Simulating Unsaturated Zone of Soil for Estimating the Recharge Rate and Flow Exchange Between a River and an Aquifer
Author:
Publisher
Springer Science and Business Media LLC
Subject
Water Science and Technology,Civil and Structural Engineering
Link
http://link.springer.com/content/pdf/10.1007/s11269-019-02458-7.pdf
Reference31 articles.
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2. Bear J (2010) Modeling groundwater flow and contaminant transport. Springer Verlag, vol23, 834 P
3. Brenot A, Petelet-Giraud E, Gourcy L (2015) Insight from surface water-groundwater interactions in an alluvial aquifer: contributions of δ2H and δ18O of water, δ34SSO4 and δ18OSO4 of sulfates, 87Sr/86Sr ratio. Procedia Earth Planet Sci 13:84–87. https://doi.org/10.1016/j.proeps.2015.07.020
4. Christelis V, Mantoglou A (2018) Pumping optimization of coastal aquifers using seawater intrusion models of variable-Fidelity and evolutionary algorithms. Water Resour Manag 33:555–568. https://doi.org/10.1007/s11269-018-2116-0
5. Doppler T, Franssen HJH, Kaiser HP, Kuhlman U, Stauffer F (2007) Field evidence of a dynamic leakage coefficient for modelling river-aquifer interactions. J Hydrol 347(1–2):177–187. https://doi.org/10.1016/j.jhydrot.2007.09.017
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