![]() |
[email protected] |
![]() |
3275638434 |
![]() |
![]() |
Paper Publishing WeChat |
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License
Tetsuya Oyamada, Shunsuke Hanehara, Hideaki Deto and Shoji Iwasaki
Full-Text PDF
XML 495 Views
DOI:10.17265/1934-7359/2014.07.001
Department of Civil and Environmental Engineering, Iwate University, Iwate 0208551, Japan
This research paper describes the tsunami damage to tide walls observed using aerial photographs and field investigations at 13 locations along the coast of Iwate Prefecture, where significant tsunami damage occurred as a result of the Great East Japan Earthquake. This paper also summarizes the characteristics of the damage. The tide walls in Iwate Prefecture were constructed on a ria (hilly type) coast, this geographical feature of Iwate being different from that of the other disaster areas, primarily Miyagi and Fukushima Prefectures. The results of our investigations show that all the devastated tide walls suffered from overflow before being damaged. In particular, the sloping and vertical type tide walls with slope protection were damaged by scouring of the infill sand or back fill soil due to the overflow of the tsunami. In the case of vertical type tide walls without slope protection, damage was caused by scouring of the back fill soil.
Tide wall, Great East Japan Earthquake, tsunami.