Time‐Fractional Flow Equations (t‐FFEs) to Upscale Transient Groundwater Flow Characterized by Temporally Non‐Darcian Flow Due to Medium Heterogeneity-Reference-Cited by-同舟云学术

Time‐Fractional Flow Equations (t‐FFEs) to Upscale Transient Groundwater Flow Characterized by Temporally Non‐Darcian Flow Due to Medium Heterogeneity

Published:2021-11 Issue:11 Volume:57 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resources Research

Author:

Xia Yuan¹^ORCID,Zhang Yong²^ORCID,Green Christopher T.³^ORCID,Fogg Graham E.⁴^ORCID

Affiliation:

1. College of Environmental Science and Engineering Guilin University of Technology Guilin China

2. Department of Geological Sciences University of Alabama Tuscaloosa AL USA

3. Integrated Modeling and Prediction Division U.S. Geological Survey Moffett Field CA USA

4. Hydrologic Sciences Department of Land, Air and Water Resources University of California Davis CA USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020WR029554

Reference66 articles.

1. Subordinated advection-dispersion equation for contaminant transport

2. Equivalent and effective conductivities of heterogeneous aquifers for steady source flow, with illustration for hydraulic tomography

3. A lithofacies approach for modeling non‐ F ickian solute transport in a heterogeneous alluvial aquifer

4. PREDICTION OF EFFECTIVE PERMEABILITY IN POROUS MEDIA BASED ON SPONTANEOUS IMBIBITION EFFECT

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