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        <identifier>oai:kitami-it.repo.nii.ac.jp:00008450</identifier>
        <datestamp>2026-02-17T02:30:40Z</datestamp>
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          <dc:title xml:lang="ja">アンカーアイスが結氷河川の物質循環に与える影響</dc:title>
          <dc:title xml:lang="en">THE INFLUENCE OF ANCHOR ICE ON MATERIAL CIRCULATION IN THE ICE-COVERED RIVER</dc:title>
          <jpcoar:creator>
            <jpcoar:creatorName xml:lang="ja">鈴木, 広卓</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:creatorName xml:lang="ja">橋場, 雅弘</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:creatorName xml:lang="ja">吉川, 泰弘</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:creatorName xml:lang="ja">黒田, 保孝</jpcoar:creatorName>
          </jpcoar:creator>
          <dcterms:accessRights rdf:resource="http://purl.org/coar/access_right/c_abf2">open access</dcterms:accessRights>
          <dc:rights>c 2015 公益社団法人　土木学会</dc:rights>
          <jpcoar:subject subjectScheme="Other">anchor ice</jpcoar:subject>
          <jpcoar:subject subjectScheme="Other">ice-covered river</jpcoar:subject>
          <jpcoar:subject subjectScheme="Other">material circulation</jpcoar:subject>
          <datacite:description descriptionType="Abstract">This study was conducted to clarify the mechanism of anchor ice formation on the river bed and to
understand the impact of anchor ice on material transport in ice-covered river. Field observations
indicated that anchor ice formation was significantly affected by the air temperatures and water
temperatures as well as by the hydraulic conditions, such as the water depth and the flow velocity. We
tried to simulate anchor ice formation in the actual river. The simulation results showed that accurate
estimation of the temperature of river bed material that incorporated the influence of solar radiation and
ground heat was critical for enhancing calculation precision. We could estimate that the anchor ice pulled
away the algae from the river bed and flushed them to downstream, similar to a bed load transport in
summer flood. This study proved that the river used for simulation had a specific material circulation due
to frazil ice and anchor ice.</datacite:description>
          <dc:publisher>公益社団法人　土木学会</dc:publisher>
          <datacite:date dateType="Issued">2015-06</datacite:date>
          <dc:language>jpn</dc:language>
          <dc:type rdf:resource="http://purl.org/coar/resource_type/c_6501">journal article</dc:type>
          <oaire:version rdf:resource="http://purl.org/coar/version/c_970fb48d4fbd8a85">VoR</oaire:version>
          <jpcoar:identifier identifierType="URI">https://kitami-it.repo.nii.ac.jp/records/8450</jpcoar:identifier>
          <jpcoar:sourceIdentifier identifierType="EISSN">2436-6714</jpcoar:sourceIdentifier>
          <jpcoar:sourceTitle>河川技術論文集</jpcoar:sourceTitle>
          <jpcoar:volume>21</jpcoar:volume>
          <jpcoar:pageStart>49</jpcoar:pageStart>
          <jpcoar:pageEnd>54</jpcoar:pageEnd>
          <jpcoar:file>
            <jpcoar:URI label="2015-06_アンカーアイスが結氷河川の物質循環に与える影響.pdf">https://kitami-it.repo.nii.ac.jp/record/8450/files/2015-06_アンカーアイスが結氷河川の物質循環に与える影響.pdf</jpcoar:URI>
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            <jpcoar:extent>4.2 MB</jpcoar:extent>
            <datacite:date dateType="Available">2017-01-12</datacite:date>
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