基于过程的热带气旋和飓风对沿海含水层地表水-地下水相互作用和污染物迁移的影响

IF 2.6 Q3 ENVIRONMENTAL SCIENCES
Mijanur Mondal , Abhijit Mukherjee , Pankaj Kumar , Nagham Mahmoud Ismaeel , Kousik Das
{"title":"基于过程的热带气旋和飓风对沿海含水层地表水-地下水相互作用和污染物迁移的影响","authors":"Mijanur Mondal ,&nbsp;Abhijit Mukherjee ,&nbsp;Pankaj Kumar ,&nbsp;Nagham Mahmoud Ismaeel ,&nbsp;Kousik Das","doi":"10.1016/j.pdisas.2024.100318","DOIUrl":null,"url":null,"abstract":"<div><p>Coastal aquifers are hydraulically connected to the sea and a storm (cyclone/hurricane) can disrupt the surface water-groundwater (SW-GW) interaction process which is largely unexplored. Thus, this study aims to explore the impact of storm surges (both positive and negative) on coastal aquifers, focusing on pollutant mobilization, groundwater level (GWL) fluctuations, and solute concentration (Salinity, Cl<sup>-</sup>) and subsequent re-stabilization based on pre-existing studies from the coast of USA and India through a systematic review process. The outcome of this study revealed that there is a positive relationship between cyclonic speed, rainfall, storm surge height and GWL in lithologically conductive aquifers. Positive surge raises GWL, salinity and transportation of surface contaminants into groundwater while negative surge induces fall in salinity, and accelerates submarine groundwater discharge and exports contaminants/nutrients to sea. The restabilization of SW-GW interaction dynamics is case dependent, which takes a week to month to years, and is dependent on local hydrogeology and intensity of storm. So, the study recommends prioritizing to safeguard the coastal groundwater otherwise increasing storms will lead to questions on freshwater sustainability and coastal ecosystems in present climate change scenario.</p></div>","PeriodicalId":52341,"journal":{"name":"Progress in Disaster Science","volume":"22 ","pages":"Article 100318"},"PeriodicalIF":2.6000,"publicationDate":"2024-02-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2590061724000085/pdfft?md5=3d09b521472d792653d42408c785fe51&pid=1-s2.0-S2590061724000085-main.pdf","citationCount":"0","resultStr":"{\"title\":\"A process-based impact of tropical cyclone and hurricane on surface water-groundwater interaction and contaminant mobilization of coastal aquifers\",\"authors\":\"Mijanur Mondal ,&nbsp;Abhijit Mukherjee ,&nbsp;Pankaj Kumar ,&nbsp;Nagham Mahmoud Ismaeel ,&nbsp;Kousik Das\",\"doi\":\"10.1016/j.pdisas.2024.100318\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Coastal aquifers are hydraulically connected to the sea and a storm (cyclone/hurricane) can disrupt the surface water-groundwater (SW-GW) interaction process which is largely unexplored. Thus, this study aims to explore the impact of storm surges (both positive and negative) on coastal aquifers, focusing on pollutant mobilization, groundwater level (GWL) fluctuations, and solute concentration (Salinity, Cl<sup>-</sup>) and subsequent re-stabilization based on pre-existing studies from the coast of USA and India through a systematic review process. The outcome of this study revealed that there is a positive relationship between cyclonic speed, rainfall, storm surge height and GWL in lithologically conductive aquifers. Positive surge raises GWL, salinity and transportation of surface contaminants into groundwater while negative surge induces fall in salinity, and accelerates submarine groundwater discharge and exports contaminants/nutrients to sea. The restabilization of SW-GW interaction dynamics is case dependent, which takes a week to month to years, and is dependent on local hydrogeology and intensity of storm. So, the study recommends prioritizing to safeguard the coastal groundwater otherwise increasing storms will lead to questions on freshwater sustainability and coastal ecosystems in present climate change scenario.</p></div>\",\"PeriodicalId\":52341,\"journal\":{\"name\":\"Progress in Disaster Science\",\"volume\":\"22 \",\"pages\":\"Article 100318\"},\"PeriodicalIF\":2.6000,\"publicationDate\":\"2024-02-29\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://www.sciencedirect.com/science/article/pii/S2590061724000085/pdfft?md5=3d09b521472d792653d42408c785fe51&pid=1-s2.0-S2590061724000085-main.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Progress in Disaster Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S2590061724000085\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Progress in Disaster Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2590061724000085","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0

摘要

沿海含水层在水力上与海洋相连,风暴(气旋/飓风)会破坏地表水-地下水(SW-GW)的相互作用过程,而这一过程在很大程度上尚未被探索。因此,本研究旨在探讨风暴潮(正面和负面)对沿海含水层的影响,重点是污染物迁移、地下水位(GWL)波动、溶质浓度(盐度、Cl-)以及随后的重新稳定。研究结果表明,在岩性传导含水层中,气旋速度、降雨量、风暴潮高度和 GWL 之间存在正相关关系。正浪涌会提高 GWL、盐度并将地表污染物带入地下水,而负浪涌则会导致盐度下降,加速海底地下水排放并将污染物/营养物质排入大海。西南-地下水相互作用动态的恢复取决于具体情况,需要一周、一个月到数年的时间,并取决于当地的水文地质和风暴强度。因此,研究建议优先保护沿海地下水,否则,在当前气候变化的情况下,风暴的增加将导致淡水可持续性和沿海生态系统的问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A process-based impact of tropical cyclone and hurricane on surface water-groundwater interaction and contaminant mobilization of coastal aquifers

Coastal aquifers are hydraulically connected to the sea and a storm (cyclone/hurricane) can disrupt the surface water-groundwater (SW-GW) interaction process which is largely unexplored. Thus, this study aims to explore the impact of storm surges (both positive and negative) on coastal aquifers, focusing on pollutant mobilization, groundwater level (GWL) fluctuations, and solute concentration (Salinity, Cl-) and subsequent re-stabilization based on pre-existing studies from the coast of USA and India through a systematic review process. The outcome of this study revealed that there is a positive relationship between cyclonic speed, rainfall, storm surge height and GWL in lithologically conductive aquifers. Positive surge raises GWL, salinity and transportation of surface contaminants into groundwater while negative surge induces fall in salinity, and accelerates submarine groundwater discharge and exports contaminants/nutrients to sea. The restabilization of SW-GW interaction dynamics is case dependent, which takes a week to month to years, and is dependent on local hydrogeology and intensity of storm. So, the study recommends prioritizing to safeguard the coastal groundwater otherwise increasing storms will lead to questions on freshwater sustainability and coastal ecosystems in present climate change scenario.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Progress in Disaster Science
Progress in Disaster Science Social Sciences-Safety Research
CiteScore
14.60
自引率
3.20%
发文量
51
审稿时长
12 weeks
期刊介绍: Progress in Disaster Science is a Gold Open Access journal focusing on integrating research and policy in disaster research, and publishes original research papers and invited viewpoint articles on disaster risk reduction; response; emergency management and recovery. A key part of the Journal's Publication output will see key experts invited to assess and comment on the current trends in disaster research, as well as highlight key papers.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信