2015
DOI: 10.1016/j.oceaneng.2015.08.053
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Scoured depth and length of pools and ditches generated by overtopping flow from embankments during the 2011 Great East Japan Tsunami

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Cited by 31 publications
(10 citation statements)
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“…Estimated processes of the failures of the coastal embankments by 2011 Tohoku Tsunami were discussed through the field observations by Kato et al [2013]. One of the main process of the failure is from the local scour around the landward toes of the coastal embankments, which were observed also by Tappin et al [2012], Tanaka and Sato [2015]. Ground near their landward toes was eroded severely by the flow over the embankments and sand under their concrete armors (as body material of the coastal embankments) was sucked out through the huge scours, leading to breaking of the concrete armors of landward slopes and finally complete flushing of the embankments themselves.…”
Section: Introductionmentioning
confidence: 99%
“…Estimated processes of the failures of the coastal embankments by 2011 Tohoku Tsunami were discussed through the field observations by Kato et al [2013]. One of the main process of the failure is from the local scour around the landward toes of the coastal embankments, which were observed also by Tappin et al [2012], Tanaka and Sato [2015]. Ground near their landward toes was eroded severely by the flow over the embankments and sand under their concrete armors (as body material of the coastal embankments) was sucked out through the huge scours, leading to breaking of the concrete armors of landward slopes and finally complete flushing of the embankments themselves.…”
Section: Introductionmentioning
confidence: 99%
“…To compare the effectiveness of DLMs (L2 with different porosities of L1), SLM (no L1) with a porosity of 0.98 was also implemented. In the 2011 GEJT, severe erosion occurred behind the embankments due to the overtopping tsunami, and the length of scouring varied from 4 to 31.78 (m) [16,39]. The length and depth of the scouring increased while increasing the momentum and energy head of the overtopping tsunami [39].…”
Section: Physical Model Of the Hybrid Defense Systemmentioning
confidence: 99%
“…In the 2011 GEJT, severe erosion occurred behind the embankments due to the overtopping tsunami, and the length of scouring varied from 4 to 31.78 (m) [16,39]. The length and depth of the scouring increased while increasing the momentum and energy head of the overtopping tsunami [39]. The study also observed that the trees that had been planted closer to the embankment on the leeward side were uprooted and produced floating debris, whereas a costal forest having no gap between the coastal dike and forest was completely damaged by the overtopping tsunami [16].…”
Section: Physical Model Of the Hybrid Defense Systemmentioning
confidence: 99%
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