Estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wells

The groundwater fluctuations due to tidal variations at an observation well in a coastal aquifer can be used to determine the tidal characteristics and aquifer parameters without conducting an aquifer test. In this study, a method, comprised of Jeng et al.'s solution (2005) and simulated anneal...

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Main Authors: Y.-J. Chen, G.-Y. Chen, H.-D. Yeh, D.-S. Jeng
Format: Article
Language:English
Published: Copernicus Publications 2011-05-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/15/1473/2011/hess-15-1473-2011.pdf
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spelling doaj-fc4e75abc27441239572c06bb3109e322020-11-25T00:04:39ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382011-05-011551473148210.5194/hess-15-1473-2011Estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wellsY.-J. ChenG.-Y. ChenH.-D. YehD.-S. JengThe groundwater fluctuations due to tidal variations at an observation well in a coastal aquifer can be used to determine the tidal characteristics and aquifer parameters without conducting an aquifer test. In this study, a method, comprised of Jeng et al.'s solution (2005) and simulated annealing (SA) algorithm, is developed to determine the coastal aquifer parameters (hydraulic diffusivity, beach slope, and aquifer thickness) as well as the tidal characteristics (bichromatic-tide amplitudes, bichromatic-tide wave frequencies, and tidal phase lag) from the analysis of the tide-induced well-water-level (WWL) data. The synthetic WWL data generated from Jeng et al.'s solution (2005) with assumed parameter values and field data obtained from Barrenjoey beach, Australia, are analyzed. The estimated parameter values obtained from analyzing synthetic WWL data by the present method show good agreements with the previously assumed parameter values. The parameter estimation procedure may however fail in the case of a large shallow water parameter which in fact violates the constraint on the use of Jeng et al.'s solution (2005). In the analysis of field WWL data, the results indicate that the aquifer parameters estimated from the present method with single or multiple well data are significantly different from those given in Nielsen (1990). Inspecting the observed WWL data and the WWL data predicted from Jeng et al.'s solution (2005) reveals that the present method may provide better estimations for the aquifer parameters than those given in Nielsen (1990).http://www.hydrol-earth-syst-sci.net/15/1473/2011/hess-15-1473-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Y.-J. Chen
G.-Y. Chen
H.-D. Yeh
D.-S. Jeng
spellingShingle Y.-J. Chen
G.-Y. Chen
H.-D. Yeh
D.-S. Jeng
Estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wells
Hydrology and Earth System Sciences
author_facet Y.-J. Chen
G.-Y. Chen
H.-D. Yeh
D.-S. Jeng
author_sort Y.-J. Chen
title Estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wells
title_short Estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wells
title_full Estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wells
title_fullStr Estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wells
title_full_unstemmed Estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wells
title_sort estimations of tidal characteristics and aquifer parameters via tide-induced head changes in coastal observation wells
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2011-05-01
description The groundwater fluctuations due to tidal variations at an observation well in a coastal aquifer can be used to determine the tidal characteristics and aquifer parameters without conducting an aquifer test. In this study, a method, comprised of Jeng et al.'s solution (2005) and simulated annealing (SA) algorithm, is developed to determine the coastal aquifer parameters (hydraulic diffusivity, beach slope, and aquifer thickness) as well as the tidal characteristics (bichromatic-tide amplitudes, bichromatic-tide wave frequencies, and tidal phase lag) from the analysis of the tide-induced well-water-level (WWL) data. The synthetic WWL data generated from Jeng et al.'s solution (2005) with assumed parameter values and field data obtained from Barrenjoey beach, Australia, are analyzed. The estimated parameter values obtained from analyzing synthetic WWL data by the present method show good agreements with the previously assumed parameter values. The parameter estimation procedure may however fail in the case of a large shallow water parameter which in fact violates the constraint on the use of Jeng et al.'s solution (2005). In the analysis of field WWL data, the results indicate that the aquifer parameters estimated from the present method with single or multiple well data are significantly different from those given in Nielsen (1990). Inspecting the observed WWL data and the WWL data predicted from Jeng et al.'s solution (2005) reveals that the present method may provide better estimations for the aquifer parameters than those given in Nielsen (1990).
url http://www.hydrol-earth-syst-sci.net/15/1473/2011/hess-15-1473-2011.pdf
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