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首页> 外文期刊>Journal of Hydrology >Assessment of the impact of sea-level rise on steady-state seawater intrusion in a layered coastal aquifer
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Assessment of the impact of sea-level rise on steady-state seawater intrusion in a layered coastal aquifer

机译:评估海平面上升对分层沿海含水层稳态海水侵入的影响

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摘要

Previous studies on the impact of sea-level rise (SLR) on seawater intrusion (SWI) are mostly based on the assumption of a homogeneous coastal aquifer. In this study, we extend those studies by investigating SLR-induced SWI in a layered coastal aquifer using the analytical method developed by Strack and Ausk (2015). We provide analytical solutions for steady-state SWI in confined and unconfined coastal aquifers, where both constant-head and constant-flux inland boundary conditions are considered. The analysis based on a three-layer aquifer indicates that in general aquifer stratification affects either or both the initial location and response distance of the interface toe. Specifically, for flux-controlled unconfined coastal systems, the toe response distance driven by SLR is a linear function of the hydraulic conductivity of the top layer and independent of hydraulic conductivities of lower layers. Using an equivalent homogeneous hydraulic conductivity (derived based on the initial interface toe location before SLR) would result in overestimation or underestimation of the toe response distance, depending on the hydraulic conductivities and thicknesses of the layers. For flux-controlled confined layered coastal systems, by contrast, SLR can not cause variation of the steady-state interface toe location, which is consistent with previous findings for homogeneous coastal aquifers. The interface toe location in head-controlled layered coastal systems is only a function of relative hydraulic conductivities between the layers. Moreover, the effect of the layer thickness on the interface toe location and response distance in the head controlled system exhibits a more complicated pattern than in the flux-controlled coastal system, as changing the layer thickness changes both the overall aquifer transmissivity and inland freshwater flux. The results obtained enhance the understanding of the impact of SLR on SWI, which could provide a first-order assessment tool for relevan
机译:对海平面上升的影响,先前的研究(SLR)对海水入侵(SWI)大多是基于均质含水层沿海的假设。在这项研究中,我们通过使用斯特拉克和Ausk(2015)开发的分析方法在分层沿海含水层调查单反诱导SWI扩展这些研究。我们提供承压和非承压沿海含水层,其中两个定水头和恒定流量内陆边界条件被认为是稳态SWI分析解决方案。基于三层含水层的分析表明,在一般的含水层分层会影响任一或接口脚趾的初始位置和响应距离两者。具体而言,磁通控制的无侧限沿海系统,由驱动SLR趾响应距离是顶层的水力传导率的独立较低层的渗透系数的线性函数和。使用等效均匀渗透系数(基于SLR之前的初始界面趾位置导出的)将导致脚趾响应距离的高估或低估,取决于渗透系数和层的厚度。对于磁通控制的密闭层状沿海系统,相比之下,SLR不能引起稳态接口脚趾的位置,这是与均相沿海蓄水层以前的研究结果是一致的变化。在头控制的层状沿海系统接口趾位置仅是层之间的相对渗透系数的函数。此外,在在头部控制系统的接口趾位置和响应距离层厚度的影响显示出了更复杂的图案比在磁通控制的沿海系统中,作为改变层厚度改变整体含水层的透射率和内陆淡水通量都。结果得到提高的单反对SWI影响的认识,这可能提供了relevan一阶评估工具

著录项

  • 来源
    《Journal of Hydrology》 |2018年第2018期|共12页
  • 作者单位

    Hohai Univ State Key Lab Hydrol Water Resources &

    Hydraul En Nanjing Jiangsu Peoples R China;

    Hohai Univ State Key Lab Hydrol Water Resources &

    Hydraul En Nanjing Jiangsu Peoples R China;

    Hohai Univ State Key Lab Hydrol Water Resources &

    Hydraul En Nanjing Jiangsu Peoples R China;

    Nanjing Univ Sch Earth Sci &

    Engn Dept Hydrosci Key Lab Surficial Geochem Minist Educ Nanjing Jiangsu Peoples R China;

    Hohai Univ State Key Lab Hydrol Water Resources &

    Hydraul En Nanjing Jiangsu Peoples R China;

    Georgia Inst Technol Sch Civil &

    Environm Engn Atlanta GA 30332 USA;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 水文科学(水界物理学);
  • 关键词

    Seawater intrusion; Sea-level rise; Layered aquifer; Analytical method;

    机译:海水侵入;海平面上升;分层含水层;分析方法;

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