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基于改进的FAST模型的千将坪滑坡涌浪研究

赵永波 王健 黄波林 谭建民 王世昌

华南地质与矿产2017,Vol.33Issue(4):411-418,8.
华南地质与矿产2017,Vol.33Issue(4):411-418,8.DOI:10.3969/j.issn.1007-3701.2017.04.010

基于改进的FAST模型的千将坪滑坡涌浪研究

Study on impulse wave generated by Qian-jiangping landslide based on improved FAST model

赵永波 1王健 2黄波林 2谭建民 3王世昌1

作者信息

  • 1. 中国地质调查局武汉地质调查中心,武汉430205
  • 2. 防灾减灾湖北省重点实验室(三峡大学),湖北宜昌443002
  • 3. 湖北长江三峡滑坡国家野外科学观测研究站,湖北宜昌443002
  • 折叠

摘要

Abstract

Qianjiangping landslide is a typical impulse wave example generated by landslide in shallow water area in Three Gorges Reservoir,but there are seldom water dynamic process and impulse wave research progress, especially focusing on waterway in range of big region and long distance. Based on the formulae derived from physical experiments on impulse wave generated in shallow water,numerical model of landslide-induced impulse wave in shallow water is built in the former Code named Forecasting Analysis System for Tsunami generated by landslides, and study on impulse wave generated by Qianjiangping landslide is carried out, updating the FAST landslide impulse wave calculation system and establishing the corresponding wave source model.The numerical calculating region is 18.6 km×11.8 km,including the Yangtze River and its branch around Qianjiangping land-slide.The calculating results show that the maximum of impulse wave is about 38.8 m and the maximum run-up is about 36.7 m.The spatial distribution of impulse wave presents that there are about 10.5 km long waterway with impulse wave above 1 m-height,there are about 9.3 km long waterway with impulse wave above 2 m-height,and there are about 8 km long waterway with impulse wave above 3 m-height.The waterway with impulse wave above 1 m-height concentrated distribute in Qinggan river and Luogudong River.There exist rapid decay and enlarge-ment effect when impulse wave propagate in waterway encountering various topographical.Comparing with multi-source data,the run-up values are differ in about ±2 m with the correlation coefficient of 0.97.The established impulse wave numerical model has the advantages of less computation resource consumption, fast calculating speed and better accuracy numerical results.This numerical model of landslide-induced impulse wave in shallow water is beneficial to the research on impulse wave problem in branch or shallow water in reservoir, which can give important technical support for forecasting and prewarning on landslide-induced impulse wave in huge re-gion and long distance.

关键词

千将坪滑坡/浅水区滑坡涌浪源模型/水波动力学/涌浪过程/影响范围

Key words

Qianjiangping landslide/numerical model of landslide-induced impulse wave in shallow water/wa-ter wave dynamic/impulse wave process/effect range

分类

天文与地球科学

引用本文复制引用

赵永波,王健,黄波林,谭建民,王世昌..基于改进的FAST模型的千将坪滑坡涌浪研究[J].华南地质与矿产,2017,33(4):411-418,8.

基金项目

国家自然科学基金(编号:41372321). (编号:41372321)

华南地质与矿产

1007-3701

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