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基于谱聚类算法的海底滑坡危险性评价

杜星 孙永福 宋玉鹏 修宗祥 单治钢

杜星,孙永福,宋玉鹏,等. 基于谱聚类算法的海底滑坡危险性评价[J]. 海洋学报,2021,43(1):93–101 doi: 10.12284/hyxb2021023
引用本文: 杜星,孙永福,宋玉鹏,等. 基于谱聚类算法的海底滑坡危险性评价[J]. 海洋学报,2021,43(1):93–101 doi: 10.12284/hyxb2021023
Du Xing,Sun Yongfu,Song Yupeng, et al. Risk assessment of submarine landslide based on spectral clustering[J]. Haiyang Xuebao,2021, 43(1):93–101 doi: 10.12284/hyxb2021023
Citation: Du Xing,Sun Yongfu,Song Yupeng, et al. Risk assessment of submarine landslide based on spectral clustering[J]. Haiyang Xuebao,2021, 43(1):93–101 doi: 10.12284/hyxb2021023

基于谱聚类算法的海底滑坡危险性评价

doi: 10.12284/hyxb2021023
基金项目: 中国电建集团华东勘测设计研究院有限公司201项目(KY2018-ZD-01);山东省自然科学基金(ZR2020QD073);国家重点研发计划项目(2017YFC0307305);国家自然科学基金(41606084)。
详细信息
    作者简介:

    杜星(1991-),男,辽宁省大连市人,工程师,主要从事海洋工程地质与灾害地质方面研究。E-mail:duxing@fio.org.cn

    通讯作者:

    单治钢(1965-),男,高级工程师(教授级),主要从事水电工程地质、岩土力学方面的研究。E-mail:shan_zg@ecidi.com

  • 中图分类号: P642.22

Risk assessment of submarine landslide based on spectral clustering

  • 摘要: 海底滑坡的危险性评价与分区,对海洋工程设施的选址和危险预防具有指导作用。本文基于无监督机器学习的谱聚类算法对黄河口埕岛海域展开了海底滑坡危险性评价,构建了输入参数为9、输出类别为4、核函数参数为0.08的海底滑坡危险性评价模型。使用该模型进行评价,将研究区分为了海底滑坡危险性高、较高、较低和低的区域。评价结果与地质环境因素分布特征对比显示,最重要的影响因素为海底沉积物类型和水动力作用,最重要的触发因子为液化。模型参数分析结果显示,合理简化输入因子可获得精度略低的评价结果,而核函数参数是影响评价准确性的重要指标。以上研究表明,谱聚类算法能够较好地用于海底滑坡危险性评价,数据类别丰富度和精度是影响评价精细程度的重要因素。
  • 图  1  研究区位置及研究点位

    Fig.  1  Location of studying area and points

    图  2  海底滑坡危险性评价网络结构示意图

    图中左侧为网络输入因子类别,右侧为输出因子类别,连线表示聚类的左右关系示意,并非一一对应关系

    Fig.  2  Schematic diagram of submarine landslide risk assessment network structure

    The left side is the network input factor category, and the right side is the output factor category. The connecting line indicates the left-right relationship of clustering, not one-to-one correspondence

    图  3  评价网络得分随核函数参数的变化

    Fig.  3  Evaluation network score changes with kernel function parameters

    图  4  黄河口海底滑坡危险性评价结果

    虚线a为危险性较高和危险性低分区间的突变界限,由海底沉积物类型的突变引起

    Fig.  4  Risk assessment result of submarine landslides in the Yellow River Estuary

    The dotted line a is the mutation boundary between high risk and low risk zones, which is caused by the mutation of seabed sediment types

    图  5  黄河口埕岛海域液化深度分布[22]

    液化深度分布使用了50年一遇风浪条件下数据进行计算,并与物探测得的液化扰动层分布进行了对比验证

    Fig.  5  Distribution of liquefaction depth in Chengdao sea area of the Yellow River Estuary[22]

    The liquefaction depth distribution is calculated by using the data of 50 years return period wind and wave, and compared with the distribution of liquefaction disturbance layer measured by geophysical prospecting

    图  6  简化输入因子得到的海底滑坡危险性评价结果

    Fig.  6  Risk assessment results of submarine landslides from simplified input factors

    图  7  不同核函数参数海底滑坡危险性评价结果

    Fig.  7  Risk assessment results of submarine landslides with different kernel function parameters

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出版历程
  • 收稿日期:  2019-12-11
  • 修回日期:  2020-02-23
  • 网络出版日期:  2021-02-24
  • 刊出日期:  2021-01-25

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