Influence of Tide‐Induced Unstable Flow on Seawater Intrusion and Submarine Groundwater Discharge-Reference-Cited by-同舟云学术

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Influence of Tide‐Induced Unstable Flow on Seawater Intrusion and Submarine Groundwater Discharge

Published:2021-04 Issue:4 Volume:57 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Res

Author:

Fang Yunhai¹²^ORCID,Zheng Tianyuan³^ORCID,Zheng Xilai¹²^ORCID,Yang Huiyu¹²,Wang Huan¹²,Walther Marc⁴

Affiliation:

1. College of Environmental Science and Engineering Ocean University of China Qingdao China

2. Key Laboratory of Marine Environment Science and Ecology Ministry of Education Ocean University of China Qingdao China

3. College of Engineering Ocean University of China Qingdao China

4. Department of Environmental Informatics Helmholtz‐Centre for Environmental Research‐UFZ Leipzig Leipzig Germany

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020WR029038

Reference47 articles.

1. Transience of seawater intrusion and retreat in response to incremental water-level variations

2. Influence of tides and waves on the fate of nutrients in a nearshore aquifer: Numerical simulations

3. Shape of the shallow aquifer at the fresh water–sea water interface on a high-energy sandy beach

4. Water table waves in an unconfined aquifer: Experiments and modeling

5. Experimental observations of watertable waves in an unconfined aquifer with a sloping boundary

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3. Dense Contaminants Mixing Into the Saltwater Wedge in Coastal Aquifers: Laboratory and Numerical Investigations;Water Resources Research;2024-07

4. Transient behavior of the freshwater-saltwater mixing zone after land reclamation in coastal aquifers;Advances in Water Resources;2024-07

5. Quantifying Seepage‐Face Evaporation and Its Effects on Groundwater Flow and Solute Transport in Small‐Slope Tidal Flat;Geophysical Research Letters;2024-06-18

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