@article{oai:kitami-it.repo.nii.ac.jp:02000014,
 author = {川尻, 峻三 and KAWAJIRI, Shunzo and 渡邊, 康玄 and Watanabe, Yasuhau and 森田, 大詩 and MORITA, Taishi and 新妻, 重明 and NIITSUMA, Shigeaki and 木下, 誠一 and KINOSHITA, Seiichi},
 journal = {河川技術論文集},
 month = {Jun},
 note = {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.},
 pages = {55--60},
 title = {河床下地質構造の把握に対する表面波探査の適用性},
 volume = {22},
 year = {2016},
 yomi = {ワタナベ, ヤスハル}
}