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Groundwater oxygen anomaly related to the 2016 Kumamoto earthquake in Southwest Japan

Cited 3 time in wos
Cited 3 time in scopus

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dc.contributor.authorSANO, Yuji-
dc.contributor.authorONDA, Satoki-
dc.contributor.authorKAGOSHIMA, Takanori-
dc.contributor.authorMIYAJIMA, Toshihiro-
dc.contributor.authorTAKAHATA, Naoto-
dc.contributor.authorSHIBATA, Tomo-
dc.contributor.authorNAKAGAWA, Chika-
dc.contributor.authorONOUE, Tetsuji-
dc.contributor.authorKim, Nak Kyu-
dc.contributor.authorLEE, Hyunwoo-
dc.contributor.authorKUSAKABE, Minoru-
dc.contributor.authorPINTI, Daniele L.-
dc.date.accessioned2021-05-10T00:53:59Z-
dc.date.available2021-05-10T00:53:59Z-
dc.date.issued2020-07-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/11881-
dc.description.abstractHere, we report the groundwater oxygen isotope anomalies caused by the 2016 Kumamoto earthquake (M_JMA 7.3) that occurred in Southwest Japan on April 16, 2016. One hundred and seventeen groundwater samples were collected from a deep well located 3 km to the southeast of the epicenter in Mifune Town, Kumamoto Prefecture; they were drinking water packed in PET bottles and distributed in the area between April 2015 and March 2018. Further, the oxygen and hydrogen isotopes were evaluated via cavity ring-down spectroscopy without performing any pretreatment. An anomalous increase was observed with respect to the δ18O value (up to 0.51‰) soon after the earthquake along with a precursory increase of 0.38‰ in January 2016 before the earthquake. During these periods, there was no noticeable change in the hydrogen isotopic ratios. Rapid crustal deformation related to the earthquake may have enhanced the microfracturing of the aquifer rocks and the production of new surfaces, inducing δ18O enrichment via oxygen isotopic exchange between rock and porewater without changing δ2H.en_US
dc.languageEnglishen_US
dc.language.isoen_USen_US
dc.subjectScience & Technologyen_US
dc.subject.classification기타()en_US
dc.titleGroundwater oxygen anomaly related to the 2016 Kumamoto earthquake in Southwest Japanen_US
dc.title.alternative일본 남서 쿠마모토에서 2016년에 발생한 지진으로 인한 지하수의 산소동위원소 이상 연구en_US
dc.typeArticleen_US
dc.identifier.bibliographicCitationSANO, Yuji, et al. 2020. "Groundwater oxygen anomaly related to the 2016 Kumamoto earthquake in Southwest Japan". <em>PROCEEDINGS OF THE JAPAN ACADEMY SERIES B-PHYSICAL AND BIOLOGICAL SCIENCES</em>, 96(7): 322-334.-
dc.citation.titlePROCEEDINGS OF THE JAPAN ACADEMY SERIES B-PHYSICAL AND BIOLOGICAL SCIENCESen_US
dc.citation.volume96en_US
dc.citation.number7en_US
dc.identifier.doi10.2183/pjab.96.024-
dc.citation.startPage322en_US
dc.citation.endPage334en_US
dc.description.articleClassificationSCI-
dc.description.jcrRateJCR 2018:47.826en_US
dc.subject.keywordgroundwateren_US
dc.subject.keywordearthquake precursorsen_US
dc.subject.keywordhydrogen isotopesen_US
dc.subject.keywordoxygen isotopesen_US
dc.subject.keyword2016 Kumamoto earthquakeen_US
dc.identifier.localId2020-0114-
dc.identifier.scopusid2-s2.0-85089616290-
dc.identifier.wosid000562159600007-
Appears in Collections  
2020-2020, Antarctic geology and meteorite research based on the Jangbogo station: Crustal evolution of Victoria Land and characteristics of asteroidal materials (20-20) / Lee, Mi Jung (PE20200)
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