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首页> 外文期刊>Environmental Geology >Mapping the threat of seawater intrusion in a regional coastal aquifer-aquitard system in the southeastern United States
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Mapping the threat of seawater intrusion in a regional coastal aquifer-aquitard system in the southeastern United States

机译:绘制美国东南部区域性沿海含水层-阿奎塔尔系统中海水入侵的威胁图

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摘要

The Upper Floridan aquifer (UFA) beneath the southeastern US Atlantic Coastal Plain and inner continental shelf is a major source of groundwater for coastal Georgia (GA) and South Carolina (SC), where it supplies over 50% of water requirements. Since pumping from the UFA first began at Savannah, GA in the late 1800s, a large (~50km radius) cone of depression has developed on the aquifer's potentiometric surface. Where a regional Miocene-age aquitard overlying the UFA is thin or absent within this cone, the opportunity exists for seawater to leak downward through the seabed and into the aquifer. Recently completed marine reflection seismic surveys on the Georgia-South Carolina coast identified 11 areas of concern (AOCs) where the UFA is susceptible to seawater intrusion. Results from this project, and from an AOC test-drilling program recently completed, are contributing to a large database of information and models being developed for the UFA by several agencies and academic institutions. The results will provide input necessary for managing groundwater resources and mitigating potential seawater intrusion on the Georgia-South Carolina coast.
机译:美国东南部大西洋沿海平原和内陆大陆架下方的上佛罗里达蓄水层(UFA)是佐治亚州沿海(GA)和南卡罗来纳州(SC)的主要地下水来源,那里的需水量超过50%。自1800年代后期开始从佐治亚州萨凡纳开始从UFA抽水以来,蓄水层的电位表面上已经形成了一个大的(约50 km半径)凹陷锥。如果在该圆锥体中上覆于UFA的区域中新世时代的阿基德很薄或不存在,那么海水就有机会通过海床向下泄漏并进入含水层。最近在佐治亚州-南卡罗来纳州海岸完成的海洋反射地震调查确定了UFA容易受到海水入侵的11个关注区域(AOC)。该项目的结果以及最近完成的AOC测试钻探计划的结果,正在为一些机构和学术机构为UFA开发的大型信息和模型数据库做出贡献。研究结果将为管理地下水资源和缓解乔治亚州-南卡罗来纳州海岸潜在的海水入侵提供必要的投入。

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