{"created":"2021-03-01T06:00:07.790610+00:00","id":7672,"links":{},"metadata":{"_buckets":{"deposit":"b67860d8-c561-45f6-a619-25d1cc184e35"},"_deposit":{"id":"7672","owners":[],"pid":{"revision_id":0,"type":"depid","value":"7672"},"status":"published"},"_oai":{"id":"oai:kitami-it.repo.nii.ac.jp:00007672","sets":["1:86"]},"author_link":["39372","39373","39374","39375","39376","39377","39378","39379","44835","39365","39366","39367","44837","44836","39370","39371"],"item_1646810750418":{"attribute_name":"\u51fa\u7248\u30bf\u30a4\u30d7","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_3_alternative_title_198":{"attribute_name":"\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb","attribute_value_mlt":[{"subitem_alternative_title":"Basic Study on the Frost Heave Pressure of Rocks : Dependence of the Maximum Frost Heave Pressure on Temperature"}]},"item_3_biblio_info_186":{"attribute_name":"\u66f8\u8a8c\u60c5\u5831","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2011-07","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"8","bibliographicPageEnd":"496","bibliographicPageStart":"485","bibliographicVolumeNumber":"127","bibliographic_titles":[{"bibliographic_title":"journal of the Mining and Materials Processing Institute of Japan"}]}]},"item_3_description_184":{"attribute_name":"\u6284\u9332","attribute_value_mlt":[{"subitem_description":"In this study, we attempted to measure frost heave pressure, i.e., the pressure that develops in the heat-flow direction when rocks are subject to frost heave and ice lenses grow. <BR>We used two kinds of rock samples: one was Ohya tuff, whose frost heave was already known to be high, and the other was Kimachi sandstone, whose frost heave was lower than that of the former. <BR>Ohya tuff and Kimachi sandstone, in which the occurrence of frost heave has previously been confirmed, were used as specimens.<BR>To conduct the experiment, we made original frost heave experiment equipment that was combined with a reaction frame and a load cell.<BR>The test results clearly showed that the maximum frost heave pressure did not depend on the kind of rock and was proportional to the temperature gradient. <BR>In addition, we clarified that the speed of the increase in pressure was proportional to the frost heave rate ? the growth rate of the ice lens.","subitem_description_type":"Abstract"}]},"item_3_full_name_183":{"attribute_name":"\u8457\u8005\u5225\u540d","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"39372","nameIdentifierScheme":"WEKO"}],"names":[{"name":"NAKAMURA, Dai","nameLang":"en"}]},{"nameIdentifiers":[{"nameIdentifier":"39373","nameIdentifierScheme":"WEKO"}],"names":[{"name":"GOTO, 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Rate","subitem_subject_scheme":"Other"},{"subitem_subject":"Temperature Gradient","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"\u8a00\u8a9e","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"\u8cc7\u6e90\u30bf\u30a4\u30d7","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"\u5ca9\u77f3\u306e\u51cd\u4e0a\u5727\u306b\u95a2\u3059\u308b\u57fa\u790e\u7684\u7814\u7a76 : \u5ca9\u77f3\u306e\u6700\u5927\u51cd\u4e0a\u5727\u306e\u6e29\u5ea6\u4f9d\u5b58\u6027","item_titles":{"attribute_name":"\u30bf\u30a4\u30c8\u30eb","attribute_value_mlt":[{"subitem_title":"\u5ca9\u77f3\u306e\u51cd\u4e0a\u5727\u306b\u95a2\u3059\u308b\u57fa\u790e\u7684\u7814\u7a76 : \u5ca9\u77f3\u306e\u6700\u5927\u51cd\u4e0a\u5727\u306e\u6e29\u5ea6\u4f9d\u5b58\u6027","subitem_title_language":"ja"},{"subitem_title":"Basic Study on the Frost Heave Pressure of Rocks : Dependence of the 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