Department of Geosciences, University of Rhode Island, Kingston, RI 02881, USA.
Department of Geosciences, University of Rhode Island, Kingston, RI 02881, USA.
Sci Total Environ. 2022 Aug 25;836:155641. doi: 10.1016/j.scitotenv.2022.155641. Epub 2022 May 2.
Saltwater intrusion (SWI) into coastal aquifers is a growing problem for the drinking water supply of coastal communities worldwide, including for the sustainability of coastal ecosystems depending on freshwater inflow. The interface between freshwater and seawater in coastal aquifers is highly dynamic and is sensitive to changes in the hydraulic gradient between the sea- and groundwater levels. Sea level rise, storm surges, and drought are natural drivers changing the hydrostatic equilibrium between fresh- and saltwater. Coastal aquifers are further stressed by groundwater over-pumping because of the increasing needs of coastal populations. A systematic literature review and analysis of the current state of understanding the SWI drivers is presented, focusing on recent (1980 to 2020) investigations in the contiguous United States (CONUS). Results confirm that SWI is an active research area in CONUS. The drivers of SWI are increasingly better understood and quantified; however, the need for increased monitoring is also recognized. Our study shows that the number of monitoring sites have not increased significantly over the review period. Additionally, geophysical, and geochemical investigation techniques and numerical modeling tools are not utilized to their full potential, and data on SWI is not readily available from some sources. We conclude that there is a need for more SWI monitoring networks and closer multi-disciplinary collaboration, particularly between practitioners in the field and emerging modeling technique experts. Though we focus primarily on CONUS, our insights may be of value to the broader SWI research community and coastal water quality managers around the globe.
海水入侵(SWI)是全球沿海社区饮用水供应面临的一个日益严重的问题,包括依赖淡水流入的沿海生态系统的可持续性。沿海含水层中淡水和海水之间的界面高度动态,对海、地下水之间水力梯度变化敏感。海平面上升、风暴潮和干旱是改变淡水和咸水之间流体静力平衡的自然驱动因素。由于沿海地区人口不断增加对地下水的过度抽取,沿海含水层进一步受到压力。本文对 SWI 驱动因素的现有理解进行了系统的文献回顾和分析,重点是美国毗邻区(CONUS)最近(1980 年至 2020 年)的调查结果。结果证实,SWI 是 CONUS 地区的一个活跃研究领域。SWI 的驱动因素越来越被理解和量化;然而,也认识到需要增加监测。我们的研究表明,在审查期间,监测点的数量没有显著增加。此外,地球物理和地球化学调查技术和数值建模工具没有被充分利用,一些来源也没有提供有关 SWI 的数据。我们得出结论,需要更多的 SWI 监测网络和更紧密的多学科合作,特别是在该领域的从业者和新兴建模技术专家之间。虽然我们主要关注 CONUS,但我们的见解可能对全球更广泛的 SWI 研究界和沿海水质管理者有价值。