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津波越流による海岸堤防陸側地盤での洗掘に関する研究

Takegawa, Naoki 神戸大学

2021.03.25

概要

In the 2011 off the Pacific coast of Tohoku Earthquake, a huge tsunami destroyed many coastal protection facilities, such as seawalls and coastal dikes. As of June 10, 2020, the number of deaths from the Great East Japan Earthquake was 15,899, and more than 90% of the deaths were caused by drowning. This huge tsunami not only caused human casualties, but also devastated coastal dikes and other coastal facilities. The purpose of this thesis is to reduce the damage to human life and social infrastructure caused by tsunami overflow through the scour prediction, countermeasures, and applications on the landward side ground of coastal dikes. This paper is composed of 6 chapters, and the contents and conclusions obtained are shown below.

 Chapter 1 introduces an overview of the 2011 off the Pacific coast of Tohoku Earthquake, the mechanism of dike failure and the necessary considerations for the design of coastal dikes.

 In Chapter 2, small-scale model experiments were carried out to examine the effect of the geogrid as scour countermeasures. Sheet-like (two-dimensional) countermeasures are expected to reduce the cost of constniction. A geogrid placed in the vicinity of a coastal dike reduced the scour area by 90%. Increasing the countenneasure length beyond the dike height has little effect on the scour area in the vicinity of tlie dike. In addition to model experiments, numerical simulations were also performed to evaluate the energy dissipation of tsunamis due to the scour hole. When the reduction effect of the velocity is high, the flow velocity decreases by 30% due to scour holes compared the case without countermeasures.

 Chapter 3 complements the validity of the results obtained in Chapter 2. The effect of geogrids was tested by increasing the external force with a vertical jet and locally reproducing a situation similar to real scale conditions. The effects of mesh size and coverage ratio (the proportion of scour countermeasures per unit area) on the scour were investigated, and it was found that when the ratio between the 85% particle size of the bed material and the mesh size below 1.0, both the scour depth and the maximum pore-water pressure are significantly suppressed. In the most effective cases, tlie sheet-like countermeasures reduced the maximum pore-water pressure and the scour depth, respectively, by 91% and 86%. As for the ground where an upward-hydraulic gradient, in the case using the geogrod, no increase in the scour depth was observed. Conversely, when gravel was used, the maximum scour depth increased by a factor of about 1.6 compared to the bed without the upward-hydraulic gradient. This is because the bearing force of the sand bed against the gravel decreases due to the upward-hydraulic gradient.

 In Chapter 4, predictive equations for the scour length and scour depth are proposed on the basis of the present experimental results and previous studies. In determining the coefficients of the equations, the results of various model experiments (Scale of model experiment: 1/50 - 1/2) were used, and tlie experimental results could be expressed in the predictive equations. A comparison between the predictive equations and the scour holes, which were confirmed during the 2011 off the Pacific coast of Tohoku Earthquake, shows good agreement with the field surveys. Furthermore, equations for the case where foundations are placed at the landward ground behind coastal dikes were also derived. From the coefficients of the predictive equations, the scour length increases about 1.2 times and the scour depth decreases about 0.47 times when the foundation is placed at the ground behind coastal dikes.

 In Chapter 5, a new method is proposed that involves using the erosion effect of the tsunami itself to do the velocity reduction work. This method is to replace a part of the ground in advance with a lightweight material to accelerate the erosion at the time of tsunami attack. When the flow was subcritical, the velocity could not be reduced even if a depression was provided. When the flow was supercritical, the depression that formed changed the flow from supercritical to subcritical, and the flow velocity decreased. Assuming a tsunami overflow to be a constant flow rate, the author predicted the tsunami run-up velocity. Comparing the predicted results with experimental results show that the velocity can be predicted with an uncertainty of approximately 20%. The simple predictive method is considered to be extremely useful given that it would be handled easily by general engineers.

 Chapter 6 summarizes the results of this thesis with the conclusions.

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