4.5 Article

Large-scale seafloor stability evaluation of the northern continental slope of South China Sea

期刊

MARINE GEORESOURCES & GEOTECHNOLOGY
卷 38, 期 7, 页码 804-817

出版社

TAYLOR & FRANCIS INC
DOI: 10.1080/1064119X.2019.1632996

关键词

The South China Sea; Northern continental slope; infinite sliding model; regional stability; quantitative evaluation

资金

  1. National Natural Science Foundation of China [51879036, 51579032]
  2. National Key Research and Development Program of China [2018YFC0309203]

向作者/读者索取更多资源

With the continuous expansion of energy demand, the deep-water continental slope in the northern South China Sea has become one of the significant offshore oil and gas exploration regions. The frequent occurrence of marine geological hazards in this region, especially submarine landslides, can cause serious damage to engineering facilities. However, there have been few studies on the stability of the northern continental slope of the South China Sea; these studies mainly focused on a specific submarine slope or small-range evaluation, resulting in a lack of large-scale and quantitative understanding. Hence, considering the variation in the physical and mechanical properties of marine soils with depth, formulas for calculating the safety factor of submarine slopes by an infinite sliding model are established, and the factors affecting slope stability such as soil properties, slope gradient and horizontal seismic action are systematically investigated. Using GIS techniques, the terrain slope gradients and a historical seismic database of the northern South China Sea are obtained. Combined with soil mechanical parameters, a regional stability evaluation of the northern continental slope is carried out. Furthermore, the distribution of risk zones is given. On the whole, under strong seismic action, large-scale submarine slope instability occurs and must be highly considered when assessing risk. This achievement is of great significance to engineering sites, route selection and engineering risk assessment.

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