4.4 Editorial Material

Macroscale transport in channel-matrix systems via integral transforms

Journal

PHYSICAL REVIEW FLUIDS
Volume 6, Issue 4, Pages -

Publisher

AMER PHYSICAL SOC
DOI: 10.1103/PhysRevFluids.6.044501

Keywords

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Funding

  1. U.S. Department of Energy (DOE), Office of Biological and Environmental Research, Subsurface Biogeochemical Research (SBR) Program Award [DE-SC0016484]
  2. National Science Foundation (NSF) [1533874, 1654009]
  3. Div Of Chem, Bioeng, Env, & Transp Sys
  4. Directorate For Engineering [1533874] Funding Source: National Science Foundation
  5. U.S. Department of Energy (DOE) [DE-SC0016484] Funding Source: U.S. Department of Energy (DOE)

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This study presents a semi-analytical solution to predict macroscopic transport in channel-matrix shear flows efficiently, and demonstrates that under appropriate dynamic conditions, the coupled system at the macro scale can be simplified to a one-dimensional advection-dispersion equation, enabling real-time macro-scale concentration estimates.
Flow and transport in coupled channel-matrix systems are ubiquitous to many environmental and engineering applications such as flows in fractured porous media over canopies and in membrane filtration units. The multiscale nature of such systems, where the horizontal length scale is often orders of magnitude larger than the vertical one, allows one to employ vertically averaged descriptions of the system. As a result, two-dimensional transport in the channel and the matrix can be upscaled to a coupled system of transient one-dimensional advection-dispersion equations, where matrix and channel properties can be analytically related to macroscopic transport observables. In this work, we first develop a semianalytical solution based on integral transforms that can be employed to predict macroscopic transport in channel-matrix shear flows in a computationally efficient manner. Then we demonstrate that under appropriate dynamic conditions, the coupled system at the macroscale can be further simplified to a single upscaled one-dimensional advection-dispersion equation, which admits an analytical closed-form solution, thus enabling real-time macroscale concentration estimates in relevant applications.

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