponential distribution for finite immobile zones or a tempered stable distribution for infinite immobile zones with an exponentially tempered power-law memory function. The second step describes well-documented early arrivals which can follow streamlines due to mechanical dispersion using the method of subordination to regional flow. Applicability and implementation of the Lagrangian solver are further checked against transport observed in various media. Results show that, although the time-nonlocal model parameters are predictable for transport with retention in alluvial settings, the standard time-nonlocal model cannot capture early arrivals. Retention and early arrivals observed in porous and fractured media can be efficiently modeled by our Lagrangian solver, allowing anomalous transport to be incorporated into 2-D/3-D models with irregular flow fields. Extensions of the particle-tracking approach are also discussed for transport with parameters conditioned on local aquifer properties, as required by transient flow and nonstationary media.
引用
收藏
页码:6311 / 6337
页数:27
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