Abstract

This paper presents the modeling of tide–induced groundwater response using the spacetime collocation approach (SCA). The newly developed SCA begins with the consideration of Trefftz basis functions which are general solutions of the governing equation deriving from the separation of variables. The solution of the groundwater response in a coastal confined aquifer with an estuary boundary where the phase and amplitude of tide can vary with time and position is then approximated by the linear combination of Trefftz basis functions using the superposition theorem. The SCA is validated for several numerical examples with analytical solutions. The comparison of the results and accuracy for the SCA with the time–marching finite difference method is carried out. In addition, the SCA is adopted to examine the tidal and groundwater piezometer data at the Xing–Da port, Kaohsiung, Taiwan. The results demonstrate the SCA may obtain highly accurate results. Moreover, it shows the advantages of the SCA such that we only discretize by a set of points on the spacetime boundary without tedious mesh generation and thus significantly enhance the applicability.

Highlights

  • In coastal areas, tidal dynamics cause periodic fluctuation of the groundwater response in coastal aquifers

  • Finding out the interaction between the tidal dynamics as well as the groundwater level may be useful for investigating coastal hydrogeology in large scale which is of importance to solve various coastal hydrogeological problems, such as deterioration of the marine environment, seawater intrusion, and the stability of coastal engineering structures with rapidly development in coastal areas [4,5]

  • We present a pioneering work for numerical solutions of tide–induced groundwater response in a coast aquifer using the spacetime meshfree method

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Summary

Introduction

Tidal dynamics cause periodic fluctuation of the groundwater response in coastal aquifers. Considerable research has been devoted to understanding the tide–induced groundwater level fluctuations in a coast aquifer [6,7,8]. Analytical studies have been found to be common for understanding tidal variation affecting groundwater level in coastal areas [9,10,11]. Sun (1997) solved an analytical solution of groundwater response to tidal–induced boundary conditions in an estuary [12]. Jiao and Tang (1999) studied the groundwater response that consisted of unconfined and confined aquifers with a semi-permeable layer [13]. Jiao and Tang (2001) further proposed an exact solution for the groundwater

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