Groundwater flow in karstic aquifer: analytic solution of dual-porosity fractional model to simulate groundwater flow-Reference-Cited by-同舟云学术

Groundwater flow in karstic aquifer: analytic solution of dual-porosity fractional model to simulate groundwater flow

Published:2022-09-04 Issue:1 Volume:30 Page:598-608
ISSN:2769-0911
Container-title:Applied Mathematics in Science and Engineering
language:en
Short-container-title:Applied Mathematics in Science and Engineering

Author:

Yadav Mahaveer Prasad¹^ORCID,Agarwal Ritu²^ORCID,Purohit Sunil Dutt³^ORCID,Kumar Devendra⁴^ORCID,Suthar Daya Lal⁵^ORCID

Affiliation:

1. Department of Mathematics, Amity University Rajasthan, Jaipur, Rajasthan, India

2. Department of Mathematics, Malaviya National Institute of Technology, Jaipur, India

3. Department of HEAS (Mathematics), Rajasthan Technical University, Kota, India

4. Department of Mathematics, University of Rajasthan, Jaipur, Rajasthan, India

5. Department of Mathematics, Wollo University, Dessie, Ethiopia

Publisher

Informa UK Limited

Link

https://www.tandfonline.com/doi/pdf/10.1080/27690911.2022.2117913

Reference32 articles.

1. Mohrlok U, Sauter M. Modelling groundwater flow in a karst terrain using discrete and double-continuum approaches. Importance of spatial and temporal distribution of recharge. Proceedings of the 12th International Congress of Speleology; 6th Conference on Limestone Hydrology and Fissured Media; Vol. 2; 1997. p. 167–170.

2. Mohrlok U, Teutsch G. Double-continuum porous equivalent (DCPE) versus discrete modelling in karst terraces. Karst Waters & Environmental Impacts; 1997. p. 319–326.

3. Analytical 1D dual-porosity equivalent solutions to 3D discrete single-continuum models. Application to karstic spring hydrograph modelling

4. The Behavior of Naturally Fractured Reservoirs

5. Pressure Transient Analysis of Naturally Fractured Reservoirs with Uniform Fracture Distribution

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