Abstract

Submarine debris flows and their generated waves are common disasters in Nature that may destroy offshore infrastructure and cause fatalities. As the propagation of submarine debris flows is complex, involving granular material sliding and wave generation, it is difficult to simulate the process using conventional numerical models. In this study, a numerical model based on the smoothed particle hydrodynamics (SPH) algorithm is proposed to simulate the propagation of submarine debris flow and predict its generated waves. This model contains the Bingham fluid model for granular material, the Newtonian fluid model for the ambient water, and a multiphase granular flow algorithm. Moreover, a boundary treatment technique is applied to consider the repulsive force from the solid boundary. Underwater rigid block slide and underwater sand flow were simulated as numerical examples to verify the proposed SPH model. The computed wave profiles were compared with the observed results recorded in references. The good agreement between the numerical results and experimental data indicates the stability and accuracy of the proposed SPH model.

Highlights

  • Submarine debris flows are widely distributed on continental shelves, continental slopes and in deepwater areas, where they pose a serious threat to offshore infrastructure, such as submarine pipelines and cables, offshore oil and gas platforms, and offshore wind farms [1]

  • Numerical models based on depth-averaged equations (DAEs) were tabulated according to their conceptual, mathematical, and numerical approaches

  • This work aimed to establish an smoothed particle hydrodynamics (SPH) model to simulate surge waves generated by submarine debris flows, and to show the accuracy and stability of this model in the simulation of multiphase flow problems

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Summary

Introduction

Submarine debris flows are widely distributed on continental shelves, continental slopes and in deepwater areas, where they pose a serious threat to offshore infrastructure, such as submarine pipelines and cables, offshore oil and gas platforms, and offshore wind farms [1]. The 1958 Lituya Bay debris flow-generated tsunami produced a run-up of over 400 m [2]. Another significant tsunami was generated by a submarine debris flow at the Nice airport in France on 16 October 1979, and swept away 11 people [3]. In 2018, the submarine debris flow induced by the Palu earthquake resulted in devastating tsunamis and caused more than 2000 fatalities in Sulawesi, Indonesia [9,10,11]. These debris flowgenerated tsunami disasters have attracted a lot of attention from researchers

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