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dc.contributor.authorTsai, Jui-Pinen_US
dc.contributor.authorChang, Liang-Chengen_US
dc.contributor.authorChang, Ping-Yuen_US
dc.contributor.authorLin, Yuan-Chienen_US
dc.contributor.authorChen, You-Chengen_US
dc.contributor.authorWu, Meng-Tingen_US
dc.contributor.authorYu, Hwa-Lungen_US
dc.date.accessioned2018-08-21T05:54:12Z-
dc.date.available2018-08-21T05:54:12Z-
dc.date.issued2017-06-01en_US
dc.identifier.issn0022-1694en_US
dc.identifier.urihttp://dx.doi.org/10.1016/j.jhydrol.2017.03.047en_US
dc.identifier.urihttp://hdl.handle.net/11536/145668-
dc.description.abstractThe delineation of groundwater recharge zones is crucial for the conservation of groundwater quality and quantity. To objectively estimate groundwater recharge zones, many field surveys are required that are costly in both time and money. To facilitate the assessment of recharge zones with high efficiency and low expense, this study proposes a 'fast-filter' approach based on empirical orthogonal function analysis and applies it in a synthetic case study and to Taiwan's Yilan Plain. In the synthetic case study, we demonstrate that the proposed method can effectively identify the recharge area by considering the head variations driven by rainfall recharge. For the case of Yilan Plain application, the field investigations (i.e., collected wellbore logs and electrical resistivity tomography [ERT] surveys) and a groundwater simulation model support the recharge zones estimated by the proposed method. The study results show that within the estimated recharge zone, all of the collected wellbore logs consist of coarse grains, and thick and continuous high resistivity zones were shown in the ERT profile images. Moreover, the groundwater model indicates that the recharge within the estimated recharge zone is 57.6% of the total recharge despite that the area of the estimated zone is only 26.8% of the study area. Therefore, the proposed method is shown to delineate recharge zones at low cost. (C) 2017 Elsevier B.V. All rights reserved.en_US
dc.language.isoen_USen_US
dc.subjectEmpirical orthogonal function analysisen_US
dc.subjectSpatiotemporal analysisen_US
dc.subjectHigh recharge areasen_US
dc.subjectAquifer typeen_US
dc.subjectElectrical resistivity tomographyen_US
dc.titleSpatial-temporal pattern recognition of groundwater head variations for recharge zone identificationen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.jhydrol.2017.03.047en_US
dc.identifier.journalJOURNAL OF HYDROLOGYen_US
dc.citation.volume549en_US
dc.citation.spage351en_US
dc.citation.epage362en_US
dc.contributor.department土木工程學系zh_TW
dc.contributor.departmentDepartment of Civil Engineeringen_US
dc.identifier.wosnumberWOS:000403855500028en_US
Appears in Collections:Articles