Shear-induced force and dispersion due to buoyancy in a horizontal Hele-Shaw cell
Prabakaran Rajamanickam

TL;DR
This study derives effective two-dimensional equations for shear flow and scalar transport in a horizontal Hele-Shaw cell influenced by buoyancy, highlighting shear-induced diffusion and buoyancy effects.
Contribution
It introduces a novel set of coupled equations accounting for shear-induced diffusion and buoyancy in a Hele-Shaw cell with variable density.
Findings
Effective diffusion coefficient for scalar transport derived
Shear-induced buoyancy force modifies Darcy's law
Framework for future scalar transport studies in Hele-Shaw cells
Abstract
This paper investigates shear flow in a Hele-Shaw cell, driven by varying horizontal buoyancy forces resulting from a horizontal density gradient induced by a scalar field. By employing asymptotic methods and taking the dependence of density and transport coefficients on the scalar field into account, effective two-dimensional hydrodynamic equations coupled with the scalar conservation equation are derived. These equations determine an effective diffusion coefficient for the scalar field accounting for shear-induced diffusion, and an effective shear-induced buoyancy force that modifies the classical Darcy's law. The derived equations provide a foundation for future research into various problems involving scalar transport in horizontal Hele-Shaw cells.
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Taxonomy
TopicsLandslides and related hazards · Geological formations and processes · Fluid Dynamics and Vibration Analysis
