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Response of Coastal Groundwater Table to Offshore Storms
引用本文:李凌 N.Cartwright P.Nielsen D.Lockington. Response of Coastal Groundwater Table to Offshore Storms[J]. 中国海洋工程, 2004, 18(3): 423-431
作者姓名:李凌 N.Cartwright P.Nielsen D.Lockington
作者单位:[1]SchoolofEngineering,TheUniversityofQueensland,St.luciaQLD4072,Australia [2]CollegeofWaterConservancyandHydropowerEngineering,HohaiUniversity,Nanjing210098,China
基金项目:ThisstudywaspartlyfundedbyCRCforSustainableTourism,AustralianResearchCouncilandanARCDiscovery(GrantDP0 3 46461 )
摘    要:Large groundwater table fluctuations were observed in a coastal aquifer during an offshore storm. The storm induced significant changes of the mean shoreline elevation, characterized by a pulse-like oscillation. This pulse propagated in the aquifer, resulting in the water table fluctuations. A general analytical solution is derived to quantify this new mechanism of water table fluctuation. The solution is applied to field observations and is found to be able to predict reasonably well the observed storm-induced water table fluctuations. Based on the analytical solution, the damping characteristics and phase shift of the oscillation as it propagates inland are examined.

关 键 词:海岸带 地下水 海平面 风暴潮

Response of Coastal Groundwater Table to Offshore Storms
L. Li a,b,N. Cartwright a,P. Nielsen a and D. Lockington a a School of Engineering,The University of Queensland,St. Lucia QLD,Australia b College of Water Conservancy and Hydropower Engineering,Hohai University,Nanjing ,China. Response of Coastal Groundwater Table to Offshore Storms[J]. China Ocean Engineering, 2004, 18(3): 423-431
Authors:L. Li a  b  N. Cartwright a  P. Nielsen a  D. Lockington a a School of Engineering  The University of Queensland  St. Lucia QLD  Australia b College of Water Conservancy  Hydropower Engineering  Hohai University  Nanjing   China
Affiliation:L. Li a,b,N. Cartwright a,P. Nielsen a and D. Lockington a a School of Engineering,The University of Queensland,St. Lucia QLD4072,Australia b College of Water Conservancy and Hydropower Engineering,Hohai University,Nanjing 210098,China
Abstract:Large groundwater table fluctuations were observed in a coastal aquifer during an offshore storm. The storm induced significant changes of the mean shoreline elevation, characterized by a pulse like oscillation. This pulse propagated in the aquifer, resulting in the water table fluctuations. A general analytical solution is derived to quantify this new mechanism of water table fluctuation. The solution is applied to field observations and is found to be able to predict reasonably well the observed storm induced water table fluctuations. Based on the analytical solution, the damping characteristics and phase shift of the oscillation as it propagates inland are examined.
Keywords:water table fluctuation  coastal aquifer  Boussinesq equation  wave effect
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