{"@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/1360574094875663872.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1046/j.1365-2478.1999.00129.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-2478.1999.00129.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-2478.1999.00129.x"}}],"dc:title":[{"@value":"Relationship between P‐ and S‐wave velocities and geological properties of near‐surface sediments of the continental slope of the Barents Sea"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Seismic velocities (<jats:italic>V</jats:italic><jats:sub>p</jats:sub> and <jats:italic>V</jats:italic><jats:sub>s</jats:sub>) of compressional (P‐) and shear (S‐) waves are important parameters for the characterization of marine sediments with respect to their sedimentological and geotechnical properties. P‐ and S‐wave velocity data of near‐surface marine sediments (upper 9 m) of the continental slope of the Barents Sea are analysed and correlated to sedimentological and geotechnical properties. The results show that the S‐wave velocity is much more sensitive to changes in lithology and mechanical properties than the P‐wave velocity, which is characterized by a narrow range of values. The correlation coefficients between S‐wave velocity and silt and clay content, wet bulk density, porosity, water content and shear strength are higher than 0.5 while the correlation coefficients of P‐wave velocity and the same parameters are always lower than 0.4. Although the relationship between <jats:italic>V</jats:italic><jats:sub>s</jats:sub> and clay content has been widely described, the data show that <jats:italic>V</jats:italic><jats:sub>s</jats:sub> is better correlated with silt content than with clay content for the sediments of the area investigated. However, they show different trends. While <jats:italic>V</jats:italic><jats:sub>s</jats:sub> increases with increasing clay content, it decreases with increasing silt content.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380574094875663873","@type":"Researcher","foaf:name":[{"@value":"Arthur Ayres"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574094875663872","@type":"Researcher","foaf:name":[{"@value":"Friedrich Theilen"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00168025"},{"@type":"EISSN","@value":"13652478"}],"prism:publicationName":[{"@value":"Geophysical Prospecting"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"1999-07","prism:volume":"47","prism:number":"4","prism:startingPage":"431","prism:endingPage":"441"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-2478.1999.00129.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-2478.1999.00129.x"}],"createdAt":"2003-03-11","modifiedAt":"2023-10-28","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360294643714643712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Subsurface Imaging With Ocean‐Bottom Distributed Acoustic Sensing and Water Phases Reverberations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588380129500800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Surface wave monitoring using ambient noise for detecting temporal variations in underground structures in landslide area"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473984256","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geotechnical properties of Holocene and latest Pleistocene sediments with special reference to shear wave velocities"},{"@language":"ja","@value":"高精度Ｓ波速度検層データを指標とした沖積層の堆積環境と工学的特性の検討"},{"@language":"ja-Kana","@value":"コウセイド Sハ ソクド ケンソウ データ オ シヒョウ ト シタ チュウセキソウ ノ タイセキ カンキョウ ト コウガクテキ トクセイ ノ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942155084672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detailed S-wave velocity structure of sediment and crust off Sanriku, Japan by a new analysis method for distributed acoustic sensing data using a seafloor cable and seismic interferometry"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1046/j.1365-2478.1999.00129.x"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01652-z_references_DOI_aPsbVufxhoSmv1UmkXQO1xOIq0"},{"@type":"CROSSREF","@value":"10.1029/2021gl095287_references_DOI_aPsbVufxhoSmv1UmkXQO1xOIq0"},{"@type":"CROSSREF","@value":"10.4116/jaqua.47.121_references_DOI_aPsbVufxhoSmv1UmkXQO1xOIq0"},{"@type":"CROSSREF","@value":"10.1016/j.enggeo.2024.107706_references_DOI_aPsbVufxhoSmv1UmkXQO1xOIq0"}]}