Heterogeneity across a broad range of scales in geologic porous media often manifests in observations of non-Fickian or anomalous transport. While traditional anomalous transport …
Flow channelization is a commonly observed phenomenon in fractured subsurface media where the flow of fluids is restricted primarily to highly transmissive fracture networks …
We investigate large‐scale particle motion and solute breakthrough in sparse three‐ dimensional discrete fracture networks characterized by power law distributed fracture …
We incorporate observations of real fracture aperture variability observed in laboratory experiments into an ensemble of three‐dimensional discrete fracture network (DFN) …
We study how the interplay between fracture aperture heterogeneity and tracer injection mode controls fluid flow and tracer transport in three‐dimensional (3D) discrete fracture …
S Yoon, JD Hyman, WS Han… - Journal of Geophysical …, 2023 - Wiley Online Library
Understanding mechanistic causes of non‐Fickian transport in fractured media is important for many hydrogeologic processes and subsurface applications. This study elucidates the …
PK Kang, Q Lei, M Dentz… - Water Resources Research, 2019 - Wiley Online Library
We investigate the effects of geological stress on fluid flow and tracer transport in natural fracture networks. We show the emergence of non‐Fickian (anomalous) transport from the …
JD Hyman, M Dentz - Advances in Water Resources, 2021 - Elsevier
We investigate the combined effects of network scale flow variability and retention due to matrix-diffusion on the scaling behavior of transport through fractured media. Two of the …