Author:
Chang Y.-C.,Jeng D.-S.,Yeh H.-D.
Abstract
Abstract. In this study, a new analytical solution for describing the tide-induced groundwater fluctuations in oceanic islands with finite length and different slopes of the beaches is developed. Unlike previous solutions, the present solution is not only applicable for a semi-infinite coastal aquifer, but also for an oceanic island with finite length and different sloping beaches. The solution can be used to investigate the effect of higher-order components and beach slopes on the water table fluctuations. The results demonstrate the effect of higher-order components increases with the shallow water parameter or amplitude parameter and the water table level increases as beach slopes decrease.
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
Reference13 articles.
1. Batu, V.: Aquifer hydraulics: a comprehensive guide to hydrogeologic data analysis, New York, John Wiley & Sons Inc., 1998.
2. Bruggeman, G. A.: Analytical solutions of geohydrological problems, Elsevier Science Ltd, 1999.
3. Dagan, G.: Second-order theory of shallow free-surface flow in porous media, Quart. J. Mech. Appl. Math., 20, 517–526, 1967.
4. Freeze, R. A. and Cherry, J. A.: Groundwater, New Jersey, Prentice-Hall, Inc., 1979.
5. Hu, L., Jiao, J. J., and Guo, H.: Analytical studies on transient groundwater flow induced by land reclamation, Water resources research, 44, W11427, https://doi.org/10.1029/2008WR006926.
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