{"@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/1361131421285556992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1155/2019/3983864"}},{"identifier":{"@type":"URI","@value":"http://downloads.hindawi.com/journals/geofluids/2019/3983864.pdf"}},{"identifier":{"@type":"URI","@value":"http://downloads.hindawi.com/journals/geofluids/2019/3983864.xml"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Heat and Helium-3 Fluxes from Teide Volcano, Canary Islands, Spain"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>During July 2016, the first integrated heat flow, CO<jats:sub>2</jats:sub>, and <jats:sup>3</jats:sup>He emission survey was conducted across 0.5 km<jats:sup>2</jats:sup> of the summit cone and crater of Teide volcano, Tenerife, Canary Islands, Spain. The thermal energy released from Teide summit cone by diffuse degassing was 2.2 MW, and the heat flux calculated through Dawson’s method was 8.1 MW, difference due to the comparison of purely convective areas as the crater with diffusive areas as the flanks of the volcano. Diffuse CO<jats:sub>2</jats:sub> output was <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M1\"><mml:mn>211</mml:mn><mml:mo>±</mml:mo><mml:mn>20</mml:mn></mml:math> t d<jats:sup>-1</jats:sup>, and <jats:sup>3</jats:sup>He emission was estimated to be within a range between 0.35 and 0.89 mol y<jats:sup>-1</jats:sup>. The obtained values of diffuse degassing and heat fluxes are close to others obtained for similar volcanic areas. The calculation of <jats:sup>3</jats:sup>He/heat ratio for the first time in this volcanic system supports the presence of an important mantle source for the degassing of Teide volcano.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381131421285556864","@type":"Researcher","foaf:name":[{"@value":"Mar Alonso"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"},{"@value":"Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285556865","@type":"Researcher","foaf:name":[{"@value":"Eleazar Padrón"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"},{"@value":"Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"},{"@value":"Agencia Insular de la Energía de Tenerife (AIET), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285556995","@type":"Researcher","foaf:name":[{"@value":"Hirochika Sumino"}],"jpcoar:affiliationName":[{"@value":"Department of Basic Science, Graduate School of Arts and Sciences, The University of Tokyo, 3-8-1 Komaba, Meguro-ku, Tokyo 153-0041, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285557121","@type":"Researcher","foaf:name":[{"@value":"Pedro A. Hernández"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"},{"@value":"Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"},{"@value":"Agencia Insular de la Energía de Tenerife (AIET), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285556994","@type":"Researcher","foaf:name":[{"@value":"Gladys V. Melián"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"},{"@value":"Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"},{"@value":"Agencia Insular de la Energía de Tenerife (AIET), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285556993","@type":"Researcher","foaf:name":[{"@value":"María Asensio-Ramos"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285556866","@type":"Researcher","foaf:name":[{"@value":"Fátima Rodríguez"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285556996","@type":"Researcher","foaf:name":[{"@value":"Germán Padilla"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"},{"@value":"Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285557120","@type":"Researcher","foaf:name":[{"@value":"Marta García-Merino"}],"jpcoar:affiliationName":[{"@value":"Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285556997","@type":"Researcher","foaf:name":[{"@value":"Cecilia Amonte"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1381131421285556992","@type":"Researcher","foaf:name":[{"@value":"Nemesio M. Pérez"}],"jpcoar:affiliationName":[{"@value":"Instituto Volcanológico de Canarias (INVOLCAN), 38320, San Cristóbal de La Laguna, Tenerife, Canary Islands, Spain"},{"@value":"Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"},{"@value":"Agencia Insular de la Energía de Tenerife (AIET), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"14688115"},{"@type":"EISSN","@value":"14688123"}],"prism:publicationName":[{"@value":"Geofluids"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2019-06-23","prism:volume":"2019","prism:startingPage":"1","prism:endingPage":"12"},"reviewed":"false","dc:rights":["http://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"http://downloads.hindawi.com/journals/geofluids/2019/3983864.pdf"},{"@id":"http://downloads.hindawi.com/journals/geofluids/2019/3983864.xml"}],"createdAt":"2019-06-23","modifiedAt":"2019-06-23","foaf:topic":[{"@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"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256971147136","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"18H04365"},{"@type":"JGN","@value":"JP18H04365"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PUBLICLY-18H04365/"}],"notation":[{"@language":"ja","@value":"高温高圧実験と超高感度希ガス分析から制約する地球内部始源的リザーバーの在処"},{"@language":"en","@value":"Constraints on Primordial Noble Gas Reservoir Deep in the Earth by High-pressure and High-temperature Experiments"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011143853601920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mid-Ocean Ridge Hydrothermal Fluxes and the Chemical Composition of the Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144715225344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Physical-chemical conditions of the Teide volcanic system (Tenerife, Canary Islands)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145162998784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Helium emission at Cumbre Vieja volcano, La Palma, Canary Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145314646656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Helium‐3 emission in and around Teide Volcano, Tenerife, Canary Islands, Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146433439104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Volcanic evolution of the island of Tenerife (Canary Islands) in the light of new K-Ar data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620762531584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Relationship between helium isotopes and heat flux from hot springs in a non‐volcanic region, Kii Peninsula, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165272694272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A magmatic source for fumaroles and diffuse degassing from the summit crater of Teide Volcano (Tenerife, Canary Islands): a geochemical evidence for the 2004–2005 seismic–volcanic crisis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093960346240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Eruptive and structural history of Teide Volcano and rift zones of Tenerife, Canary Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095060996736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Global emissions of helium‐3 by subaerial volcanism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096157656192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Volcanoes and the environment: Lessons for understanding Earth's past and future from studies of present-day volcanic emissions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096299026304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon Dioxide Discharged through the Las Cañadas Aquifer, Tenerife, Canary Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360845538931699200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon dioxide diffuse degassing and estimation of heat release from volcanic and hydrothermal systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640249413504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diffuse volcanic degassing and thermal energy release from Hengill volcanic