{"@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/1362825893576412416.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2010jb007526"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010JB007526"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2010JB007526"}}],"dc:title":[{"@value":"Dependence of spectral‐induced polarization response of sandstone on temperature and its relevance to permeability estimation"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The possibility to estimate permeability from the electrical spectral induced polarization (SIP) response might be the most important benefit offered by SIP measurements. It can thus be deduced that, in the future, SIP measurements will be carried out more frequently at the field scale or in a well‐logging context to estimate permeability. In the shallow subsurface, however, the temperature generally exhibits seasonal variability, and in the deeper subsurface, it usually increases with depth. Hence, knowledge about the dependence of the SIP response on temperature is necessary in order to avoid possible misinterpretation of datasets impacted by thermal effects. In our study, we present a semiempirical framework to describe the temperature dependence of the SIP response. We briefly introduce the SIP response and its relation to permeability in terms of an electrochemical polarization mechanism and combine this formulation with relationships for the dependence of ionic mobility on temperature. We compare the predictions of our formulation with the experimental data from SIP measurements performed on sandstone at temperatures from 0°C to 80°C. The measured SIP response was transformed into a relaxation time distribution, using the empirical Cole‐Cole model and a regularized Debye decomposition procedure. The SIP response was found to be in good agreement with the theoretical model. The temperature dependence of both direct current conductivity and relaxation time is controlled mainly by the dependence of ionic mobility on temperature, and the shape of the relaxation time distribution of the investigated sandstone is almost independent of temperature. The temperature effect on the SIP response can therefore be easily corrected.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380285711829471235","@type":"Researcher","foaf:name":[{"@value":"N. Zisser"}],"jpcoar:affiliationName":[{"@value":"Section HPHT/Petrophysics University of Bonn  Bonn Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893576412418","@type":"Researcher","foaf:name":[{"@value":"A. Kemna"}],"jpcoar:affiliationName":[{"@value":"Department of Geodynamics and Geophysics University of Bonn  Bonn Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893576412416","@type":"Researcher","foaf:name":[{"@value":"G. Nover"}],"jpcoar:affiliationName":[{"@value":"Section HPHT/Petrophysics University of Bonn  Bonn Germany"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2010-09","prism:volume":"115","prism:number":"B9","prism:startingPage":"B09214"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2010JB007526"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2010JB007526"}],"createdAt":"2010-09-29","modifiedAt":"2023-11-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390001288107943040","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"海洋資源の成因の科学的研究に基づく調査海域絞込み手法の開発： 戦略的イノベーション創造プログラム（SIP）「次世代海洋資源調査技術」における 産総研地質調査総合センター（GSJ）の研究開発成果"},{"@language":"en","@value":"Scientific research on formation processes of ocean resources: GSJ’s research results of the Cross-ministerial Strategic Innovation Promotion Program (SIP), “Next-generation technology for ocean resources exploration”."},{"@language":"ja-Kana","@value":"カイヨウ シゲン ノ セイイン ノ カガクテキ ケンキュウ ニ モトズク チョウサ カイイキ シボリコミ シュホウ ノ カイハツ : センリャクテキ イノベーション ソウゾウ プログラム(SIP)「 ジセダイ カイヨウ シゲン チョウサ ギジュツ 」 ニ オケル サン ソウケン チシツ チョウサ ソウゴウ センター(GSJ)ノ ケンキュウ カイハツ セイカ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317003648768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Depth profiles of resistivity and spectral IP for active modern submarine hydrothermal deposits : a case study from the Iheya North Knoll and the Iheya Minor Ridge in Okinawa Trough, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2010jb007526"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.69.265_references_DOI_9tqYFFFkAOXMQGaSjU7mLmjAKb0"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0691-6_references_DOI_9tqYFFFkAOXMQGaSjU7mLmjAKb0"}]}