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Injection commenced at Sleipner in 1996 with CO2 separated from natural gas being injected into the Utsira Sand, a major saline aquifer of late Cenozoic age. CO2 injection is via a near-horizontal well at a depth of about 1012 m below sea level (bsl) some 200 m below the reservoir top, at a rate approaching 1 million tonnes (Mt) per year, with more than 11 Mt currently stored.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319831487234","@type":"Researcher","foaf:name":[{"@value":"Andy Chadwick"}],"jpcoar:affiliationName":[{"@value":"1 British Geological Survey"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319831487241","@type":"Researcher","foaf:name":[{"@value":"Gareth Williams"}],"jpcoar:affiliationName":[{"@value":"1 British Geological Survey"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319831487242","@type":"Researcher","foaf:name":[{"@value":"Nicolas Delepine"}],"jpcoar:affiliationName":[{"@value":"2 IFP"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319831487236","@type":"Researcher","foaf:name":[{"@value":"Vincent Clochard"}],"jpcoar:affiliationName":[{"@value":"2 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