{"title":"Mechanical Coupling Effect on Tide-Induced Fluctuations in a Multilayer Aquifer System","authors":"Julián E. Cuello, Luis Guarracino","doi":"10.1002/hyp.15303","DOIUrl":null,"url":null,"abstract":"<div>\n \n <p>We present a new analytical solution to study the mechanical coupling on tidal-induced head fluctuations in a coastal aquifer system. The conceptual model consists of two overlying confined units that extend infinitely under the sea. The proposed model assumes that the tidal fluctuations in the overlying aquifer are described by the classical equation derived by van der Kamp. For the underlying aquifer, a closed form analytical expression is derived by solving a boundary value problem that considers the loading effect produced by the overlying unit. The amplitude and phase lag of the underlying aquifer depend on both the specific storage and the thickness of the overlying unit. A parametric study shows that the mechanical coupling effect can be important for both large values of specific storage and thickness of the overlying aquifer.</p>\n </div>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"38 10","pages":""},"PeriodicalIF":3.2000,"publicationDate":"2024-10-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Hydrological Processes","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/hyp.15303","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"Environmental Science","Score":null,"Total":0}
引用次数: 0
Abstract
We present a new analytical solution to study the mechanical coupling on tidal-induced head fluctuations in a coastal aquifer system. The conceptual model consists of two overlying confined units that extend infinitely under the sea. The proposed model assumes that the tidal fluctuations in the overlying aquifer are described by the classical equation derived by van der Kamp. For the underlying aquifer, a closed form analytical expression is derived by solving a boundary value problem that considers the loading effect produced by the overlying unit. The amplitude and phase lag of the underlying aquifer depend on both the specific storage and the thickness of the overlying unit. A parametric study shows that the mechanical coupling effect can be important for both large values of specific storage and thickness of the overlying aquifer.
我们提出了一种新的分析方案,用于研究沿海含水层系统中潮汐引起的水头波动的力学耦合。概念模型由两个无限向海底延伸的上覆承压单元组成。提出的模型假定上覆含水层中的潮汐波动由 van der Kamp 推导的经典方程描述。对于上覆含水层,通过求解一个考虑了上覆单元产生的负荷效应的边界值问题,可以得到一个封闭形式的分析表达式。下伏含水层的振幅和相位滞后取决于上覆单元的比储量和厚度。参数研究表明,机械耦合效应在上覆含水层的比储量和厚度达到较大值时都很重要。
期刊介绍:
Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.