{"@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/1361137043830719488.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.jog.2004.07.008"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0264370704000845?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0264370704000845?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"30008919656"}}],"dc:title":[{"@value":"A 100m laser strainmeter system installed in a 1km deep tunnel at Kamioka, Gifu, Japan"}],"description":[{"notation":[{"@value":"Abstract   We have installed a laser strainmeter system in a deep tunnel about 1,000 m below the ground surface at Kamioka, Gifu, Japan. The system consists of three types of independent interferometers: (1) an EW linear strainmeter of the Michelson type with unequal arms, (2) an NS-EW differential strainmeter of the Michelson type with equal arms and (3) a NS absolute strainmeter of the Fabry–Perot type. These are configured in L-shaped vacuum pipes, each of which has a length of 100 m. (1) and (2) are highly sensitive (order of 10−13 strain) and have wide dynamical range (10−13–10−6). Observations with strainmeters (1) and (2) started on June 11, 2003. (3) is a new device for absolute-length measurements of the order of 10−9 of a long-baseline (100 m) Fabry–Perot cavity by the use of phase-modulated light. This third strainmeter will be ready for operation before the end of 2004. The laser source of strainmeters (1) and (2) is a frequency-doubled YAG laser with a wavelength of 532 nm. The laser frequency is locked onto an iodine absorption line and a stability of 2 × 10−13 is attained. The light paths of the laser strainmeter system are enclosed in SUS304 stainless steel pipes. The inside pressure is kept to be 10−4 Pa. Consequently, quantitative measurement of crustal strains of the order of 10−13 can be attained by employing the laser strainmeter system of (1) and (2) at Kamioka. This resolving power corresponds to that of a superconducting gravimeter. Using the laser strainmeter system, we expect to determine parameters related to fluid core resonance, core modes and core undertone as well as other geodynamic signals such as slow strain changes caused by silent earthquakes or slow earthquakes."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137043830719616","@type":"Researcher","foaf:name":[{"@value":"Shuzo Takemoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719489","@type":"Researcher","foaf:name":[{"@value":"Akito Araya"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719495","@type":"Researcher","foaf:name":[{"@value":"Junpei Akamatsu"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719618","@type":"Researcher","foaf:name":[{"@value":"Wataru Morii"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719491","@type":"Researcher","foaf:name":[{"@value":"Hideo Momose"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719492","@type":"Researcher","foaf:name":[{"@value":"Masatake Ohashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719490","@type":"Researcher","foaf:name":[{"@value":"Ichiro Kawasaki"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719498","@type":"Researcher","foaf:name":[{"@value":"Toshihiro Higashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719499","@type":"Researcher","foaf:name":[{"@value":"Yoichi Fukuda"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719494","@type":"Researcher","foaf:name":[{"@value":"Shinji Miyoki"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719497","@type":"Researcher","foaf:name":[{"@value":"Takashi Uchiyama"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719488","@type":"Researcher","foaf:name":[{"@value":"Daisuke Tatsumi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719493","@type":"Researcher","foaf:name":[{"@value":"Hideo Hanada"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719619","@type":"Researcher","foaf:name":[{"@value":"Isao Naito"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719496","@type":"Researcher","foaf:name":[{"@value":"Souichi Telada"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719621","@type":"Researcher","foaf:name":[{"@value":"Nobuo Ichikawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719617","@type":"Researcher","foaf:name":[{"@value":"Kensuke Onoue"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137043830719620","@type":"Researcher","foaf:name":[{"@value":"Yasuo Wada"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02643707"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/02643707"}],"prism:publicationName":[{"@value":"Journal of Geodynamics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2004-10","prism:volume":"38","prism:number":"3-5","prism:startingPage":"477","prism:endingPage":"488"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0264370704000845?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0264370704000845?httpAccept=text/plain"}],"createdAt":"2004-11-12","modifiedAt":"2021-06-28","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845760782063360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Design and operation of a 1500-m laser strainmeter installed at an underground site in Kamioka, Japan"},{"@value":"Design and Operation of a 1500−M Laser Strainmeter Installed at an Underground Site in Kamioka, 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2006"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204067034368","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evaluation of Detection Level of Crustal Deformation Observation in the Time Domain Through Power Spectrum Analysis<br>—Investigation of a Long-Baseline Laser Extensometer—"},{"@language":"ja","@value":"パワースペクトルを介した時間領域における地殻変動データの検出能力評価"},{"@value":"Evaluation of detection level of crustal deformation observation in the time domain through power spectrum analysis: investigation of a long-baseline laser extensometer"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204612610816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Experimental Demonstration of Cryogenic Mirror Technique  -Achievements of CLIO-"},{"@language":"ja","@value":"低温鏡の実証　　‐　Ｃｒｙｏｇｅｎｉｃ　Ｌａｓｅｒ　Ｉｎｔｅｒｆｅｒｏｍｅｔｅｒ　Ｏｂｓｅｒｖａｔｏｒｙ（ＣＬＩＯ）の成果　‐"},{"@value":"低温鏡の実証--Cryogenic Laser 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