Assessing the Connectivity of a Regional Fractured Aquifer Based on a Hydraulic Conductivity Field Reversed by Multi-Well Pumping Tests and Numerical Groundwater Flow Modeling-Reference-Cited by-同舟云学术

Assessing the Connectivity of a Regional Fractured Aquifer Based on a Hydraulic Conductivity Field Reversed by Multi-Well Pumping Tests and Numerical Groundwater Flow Modeling

Published:2023-08-10 Issue:6 Volume:34 Page:1926-1939
ISSN:1674-487X
Container-title:Journal of Earth Science
language:en
Short-container-title:J. Earth Sci.

Author:

Lin Jingjing^ORCID,Ma Rui^ORCID,Sun Ziyong,Tang Liansong

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://link.springer.com/content/pdf/10.1007/s12583-022-1674-5.pdf

Reference36 articles.

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2. Berkowitz, B., Bear, J., Braester, C., 1988. Continuum Models for Contaminant Transport in Fractured Porous Formations. Water Resources Research, 24(8): 1225–1236. https://doi.org/10.1029/wr024i008p01225

3. Bianchi, M., Pedretti, D., 2017. Geological Entropy and Solute Transport in Heterogeneous Porous Media. Water Resources Research, 53(6): 4691–4708. https://doi.org/10.1002/2016wr020195

4. Bianchi, M., Pedretti, D., 2018. An Entrogram-Based Approach to Describe Spatial Heterogeneity with Applications to Solute Transport in Porous Media. Water Resources Research, 54(7): 4432–4448. https://doi.org/10.1029/2018wr022827

5. Dijkstra, E. W., 1959. A Note on Two Problems in Connexion with Graphs. Numerische Mathematik, 1(1): 269–271. https://doi.org/10.1007/bf01386390

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