Browsing by Author "Kang, Peter K"

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    Anomalous Transport in Dissolving Porous Media: Transitions Between Fickian and Non-Fickian Regimes
    (2025-02-17) Deng, Jingxuan; Sharma, Rishabh; Szymczak, Piotr; Kang, Peter K; pkkang@umn.edu; Kang, Peter K; University of Minnesota Kang Research Lab
    Mineral dissolution is a key geologic process with broad impacts on natural processes and human activities. Depending on the interplay between advection, diffusion, and reaction rates, mineral dissolution can produce various dissolution patterns, such as wormholing and uniform dissolution. The resulting changes in pore structure directly influence the flow field, which in turn control solute transport behavior. In this study, we conducted numerical modeling of mineral dissolution and solute transport in pore networks to investigate how initial network heterogeneity and dissolution regimes affect transport dynamics. Our findings show that wormholing increases network heterogeneity by creating preferential flow paths and stagnation zones, resulting in a transition from Fickian to non-Fickian transport. Conversely, uniform dissolution extensively homogenizes the pore network and the flow field, leading to a transition from non-Fickian to Fickian transport, even in networks with high initial heterogeneity. Based on the initial heterogeneity and Damköhler number, transitions can be predicted.
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    Data Repository for Effects of Fluid Flow and Fracture Aperture on Solute Exchange in Triple Porosity Carbonates: Etched Rock Core Experiments and Numerical Modeling
    (2025-01-30) Soucey, Charles E; Sutton, Collin R; Zahasky, Christopher; Yang, Weipeng; Kang, Peter K; pkkang@umn.edu; Kang, Peter K; Kang Research Lab
    The data contained in this repository is related to the results and figures shown in the manuscript "Effects of Fluid Flow and Fracture Aperture on Solute Exchange in Triple Porosity Carbonates: Etched Rock Core Experiments and Numerical Modeling." The data encompasses multiple different data types and covers all of the major experiments used in the manuscript, including PET scan data extracted from core flooding experiments in our etched rock cores, COMSOL numerical model files, image data from digital photographs and HSV thresholding of cores, and breakthrough curve data with model files for MFIT curve fitting. The files included here are the necessary files for replicating the primary results outlined in the paper. This data is now released for the purpose of allowing open access to data and information for the purpose of replicating our results in future studies.
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    Numerical simulation setup for variable-density flows in vertical fractures
    (2023-09-07) Cao, Hongfan; Yoon, Seonkyoo; Kang, Peter K; cao00137@umn.edu; Cao, Hongfan; University of Minnesota Kang Research Group
    Fluids with different densities often coexist in subsurface fractures and lead to variable-density flows that control subsurface processes such as seawater intrusion, contaminant transport, and geologic carbon sequestration. In nature, fractures have dip angles relative to gravity, and density effects are maximized in vertical fractures. However, most studies on flow and transport through fractures are often limited to horizontal fractures. Here, we study the mixing and transport of variable density fluids in vertical fractures by combining three-dimensional (3D) pore-scale numerical simulations and visual laboratory experiments. Two miscible fluids with different densities are injected through two inlets at the bottom of a fracture and exit from an outlet at the top of the fracture. Laboratory experiments show the emergence of an unstable focused flow path, which we term a “runlet.” We successfully reproduce an unstable runlet using 3D numerical simulations, and elucidate the underlying mechanisms triggering the runlet. Dimensionless number analysis shows that the runlet instability arises due to the Rayleigh-Taylor instability, and flow topology analysis is applied to identify 3D vortices that are caused by the Rayleigh-Taylor instability. Even under laminar flow regimes, fluid inertia is shown to control the runlet instability by affecting the size and movement of vortices. Finally, we confirm the emergence of a runlet in rough-walled fractures. Since a runlet dramatically affects fluid distribution, residence time, and mixing, the findings in this study have direct implications for the management of groundwater resources and subsurface applications.
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    Particle image velocimetry data characterizing flow and turbulence fields at free-flow-porous media interface
    (2020-12-01) Kang, Peter K; Kim, Junsong; pkkang@umn.edu; Kang, Peter K
    The data includes two-dimensional (2D) instantaneous velocity fields and time-averaged 2D flow properties. We obtained the velocity data in an experimental flume, which is composed of an open channel and underlying porous media, at the St. Anthony Falls Laboratory, University of Minnesota using Particle Image Velocimetry (PIV). The PIV is a non-intrusive laser optical measurement technique, which measures flow at the high spatiotemporal resolution by estimating cross-correlations between laser-illuminated subsequent images recorded by a high-speed camera. We used the PIV-measured 2D flow fields to validate the results of numerical flow simulations based on Large Eddy Simulation. The main objective of this study is to investigate pore-scale flow effects on solute transport across open channel- porous media interfaces. The released data would also be useful to researchers who need to validate flow simulation results.