Modeling bimolecular reactions and transport in porous media via particle tracking

被引:78
|
作者
Ding, Dong [1 ]
Benson, David A. [1 ]
Paster, Amir [2 ]
Bolster, Diogo [2 ]
机构
[1] Colorado Sch Mines, Golden, CO 80401 USA
[2] Univ Notre Dame, Environm Fluid Mech Labs, Dept Civil & Environm Engn & Earth Sci, Notre Dame, IN 46556 USA
基金
美国国家科学基金会;
关键词
Lagrangian particle method; Chemical reactions; DIFFUSION-PROCESSES; REACTION-KINETICS; SCALE DISPERSION; TRACER TEST; SIMULATION; RATES; BIODEGRADATION; EQUATIONS; EVOLUTION; DILUTION;
D O I
10.1016/j.advwatres.2012.11.001
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 use a particle-tracking method to simulate several one-dimensional bimolecular reactive transport experiments. In our numerical scheme, the reactants are represented by particles: advection and dispersion dominate the flow, and molecular diffusion dictates, in large part, the reactions. The particle/particle reactions are determined by a combination of two probabilities dictated by the physics of transport and energetics of reaction. The first is that reactant particles occupy the same volume over a short time interval. The second is the conditional probability that two collocated particles favorably transform into a reaction. The first probability is a direct physical representation of the degree of mixing in an advancing interface between dissimilar waters, and as such lacks empirical parameters except for the user-defined number of particles. This number can be determined analytically from concentration autocovariance, if this type of data is available. The simulations compare favorably to two physical experiments. In one, the concentration of product, 1,2-naphthoquinoe-4-aminobenzene (NQAB) from reaction between 1,2-naphthoquinone-4-sulfonic acid (NQS) and aniline (AN), was measured at the outflow of a column filled with glass beads at different times. In the other, the concentration distribution of reactants (CuSO4 and EDTA(4-)) and product (CuEDTA(2-)) were quantified by snapshots of light transmitted through a column packed with cryolite sand. These snapshots allow us to estimate concentration statistics and calculate the required number of particles. The experiments differ significantly due to a similar to 10(7) difference in thermodynamic rate coefficients, making the latter experiment effectively instantaneous. When compared to the solution of the advection-dispersion-reaction equation (ADRE) with the well-mixed reaction coefficient, the experiments and the particle-tracking simulations showed on the order of 20-40% less overall product, which is attributed to poor mixing. The poor mixing also leads to higher product concentrations on the edges of the mixing zones, which the particle model simulates more accurately than the ADRE. (C) 2012 Elsevier Ltd. All rights reserved.
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页码:56 / 65
页数:10
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