Reactive Transport with Fluid-Solid Interactions in Dual-Porosity Media

被引:7
|
作者
Nissan, Alon [1 ,2 ,3 ]
Alcolombri, Uria [2 ]
de Schaetzen, Frederic [2 ]
Berkowitz, Brian [1 ]
Jimenez-Martinez, Joaquin [2 ,3 ]
机构
[1] Weizmann Inst Sci, Dept Earth & Planetary Sci, IL-7610001 Rehovot, Israel
[2] Swiss Fed Inst Technol, Dept Civil Environm & Geomat Engn, CH-8092 Zurich, Switzerland
[3] Swiss Fed Inst Aquat Sci & Technol, Dept Water Resources & Drinking Water, CH-8600 Dubendorf, Switzerland
来源
ACS ES&T WATER | 2021年 / 1卷 / 02期
基金
以色列科学基金会; 瑞士国家科学基金会;
关键词
fluid flow dynamics; surface reaction; microfluidics; hydrogel; enzymes; scaling laws; POROUS-MEDIA; PORE-SCALE; FLOW; MODEL; PERMEABILITY; DISSOLUTION; WATER; DISPERSION; CARBONATE; BIOFILMS;
D O I
10.1021/acsestwater.0c00043
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We study pore-scale dynamics of reactive transport in heterogeneous, dual-porosity media, wherein a reactant in the invading fluid interacts chemically with the surface of the permeable grains, leading to the irreversible reaction A(aq) + B-s -> C-aq. A microfluidic porous medium was synthesized, consisting of a single layer of hydrogel pillars (grains), chemically modified to contain immobilized enzymes on the grain surfaces. Fluorescence microscopy was used to monitor the spatiotemporal evolution of the reaction product C-aq at different flow rates (Peclet values) and to characterize the impact on its transport. The experimental setup enables delineation of three key features of the temporal evolution of the reaction product within the domain: (i) the characteristic time until the rate of C-aq production reaches steady state, (ii) the magnitude of the reaction rate at steady state, and (iii) the rate at which C-aq is flushed from the system. These features, individually, are found to be sensitive to the value of the Pedet number, because of the relative impact of diffusion (vs advection) on the production and spatiotemporal evolution of C-aq within the system. As the Peclet number increases, the production of C-aq is reduced and the transport becomes more localized within the vicinity of the grains. The dual-porosity feature causes the residence time of the transported species to increase, by forming stagnant zones and diffusive-dominant regions within the flow field, thus enhancing the reaction potential of the system. Using complementary numerical simulations, we explore these effects for a wider range of Peclet and Damkohler numbers and propose nonlinear scaling laws for the key features of the temporal evolution of C-aq.
引用
收藏
页码:259 / 268
页数:10
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