Analytical Study of Unsteady Nested Groundwater Flow Systems
Two analytical solutions using segregation variable method to calculate the hydraulic head under steady and unsteady flow conditions based on Tóth’s classical model were developed. The impacts of anisotropy ratio, hydraulic conductivity (K), and specific yield (μs) on the flow patterns were analyzed...
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Hindawi Limited
2015-01-01
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Series: | Mathematical Problems in Engineering |
Online Access: | http://dx.doi.org/10.1155/2015/284181 |
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doaj-3aedf67135204493b95ca3af930e73432020-11-24T23:30:20ZengHindawi LimitedMathematical Problems in Engineering1024-123X1563-51472015-01-01201510.1155/2015/284181284181Analytical Study of Unsteady Nested Groundwater Flow SystemsHong Niu0Xing Liang1Sheng-nan Ni2Zhang Wen3School of Environmental Studies, China University of Geosciences, Wuhan 430074, ChinaSchool of Environmental Studies, China University of Geosciences, Wuhan 430074, ChinaShanghai Astronomical Observatory, Chinese Academy of Sciences, Shanghai 200030, ChinaSchool of Environmental Studies, China University of Geosciences, Wuhan 430074, ChinaTwo analytical solutions using segregation variable method to calculate the hydraulic head under steady and unsteady flow conditions based on Tóth’s classical model were developed. The impacts of anisotropy ratio, hydraulic conductivity (K), and specific yield (μs) on the flow patterns were analyzed. It was found that the area of the equal velocity region increases and the penetrating depth of the flow system decreases at steady state with anisotropy ratio increases, which is defined as ε=Kx/Kz. In addition, stagnant zones can be found in the flow field where the streamlines have opposite directions. These stagnant zones move toward the surface as the horizontal hydraulic conductivity increases. The results of the study on transient flow indicate that a relative increase in hydraulic conductivity produces a positive impact on hydraulic head and a relative enhancement in specific yield produces a negative effect on hydraulic head at early times.http://dx.doi.org/10.1155/2015/284181 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Hong Niu Xing Liang Sheng-nan Ni Zhang Wen |
spellingShingle |
Hong Niu Xing Liang Sheng-nan Ni Zhang Wen Analytical Study of Unsteady Nested Groundwater Flow Systems Mathematical Problems in Engineering |
author_facet |
Hong Niu Xing Liang Sheng-nan Ni Zhang Wen |
author_sort |
Hong Niu |
title |
Analytical Study of Unsteady Nested Groundwater Flow Systems |
title_short |
Analytical Study of Unsteady Nested Groundwater Flow Systems |
title_full |
Analytical Study of Unsteady Nested Groundwater Flow Systems |
title_fullStr |
Analytical Study of Unsteady Nested Groundwater Flow Systems |
title_full_unstemmed |
Analytical Study of Unsteady Nested Groundwater Flow Systems |
title_sort |
analytical study of unsteady nested groundwater flow systems |
publisher |
Hindawi Limited |
series |
Mathematical Problems in Engineering |
issn |
1024-123X 1563-5147 |
publishDate |
2015-01-01 |
description |
Two analytical solutions using segregation variable method to calculate the hydraulic head under steady and unsteady flow conditions based on Tóth’s classical model were developed. The impacts of anisotropy ratio, hydraulic conductivity (K), and specific yield (μs) on the flow patterns were analyzed. It was found that the area of the equal velocity region increases and the penetrating depth of the flow system decreases at steady state with anisotropy ratio increases, which is defined as ε=Kx/Kz. In addition, stagnant zones can be found in the flow field where the streamlines have opposite directions. These stagnant zones move toward the surface as the horizontal hydraulic conductivity increases. The results of the study on transient flow indicate that a relative increase in hydraulic conductivity produces a positive impact on hydraulic head and a relative enhancement in specific yield produces a negative effect on hydraulic head at early times. |
url |
http://dx.doi.org/10.1155/2015/284181 |
work_keys_str_mv |
AT hongniu analyticalstudyofunsteadynestedgroundwaterflowsystems AT xingliang analyticalstudyofunsteadynestedgroundwaterflowsystems AT shengnanni analyticalstudyofunsteadynestedgroundwaterflowsystems AT zhangwen analyticalstudyofunsteadynestedgroundwaterflowsystems |
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1725541730893168640 |