An Analytical Solution for Tidal Fluctuations in Heterogeneous Coastal Leaky Aquifer Systems

碩士 === 國立交通大學 === 環境工程系所 === 99 === The coastal leaky aquifer system includes an unconfined aquifer on the top, a confined aquifer at the bottom, and an aquitard in between. This aquifer system was usually assumed to be homogeneous and of an infinite extent in the horizontal direction. The aquifer...

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Main Authors: Li, Guo-Hao, 李國豪
Other Authors: Yeh, Hund-Der
Format: Others
Language:en_US
Published: 2011
Online Access:http://ndltd.ncl.edu.tw/handle/21850957642300260287
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spelling ndltd-TW-099NCTU55150262016-08-22T04:17:26Z http://ndltd.ncl.edu.tw/handle/21850957642300260287 An Analytical Solution for Tidal Fluctuations in Heterogeneous Coastal Leaky Aquifer Systems 考慮潮汐擾動在非均質沿海滲&;#63822;含水層系統之解析解 Li, Guo-Hao 李國豪 碩士 國立交通大學 環境工程系所 99 The coastal leaky aquifer system includes an unconfined aquifer on the top, a confined aquifer at the bottom, and an aquitard in between. This aquifer system was usually assumed to be homogeneous and of an infinite extent in the horizontal direction. The aquifer system may however be heterogeneous due to depositional and post depositional processes. This study considers that the aquitard and confined aquifer are heterogeneous and both formations are divided into several homogeneous regions. A one-dimensional analytical model is developed for describing the head fluctuation in such a heterogeneous leaky aquifer system. The water table of the upper unconfined aquifer is maintained constant. It is revealed that both the length increasing and location nearing coast line of the heterogeneous aquitard have significant decreasing on the amplitude and increasing phase shift of the head fluctuation in the confined aquifer. Besides, this study indicates a heterogeneous trending confined aquifer may probably cause a shorter tidal intrusion distance and lower head distribution in a coastal leaky aquifer system. Yeh, Hund-Der 葉弘德 2011 學位論文 ; thesis 30 en_US
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language en_US
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description 碩士 === 國立交通大學 === 環境工程系所 === 99 === The coastal leaky aquifer system includes an unconfined aquifer on the top, a confined aquifer at the bottom, and an aquitard in between. This aquifer system was usually assumed to be homogeneous and of an infinite extent in the horizontal direction. The aquifer system may however be heterogeneous due to depositional and post depositional processes. This study considers that the aquitard and confined aquifer are heterogeneous and both formations are divided into several homogeneous regions. A one-dimensional analytical model is developed for describing the head fluctuation in such a heterogeneous leaky aquifer system. The water table of the upper unconfined aquifer is maintained constant. It is revealed that both the length increasing and location nearing coast line of the heterogeneous aquitard have significant decreasing on the amplitude and increasing phase shift of the head fluctuation in the confined aquifer. Besides, this study indicates a heterogeneous trending confined aquifer may probably cause a shorter tidal intrusion distance and lower head distribution in a coastal leaky aquifer system.
author2 Yeh, Hund-Der
author_facet Yeh, Hund-Der
Li, Guo-Hao
李國豪
author Li, Guo-Hao
李國豪
spellingShingle Li, Guo-Hao
李國豪
An Analytical Solution for Tidal Fluctuations in Heterogeneous Coastal Leaky Aquifer Systems
author_sort Li, Guo-Hao
title An Analytical Solution for Tidal Fluctuations in Heterogeneous Coastal Leaky Aquifer Systems
title_short An Analytical Solution for Tidal Fluctuations in Heterogeneous Coastal Leaky Aquifer Systems
title_full An Analytical Solution for Tidal Fluctuations in Heterogeneous Coastal Leaky Aquifer Systems
title_fullStr An Analytical Solution for Tidal Fluctuations in Heterogeneous Coastal Leaky Aquifer Systems
title_full_unstemmed An Analytical Solution for Tidal Fluctuations in Heterogeneous Coastal Leaky Aquifer Systems
title_sort analytical solution for tidal fluctuations in heterogeneous coastal leaky aquifer systems
publishDate 2011
url http://ndltd.ncl.edu.tw/handle/21850957642300260287
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