Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan

This study investigated the hydraulic properties of the heterogeneous aquifers of an artificial island (Yunlin Offshore Industrial Park) in Taiwan. The research was based on the groundwater level response affected by tidal fluctuation using the hydraulic tomography (HT) to analyze the hydraulic diff...

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Main Authors: Jet-Chau Wen, Hong-Ru Lin, Tian-Chyi Jim Yeh, Yu-Li Wang, Keng-Li Lin, Shao-Yang Huang
Format: Article
Language:English
Published: Wiley 2018-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2018/6046258
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author Jet-Chau Wen
Hong-Ru Lin
Tian-Chyi Jim Yeh
Yu-Li Wang
Keng-Li Lin
Shao-Yang Huang
author_facet Jet-Chau Wen
Hong-Ru Lin
Tian-Chyi Jim Yeh
Yu-Li Wang
Keng-Li Lin
Shao-Yang Huang
author_sort Jet-Chau Wen
collection DOAJ
description This study investigated the hydraulic properties of the heterogeneous aquifers of an artificial island (Yunlin Offshore Industrial Park) in Taiwan. The research was based on the groundwater level response affected by tidal fluctuation using the hydraulic tomography (HT) to analyze the hydraulic diffusivity (α). Specifically, the power spectrum ratio of groundwater and tidal fluctuations derived from the Gelhar solution was used to estimate α in homogeneous aquifers; this, however, could not be applied in the artificial island. Next, the spatial distribution of the groundwater level response affected by tidal fluctuation was analyzed and found to be irregular, proving the existence of hydrogeological heterogeneity in the artificial island. Furthermore, the results of the estimated α using the HT showed low error and high correlation, 0.41 m2/hr and 0.83, respectively, between the optimal estimated heterogeneous and reference α fields in the synthetic aquifer. Last, the HT was used in the real tested scenario. By comparing the predicted groundwater levels of the optimal estimated heterogeneous α field and the observed groundwater levels of the real aquifer, it was found that the correlation was higher than 0.99. Therefore, the HT can be used to obtain the optimal estimated heterogeneous α field in the artificial island.
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institution Kabale University
issn 1468-8115
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language English
publishDate 2018-01-01
publisher Wiley
record_format Article
series Geofluids
spelling doaj-art-1a848857c9a046b3b51e32b00d313d4b2025-02-03T01:28:56ZengWileyGeofluids1468-81151468-81232018-01-01201810.1155/2018/60462586046258Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in TaiwanJet-Chau Wen0Hong-Ru Lin1Tian-Chyi Jim Yeh2Yu-Li Wang3Keng-Li Lin4Shao-Yang Huang5Department of Safety, Health and Environmental Engineering, National Yunlin University of Science and Technology, Douliou, Yunlin, TaiwanDoctoral Program, Graduate School of Engineering Science and Technology, National Yunlin University of Science and Technology, Douliou, Yunlin, TaiwanDepartment of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ, USADepartment of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ, USADepartment of Environment, AECOM Taiwan Corporation, Kaohsiung, TaiwanResearch Center for Soil and Water Resources and Natural Disaster Prevention, National Yunlin University of Science and Technology, Douliou, Yunlin, TaiwanThis study investigated the hydraulic properties of the heterogeneous aquifers of an artificial island (Yunlin Offshore Industrial Park) in Taiwan. The research was based on the groundwater level response affected by tidal fluctuation using the hydraulic tomography (HT) to analyze the hydraulic diffusivity (α). Specifically, the power spectrum ratio of groundwater and tidal fluctuations derived from the Gelhar solution was used to estimate α in homogeneous aquifers; this, however, could not be applied in the artificial island. Next, the spatial distribution of the groundwater level response affected by tidal fluctuation was analyzed and found to be irregular, proving the existence of hydrogeological heterogeneity in the artificial island. Furthermore, the results of the estimated α using the HT showed low error and high correlation, 0.41 m2/hr and 0.83, respectively, between the optimal estimated heterogeneous and reference α fields in the synthetic aquifer. Last, the HT was used in the real tested scenario. By comparing the predicted groundwater levels of the optimal estimated heterogeneous α field and the observed groundwater levels of the real aquifer, it was found that the correlation was higher than 0.99. Therefore, the HT can be used to obtain the optimal estimated heterogeneous α field in the artificial island.http://dx.doi.org/10.1155/2018/6046258
spellingShingle Jet-Chau Wen
Hong-Ru Lin
Tian-Chyi Jim Yeh
Yu-Li Wang
Keng-Li Lin
Shao-Yang Huang
Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan
Geofluids
title Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan
title_full Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan
title_fullStr Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan
title_full_unstemmed Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan
title_short Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan
title_sort hydraulic tomography for estimating the diffusivity of heterogeneous aquifers based on groundwater response to tidal fluctuation in an artificial island in taiwan
url http://dx.doi.org/10.1155/2018/6046258
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