IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2010~)
Responses of submarine groundwater to silty-sand coast reclamation: A case study in south of Laizhou Bay, China
Liu, Sen1,2,3,4; Gao, Maosheng3,4,5; Tang, Zhonghua1; Hou, Guohua3,4,5; Guo, Fei6
2016-11-05
Source PublicationESTUARINE COASTAL AND SHELF SCIENCE
Volume181Issue:2016Pages:51-60
SubtypeArticle
AbstractCoastal reclamation can result in considerable changes in the quality and quantity of submarine groundwater at the land/sea interface. In this study, submarine groundwater monitoring wells and water samples were designed and implemented to get data of groundwater level, electrical conductivity, temperature, and hydrochemistry data to examine the responses of silty-sand submarine groundwater in different sedimentary strata to reclamation in south of Laizhou Bay. The submarine groundwater is mainly saline water and its salinity in the deep aquifer is higher than that of seawater and close to brine. It was formed in the Late Pleistocene and Holocene. Drilling core data indicates that there is a strati graphic boundary at a depth of 18.58 m, with Holocene strata above, and Late Pleistocene strata below, this level. Continuous electrical conductivity data indicates that the submarine groundwater properties are stratigraphically distributed in this study area. And there is an interface at a depth of 38 m. Above the 38 m depth, the water quantity of submarine ground-saline water is freshening. The major ions showed a tendency to change continually above 25 m, but the tended to stabilize below 25 m depth. Freshwater is the major recharge source in the upper section of the Holocene strata, between the surface and 8.00 m depth, and the hydrochemical type has changed from Cl-Na to Cl center dot HCO3-Na. In the lower section of Holocene strata (8.00-23.00 m) and upper section of late Late Pleistocene strata (23.00-38.00 m), groundwater is influenced by seawater and groundwater of upper aquifer. The freshwater, seawater, and groundwater recharge in the upper aquifer has no influence on the groundwater in the section below the late Late Pleistocene (between 38.00 and 49.15 m) and the early Late Pleistocene strata (between 49.15 and 75.00 m). The filling layer, added in the coastal reclamation project, is comprised of clayey silt and fine sand, and its high porosity means that it is suitable for water storage. After the reclamation, meteoric water was stored in the filling layer that became the stable recharge resource. The recharge resource and the filling layer can improve the properties of the confined aquifer to increase the groundwater level. They may also influence the groundwater quantity and the flow direction. The groundwater in the Holocene strata is clearly influenced by recharge and the previously saline water aquifers receive freshwater on an on-going basis, such that the water is now becoming fresh. (C) 2016 Elsevier Ltd. All rights reserved.
KeywordSubmarine Groundwater Reclamation Laizhou Bay Silty Coast Electrical Conductivity
WOS HeadingsScience & Technology ; Life Sciences & Biomedicine ; Physical Sciences
DOI10.1016/j.ecss.2016.08.012
WOS KeywordLAND RECLAMATION ; SHALLOW GROUNDWATER ; INTRUSION ; SHENZHEN ; AREA ; SALINIZATION ; EVOLUTION ; AQUIFER ; FLOW
Indexed BySCI
Language英语
WOS Research AreaMarine & Freshwater Biology ; Oceanography
WOS SubjectMarine & Freshwater Biology ; Oceanography
WOS IDWOS:000386406500005
Citation statistics
Cited Times:4[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/5659
Collection黄土与第四纪地质国家重点实验室(2010~)
Affiliation1.China Univ Geosci, Sch Environm Studies, 388 Lumo Rd, Wuhan 430074, Peoples R China
2.Chinese Acad Geol Sci, Beijing 100037, Peoples R China
3.Qingdao Inst Marine Geol, Fuzhounan Rd 62, Qingdao 266071, Shandong, Peoples R China
4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China
5.Minist Land & Resources, Key Lab Marine Hydrocarbon Resources & Environm G, Qingdao 266071, Peoples R China
6.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
Recommended Citation
GB/T 7714
Liu, Sen,Gao, Maosheng,Tang, Zhonghua,et al. Responses of submarine groundwater to silty-sand coast reclamation: A case study in south of Laizhou Bay, China[J]. ESTUARINE COASTAL AND SHELF SCIENCE,2016,181(2016):51-60.
APA Liu, Sen,Gao, Maosheng,Tang, Zhonghua,Hou, Guohua,&Guo, Fei.(2016).Responses of submarine groundwater to silty-sand coast reclamation: A case study in south of Laizhou Bay, China.ESTUARINE COASTAL AND SHELF SCIENCE,181(2016),51-60.
MLA Liu, Sen,et al."Responses of submarine groundwater to silty-sand coast reclamation: A case study in south of Laizhou Bay, China".ESTUARINE COASTAL AND SHELF SCIENCE 181.2016(2016):51-60.
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