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        <identifier>oai:kitami-it.repo.nii.ac.jp:02000014</identifier>
        <datestamp>2026-02-17T03:47:15Z</datestamp>
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          <dc:title>河床下地質構造の把握に対する表面波探査の適用性</dc:title>
          <dc:title>APPLICABILITY OF SURFACE WAVE METHOD TO GEOLOGICAL PROFILE UNDER RIVERBED</dc:title>
          <dc:creator>川尻, 峻三</dc:creator>
          <dc:creator>KAWAJIRI, Shunzo</dc:creator>
          <dc:creator>渡邊, 康玄</dc:creator>
          <dc:creator>Watanabe, Yasuharu</dc:creator>
          <dc:creator>森田, 大詩</dc:creator>
          <dc:creator>MORITA, Taishi</dc:creator>
          <dc:creator>新妻, 重明</dc:creator>
          <dc:creator>NIITSUMA, Shigeaki</dc:creator>
          <dc:creator>木下, 誠一</dc:creator>
          <dc:creator>KINOSHITA, Seiichi</dc:creator>
          <dc:subject>Surface wave method</dc:subject>
          <dc:subject>S-warn velocity</dc:subject>
          <dc:subject>N-vale</dc:subject>
          <dc:subject>geological profile</dc:subject>
          <dc:subject>under riverbed</dc:subject>
          <dc:description>This paper is considering the applicability of the surface wave method for understanding the geological profile under the riverbed. The profile of S-wave velocity and the N-value were well matched. Therefore, S-wave velocity in the grom1d of the river zone can be treated as an indicator similar to the N -value. It is reasonable estimate of the geological cross-sectional view by using the S-wave velocity distribution. In addition, the pseudo-three-dimensional dist1ibution of S-wave velocity, was consistent with the local situation. As a results, the use of the S-wave velocity distribution obtained from the surface wave method, it is possible to create the 3D hazard map for riverbed degradation and improving the accuracy of the analysis model.</dc:description>
          <dc:description>journal article</dc:description>
          <dc:publisher>土木学会</dc:publisher>
          <dc:date>2016-06</dc:date>
          <dc:format>application/pdf</dc:format>
          <dc:identifier>河川技術論文集</dc:identifier>
          <dc:identifier>22</dc:identifier>
          <dc:identifier>55</dc:identifier>
          <dc:identifier>60</dc:identifier>
          <dc:identifier>https://kitami-it.repo.nii.ac.jp/record/2000014/files/kasengijutu_22,55-60.pdf</dc:identifier>
          <dc:identifier>https://kitami-it.repo.nii.ac.jp/records/2000014</dc:identifier>
          <dc:language>jpn</dc:language>
          <dc:rights>c 2016 土木学会</dc:rights>
          <dc:rights>open access</dc:rights>
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