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Article: Modeling the influences of land reclamation on groundwater systems: A case study in Shekou peninsula, Shenzhen, China

TitleModeling the influences of land reclamation on groundwater systems: A case study in Shekou peninsula, Shenzhen, China
Authors
KeywordsFEFLOW
Groundwater system
Land reclamation
Shenzhen
Submarine groundwater discharge
Issue Date2010
PublisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/enggeo
Citation
Engineering Geology, 2010, v. 114 n. 3-4, p. 144-153 How to Cite?
AbstractLand has been reclaimed along the coastal areas in many parts of the world to meet the growing demand for houses and other land use. Over 15km2 of land has been reclaimed around the Shekou peninsula, Shenzhen, China. Land reclamation may have significant influences on groundwater systems but this problem has not been adequately studied. Using FEFLOW (Diersch, 2005), a three-dimensional finite element groundwater model, the response of the groundwater system on the impact of land reclamation in the Shekou peninsula from 1983 to 2007 was simulated. The model was calibrated against observed groundwater levels in three observation wells. The results showed that, after reclamation, there was a regional increase of groundwater level in the study area. The groundwater divide between western and eastern coastlines moved during different reclamation stages. The results also showed that, submarine groundwater discharge along the coastlines was increased due to the increase of recharge in the newly reclaimed land. The model predicts change of groundwater level between 2007 and 2025, which demonstrates that the response of the aquifer system to land reclamation is a long lasting process. There will be a further increase in groundwater level and it may take about 10years for the systems to reach a new equilibrium. It is suggested that the changes of the groundwater flow system due to large-scale land reclamation should be modeled before reclamation to investigate possible engineering and environmental consequences. © 2010.
Persistent Identifierhttp://hdl.handle.net/10722/129152
ISSN
2023 Impact Factor: 6.9
2023 SCImago Journal Rankings: 2.437
ISI Accession Number ID
Funding AgencyGrant Number
Research Grants Council project of the Hong Kong Special Administrative RegionHKU 7028/06P
Land and Resources Department, Shenzhen Government, China
Funding Information:

The study was partially supported by the Research Grants Council project of the Hong Kong Special Administrative Region (HKU 7028/06P) and the project of "Studies on seawater intrusion and countermeasures in Shenzhen" funded by the Land and Resources Department, Shenzhen Government, China. We give thanks for the constructive comments for three anonymous reviewers.

References
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DC FieldValueLanguage
dc.contributor.authorHu, Len_HK
dc.contributor.authorJiao, JJen_HK
dc.date.accessioned2010-12-23T08:33:09Z-
dc.date.available2010-12-23T08:33:09Z-
dc.date.issued2010en_HK
dc.identifier.citationEngineering Geology, 2010, v. 114 n. 3-4, p. 144-153en_HK
dc.identifier.issn0013-7952en_HK
dc.identifier.urihttp://hdl.handle.net/10722/129152-
dc.description.abstractLand has been reclaimed along the coastal areas in many parts of the world to meet the growing demand for houses and other land use. Over 15km2 of land has been reclaimed around the Shekou peninsula, Shenzhen, China. Land reclamation may have significant influences on groundwater systems but this problem has not been adequately studied. Using FEFLOW (Diersch, 2005), a three-dimensional finite element groundwater model, the response of the groundwater system on the impact of land reclamation in the Shekou peninsula from 1983 to 2007 was simulated. The model was calibrated against observed groundwater levels in three observation wells. The results showed that, after reclamation, there was a regional increase of groundwater level in the study area. The groundwater divide between western and eastern coastlines moved during different reclamation stages. The results also showed that, submarine groundwater discharge along the coastlines was increased due to the increase of recharge in the newly reclaimed land. The model predicts change of groundwater level between 2007 and 2025, which demonstrates that the response of the aquifer system to land reclamation is a long lasting process. There will be a further increase in groundwater level and it may take about 10years for the systems to reach a new equilibrium. It is suggested that the changes of the groundwater flow system due to large-scale land reclamation should be modeled before reclamation to investigate possible engineering and environmental consequences. © 2010.en_HK
dc.languageengen_US
dc.publisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/enggeoen_HK
dc.relation.ispartofEngineering Geologyen_HK
dc.subjectFEFLOWen_HK
dc.subjectGroundwater systemen_HK
dc.subjectLand reclamationen_HK
dc.subjectShenzhenen_HK
dc.subjectSubmarine groundwater dischargeen_HK
dc.titleModeling the influences of land reclamation on groundwater systems: A case study in Shekou peninsula, Shenzhen, Chinaen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0013-7952&volume=114&issue=3-4&spage=144&epage=153&date=2010&atitle=Modeling+the+influences+of+land+reclamation+on+groundwater+systems:+A+case+study+in+Shekou+peninsula,+Shenzhen,+China-
dc.identifier.emailJiao, JJ:jjiao@hku.hken_HK
dc.identifier.authorityJiao, JJ=rp00712en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1016/j.enggeo.2010.04.011en_HK
dc.identifier.scopuseid_2-s2.0-77955176293en_HK
dc.identifier.hkuros178636en_US
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-77955176293&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume114en_HK
dc.identifier.issue3-4en_HK
dc.identifier.spage144en_HK
dc.identifier.epage153en_HK
dc.identifier.isiWOS:000280884200005-
dc.publisher.placeNetherlandsen_HK
dc.relation.projectSubmarine groundwater discharge in Tolo Harbour and its possible ecological influence-
dc.identifier.scopusauthoridHu, L=14012430500en_HK
dc.identifier.scopusauthoridJiao, JJ=7102382963en_HK
dc.identifier.citeulike7110524-
dc.identifier.issnl0013-7952-

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