Influence of Tide‐Induced Unstable Flow on Seawater Intrusion and Submarine Groundwater Discharge. Issue 4 (22nd April 2021)

• Record Type: Journal Article
• Authors: Fang, Yunhai; Zheng, Tianyuan; Zheng, Xilai; Yang, Huiyu; Wang, Huan; Walther, Marc
• Is Part Of: Water resources research. Volume 57:Issue 4(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-04-22
• Subjects: salt finger -- saltwater intrusion -- submarine groundwater discharge -- tide -- unconfined aquifer; Hydrology -- Periodicals; 333.91
• DOI: 10.1029/2020WR029038
• Languages: English
• ISSNs: 0043-1397

Abstract

Abstract: Recent studies have confirmed the instability of tide‐induced upper saline plume (USP) in tidal beach aquifers. A systematic understanding of how the unstable USP contributes to groundwater flow and salinity distribution is still lacking. Here we used laboratory experiments and numerical simulations to examine the responses of the salinity distribution and submarine groundwater discharge (SGD) to tide‐induced unstable flow. The results revealed that changes in physical forcing conditions (tides and inland freshwater input) drove the transition of the USP from stable to unstable states. Meanwhile, the phase‐averaged SGD and its components fluctuated over time, and their oscillation amplitudes depended on the physical forcing conditions. There was a correlation between USP instability and the fluctuation of water exchange across the aquifer‐sea interface. The fluxes across the aquifer‐sea interface under unstable conditions usually varied considerably over time with a lower frequency in comparison to stable conditions. The extent of seawater intrusion (SWI) measured by the total salt mass stored in the aquifer also varied over time, especially under unstable conditions. The vibration tendency of the total salt mass was opposite to that of the sum of inland freshwater discharge and tide‐induced circulation efflux. For coastal aquifers affected by tides, SWI was dominated by the sum of inland freshwater discharge and tide‐induced circulation efflux, followed by the sum of inland freshwater input and tide‐induced circulation influx. These findings lay the foundation for gaining a better understanding of tide‐induced unstable flow and its potential implications. Key Points: The phase‐averaged submarine groundwater discharge (SGD) and seawater intrusion extent fluctuate with time, especially under unstable conditions There is a correlation between the instability of tide‐induced upper saline plume and the fluctuation of SGD The extent of seawater intrusion is dominated by the sum of freshwater discharge and tide‐induced efflux