system, Iceland"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640249441792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diffuse volcanic gas emission and thermal energy release from the summit crater of Pico do Fogo, Cape Verde"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640249452416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Carbon dioxide and helium dissolved gases in groundwater at central Tenerife Island, Canary Islands: chemical and isotopic characterization"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846643404916480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diffusive helium emissions as a precursory sign of volcanic unrest"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568553481728","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stratigraphy, structure and geochronology of the Las Cañadas caldera (Tenerife, Canary Islands)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569294934400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Vertical and lateral collapses on Tenerife (Canary Islands) and other volcanic ocean islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570810948480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"40 Ar/ 39 Ar stratigraphy of pyroclastic units from the Cañadas Volcanic Edifice (Tenerife, Canary Islands) and their bearing on the structural evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570955245952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Helium/Carbon Dioxide Ratios as Premonitors of Volcanic Activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571326358656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Helium-3 Emission Related to Volcanic Activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571425366784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"3He/4He Isotopic Ratios in Volcanic-Hydrothermal Discharges from the Canary Islands, Spain: Implications on the Origin of the Volcanic Activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520175796736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Using microscope observations of thin sections to estimate soil permeability with the Kozeny–Carman equation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521337393152","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Origin of 3He/4He ratios in HIMU-type basalts constrained from Canary Island lavas"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994043233408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Variable 3He/heat ratios in submarine hydrothermal systems: evidence from two plumes over the Juan de Fuca ridge"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996146567808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An Improved Method for Measuring Soil Respiration in the Field"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468328998656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Canary Islands origin: a unifying model"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468993831552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Helium isotopes in geothermal systems: Iceland, The Geysers, Raft River and Steamboat Springs"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945875082880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CO2 emissions and heat flow through soil, fumaroles, and steam heated mud pools at the Reykjanes geothermal area, SW Iceland"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946175937536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Helium isotope ratios in mafic phenocrysts and geothermal fluids from La Palma, the Canary Islands (Spain): implications for HIMU mantle sources"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946418003072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An increasing trend of diffuse CO\n            <sub>2</sub>\n            emission from Teide volcano (Tenerife, Canary Islands): geochemical evidence of magma degassing episodes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420542738688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diffuse emission of carbon dioxide, methane, and helium‐3 from Teide Volcano, Tenerife, Canary Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420969646592","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Primordial neon, helium, and hydrogen in oceanic basalts"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893305516800","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Las Cañadas caldera (Tenerife, Canary Islands): an overlapping collapse caldera generated by magma-chamber migration"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894699175424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The nature and assessment of heat flow from hydrothermal areas"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370597572096","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Migration of carrier and trace gases in the geosphere: an overview"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844302772352","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Noble Gas Isotope Geochemistry of Mid-Ocean Ridge and Ocean Island Basalts: Characterization of Mantle Source Reservoirs"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318700833024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An in situ method for measuring CO2 flux from volcanic-hydrothermal fumaroles"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319161726848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CO2 soil flux at Vulcano (Italy): comparison between active and passive methods"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320340790144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Morphological and statistical characterisation of recent mafic volcanism on Tenerife (Canary Islands, Spain)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795050839424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Determination of tritium by mass spectrometric measurement of 3He"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795626670208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"CO<sub>2</sub> degassing and energy release at Solfatara volcano, Campi Flegrei, Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268375553280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diffuse CO2 degassing at Vesuvio, Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268525762048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stratigraphy, structure, and volcanic evolution of the Pico Teide–Pico Viejo formation, Tenerife, Canary Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268895034112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geographical distribution of <sup>3</sup>He/<sup>4</sup>He ratios in Japan: Implications for arc tectonics and incipient magmatism"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233268942914816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Implications for the early shield-stage evolution of Tenerife from K/Ar ages and magnetic stratigraphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679528396928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The 3He/4He ratio of the new internal He Standard of Japan (HESJ)."},{"@language":"ja-Kana","@value":"3He 4He ratio of the new internal He Standard of Japan HESJ"},{"@value":"The 3 He/ 4 He ratio of new internal He Standard of Japan (HESJ)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679528438528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"3He/4He ratio distribution in and around the Hakone volcano."},{"@value":"3He/4He ratio distribution in and around Hakone volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681470559232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Highly Sensitive and Precise Measurement of Helium Isotopes Using a Mass Spectrometer with Double Collector System."}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1155/2019/3983864"},{"@type":"KAKEN","@value":"PRODUCT-22844111"},{"@type":"OPENAIRE","@value":"doi_dedup___::c35d6074df05a91ca54a5243b7931f8b"}]}