{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361137043573604608.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4154/gc.2018.09"}}],"dc:title":[{"@value":"Evaluations of the downward velocity of soil water movement in the unsaturated zone in a groundwater recharge area using δ18 O tracer: the Kumamoto region, southern Japan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Water and substances from the surface infiltrate the unsaturated zone before reaching groundwater. Yet, little study has been done on the unsaturated zone due to the difficulty of sampling. A lot of studies have been carried out on the top soil down to a depth of one metre and on shallow aquifers because they are easily accessible for sampling. The unsaturated zone of the Kumamotoregion recharge areas is important due to concerns about groundwater pollution from agriculture. The aim of this study was to estimate the downward velocity of soil water movement through the unsaturated zone and the recharge rate using δ18O as a tracer. Five sampling sites were selected and a core was taken from each site. The cores were cut into 0.1 m pieces and soil water was extracted from each to analyze for δD and the δ18O content. Average δD and δ18O compositions of soil water were similar to the isotopic compositions of summer precipitation. Annual average recharge rate and the downward velocity of soil water in each site were estimated by fitting a vertical δ18O profile pattern to a precipitation δ18O time series as a theoretical water displacement flow model for recharge. An estimated annual average recharge rate in the recharge area ranged from 745 to 1058 mm/yr with the annual average downward velocity of 1.37 to 2.34 m/yr. Based on the estimated downward velocity, the infiltration time for soilwater to reach the aquifer was determined as ranging from 9 to 24 years, which corresponds with previous groundwater age estimations presented in an earlier published study on the same area. It was assumed that contaminants will reach aquifers in 9 to 25 years if the effects of diffusion and microbiological reaction are not taken into account.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137043573604480","@type":"Researcher","foaf:name":[{"@value":"Azusa Okomura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043573604481","@type":"Researcher","foaf:name":[{"@value":"Takahiro Hosono"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043573604608","@type":"Researcher","foaf:name":[{"@value":"Dennis Boateng"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043573604609","@type":"Researcher","foaf:name":[{"@value":"Jun Shimada"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"1330030X"},{"@type":"EISSN","@value":"13334875"}],"prism:publicationName":[{"@value":"Geologia Croatica"}],"dc:publisher":[{"@value":"Croatian Geological Survey"}],"prism:publicationDate":"2018-06-20","prism:volume":"71","prism:number":"2","prism:startingPage":"65","prism:endingPage":"82"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","createdAt":"2018-07-02","modifiedAt":"2021-07-20","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=soil%20water;%20oxygen%20isotope;%20recharge%20rate;%20infiltration%20time","dc:title":"soil water; oxygen isotope; recharge rate; infiltration time"},{"@id":"https://cir.nii.ac.jp/all?q=QE1-996.5","dc:title":"QE1-996.5"},{"@id":"https://cir.nii.ac.jp/all?q=Geology","dc:title":"Geology"},{"@id":"https://cir.nii.ac.jp/all?q=soil%20water,%20oxygen%20isotope,%20recharge%20rate,%20infiltration%20time","dc:title":"soil water, oxygen isotope, recharge rate, infiltration time"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050850247217428224","@type":"Article","resourceType":"学術雑誌論文(journal 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hydrological modeling for detailed characterization of regional catchment water dynamics in Kumamoto area, southern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643802130176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrothermal and magmatic contributions to surface waters in the Aso caldera, southern Japan: Implications for weathering processes in volcanic areas"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567189387687424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recovery of Lost Nexus Synergy via Payment for Environmental Services in Kumamoto, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092855218048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Post-seismic hydrochemical changes in regional groundwater flow systems in 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earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131416930196224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Identification of changes in subsurface temperature and groundwater flow after the 2016 Kumamoto earthquake using long-term well temperature–depth profiles"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131416930201088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes of groundwater flow systems after the 2016 Mw 7.0 Kumamoto earthquake deduced by stable isotopic and CFC-12 compositions of natural springs"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417127743744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origins and pathways of deeply derived carbon and fluids observed in hot spring waters from non-active volcanic fields, 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