Collapse Mechanisms of Seawall Due to the March 2011 Japan Tsunami Using the MPS Method

Author:

Arikawa Taro1,Ishikawa Nobutaka2,Beppu Masuhiro3,Tatesawa Hiroshi4

Affiliation:

1. Port and Airport Research Institute, 3-1-1 Nagase, Yokosuka 239-0826, Japan

2. Professor Emeritus of National Defense Academy, Yokosuka 238-0022, Japan

3. Dept. of Civil and Environmental Engineering, National Defense Academy, Yokosuka 239-8686 Japan

4. Bousai Consultant Co. Ltd., Morioka 020-0125, Japan

Abstract

On March 11 2011 a huge tsunami was caused by a magnitude 9.0 earthquake, which devastated the sea defenses in the Tohoku coastal region of Japan. We investigated one of the disaster areas, the Taro district, which had been very famous for having a 10m high seawall. This paper focuses on why the seawall in the Taro district collapsed during the tsunami. To this end the present work involves (1) the field disaster investigation, (2) the scale of the March 11 tsunami by performing its runup calculation, (3) the overflowing effects of the tsunami on the seawall by using the MPS (Moving Particle Semi-implicit) method, (4) the overflowing model test of a seawall and (5) the possible collapse mechanisms of the seawalls, in which they were mainly destroyed by the overflowing and the ensuing draw down wave of the tsunami.

Publisher

SAGE Publications

Subject

Mechanics of Materials,Safety, Risk, Reliability and Quality,Building and Construction

Reference11 articles.

1. Tsunami source of the 2011 off the Pacific coast of Tohoku Earthquake

2. Nakayama Y., Fluid Dynamics, P.129, Yokendo, March 1989, (in Japanese).

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