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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Main Authors: Hong Niu, Xing Liang, Sheng-nan Ni, Zhang Wen
Format: Article
Language:English
Published: Hindawi Limited 2015-01-01
Series:Mathematical Problems in Engineering
Online Access:http://dx.doi.org/10.1155/2015/284181
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spelling 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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