Modeling the Spatial and Seasonal Variations of Groundwater Head in an Urbanized Area under Low Impact Development

Increasing impervious land cover has great impacts on groundwater regimes in urbanized areas. Low impact development (LID) is generally regarded as a sustainable solution for groundwater conservation. However, the effects of LID on the spatial-temporal distribution of groundwater are not yet fully u...

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Main Authors: Yu Zheng, Sidian Chen, Huapeng Qin, Jiu Jimmy Jiao
Format: Article
Language:English
Published: MDPI AG 2018-06-01
Series:Water
Subjects:
LID
Online Access:http://www.mdpi.com/2073-4441/10/6/803
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spelling doaj-12594dc4ebba44f8a7e2663bd4b6e8592020-11-25T00:06:26ZengMDPI AGWater2073-44412018-06-0110680310.3390/w10060803w10060803Modeling the Spatial and Seasonal Variations of Groundwater Head in an Urbanized Area under Low Impact DevelopmentYu Zheng0Sidian Chen1Huapeng Qin2Jiu Jimmy Jiao3Key Laboratory for Urban Habitat Environmental Science and Technology, School of Environment and Energy, Peking University Shenzhen Graduate School, Shenzhen 518055, ChinaKey Laboratory for Urban Habitat Environmental Science and Technology, School of Environment and Energy, Peking University Shenzhen Graduate School, Shenzhen 518055, ChinaKey Laboratory for Urban Habitat Environmental Science and Technology, School of Environment and Energy, Peking University Shenzhen Graduate School, Shenzhen 518055, ChinaDepartment of Earth Sciences, The University of Hong Kong, Hong Kong, ChinaIncreasing impervious land cover has great impacts on groundwater regimes in urbanized areas. Low impact development (LID) is generally regarded as a sustainable solution for groundwater conservation. However, the effects of LID on the spatial-temporal distribution of groundwater are not yet fully understood. In this case study, a coupled Storm Water Management Model (SWMM) and Finite Element Subsurface FLOW system (FEFLOW) model was used to simulate surface and groundwater flow in an urbanized area in Shenzhen, China. After verification, the model was used to analyze the spatial-seasonal variations of groundwater head and hydrological processes under different LID scenarios. The results indicate that if the runoff from 7.5% and 15% of impervious area is treated by LID facilities, the annual surface runoff decreases by 5% and 9%, respectively, and the spatial average groundwater head relative to sea level pressure increases by 0.9 m and 1.7 m in the study area, respectively. The rise in groundwater head generally decreases from the recharge zones to the discharge zones surrounded by the streams and coastal waters. However, the groundwater head change is determined not only by the location in the catchment, but also by the hydraulic conductivity of underlying aquifer and LID infiltration intensity. Moreover, LID significantly enhances groundwater recharge and aquifer storage in the wet seasons; in turn it increases aquifer release and groundwater discharge in the dry seasons. However, LID has the potential to increase the risk of groundwater flooding during wet seasons in areas with poor aquifer drainage capacity and shallow groundwater depth. The findings from this study provide the basis for further assessing the benefit and risk of LID infiltration for groundwater supplementation in the urbanized areas.http://www.mdpi.com/2073-4441/10/6/803LIDinfiltrationrechargehydrological balance
collection DOAJ
language English
format Article
sources DOAJ
author Yu Zheng
Sidian Chen
Huapeng Qin
Jiu Jimmy Jiao
spellingShingle Yu Zheng
Sidian Chen
Huapeng Qin
Jiu Jimmy Jiao
Modeling the Spatial and Seasonal Variations of Groundwater Head in an Urbanized Area under Low Impact Development
Water
LID
infiltration
recharge
hydrological balance
author_facet Yu Zheng
Sidian Chen
Huapeng Qin
Jiu Jimmy Jiao
author_sort Yu Zheng
title Modeling the Spatial and Seasonal Variations of Groundwater Head in an Urbanized Area under Low Impact Development
title_short Modeling the Spatial and Seasonal Variations of Groundwater Head in an Urbanized Area under Low Impact Development
title_full Modeling the Spatial and Seasonal Variations of Groundwater Head in an Urbanized Area under Low Impact Development
title_fullStr Modeling the Spatial and Seasonal Variations of Groundwater Head in an Urbanized Area under Low Impact Development
title_full_unstemmed Modeling the Spatial and Seasonal Variations of Groundwater Head in an Urbanized Area under Low Impact Development
title_sort modeling the spatial and seasonal variations of groundwater head in an urbanized area under low impact development
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2018-06-01
description Increasing impervious land cover has great impacts on groundwater regimes in urbanized areas. Low impact development (LID) is generally regarded as a sustainable solution for groundwater conservation. However, the effects of LID on the spatial-temporal distribution of groundwater are not yet fully understood. In this case study, a coupled Storm Water Management Model (SWMM) and Finite Element Subsurface FLOW system (FEFLOW) model was used to simulate surface and groundwater flow in an urbanized area in Shenzhen, China. After verification, the model was used to analyze the spatial-seasonal variations of groundwater head and hydrological processes under different LID scenarios. The results indicate that if the runoff from 7.5% and 15% of impervious area is treated by LID facilities, the annual surface runoff decreases by 5% and 9%, respectively, and the spatial average groundwater head relative to sea level pressure increases by 0.9 m and 1.7 m in the study area, respectively. The rise in groundwater head generally decreases from the recharge zones to the discharge zones surrounded by the streams and coastal waters. However, the groundwater head change is determined not only by the location in the catchment, but also by the hydraulic conductivity of underlying aquifer and LID infiltration intensity. Moreover, LID significantly enhances groundwater recharge and aquifer storage in the wet seasons; in turn it increases aquifer release and groundwater discharge in the dry seasons. However, LID has the potential to increase the risk of groundwater flooding during wet seasons in areas with poor aquifer drainage capacity and shallow groundwater depth. The findings from this study provide the basis for further assessing the benefit and risk of LID infiltration for groundwater supplementation in the urbanized areas.
topic LID
infiltration
recharge
hydrological balance
url http://www.mdpi.com/2073-4441/10/6/803
work_keys_str_mv AT yuzheng modelingthespatialandseasonalvariationsofgroundwaterheadinanurbanizedareaunderlowimpactdevelopment
AT sidianchen modelingthespatialandseasonalvariationsofgroundwaterheadinanurbanizedareaunderlowimpactdevelopment
AT huapengqin modelingthespatialandseasonalvariationsofgroundwaterheadinanurbanizedareaunderlowimpactdevelopment
AT jiujimmyjiao modelingthespatialandseasonalvariationsofgroundwaterheadinanurbanizedareaunderlowimpactdevelopment
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