土工基础 ›› 2025, Vol. 39 ›› Issue (4): 580-585.

• 专题论述 • 上一篇    下一篇

海底原位探杆贯入的离散元模拟

施榕俊1,刘宜胜1,张国堙2   

  1. (1.浙江理工大学 机械工程学院,杭州 310018;2.自然资源部第二海洋研究所,杭州 310027)
  • 收稿日期:2023-06-27 修回日期:2023-07-04 出版日期:2025-08-31 发布日期:2025-08-27
  • 通讯作者: 刘宜胜(1979-),男,博士,副教授,研究方向为海洋海底探测装备。
  • 作者简介:施榕俊(1997-),男,硕士研究生,研究方向为海洋海底探测装备。
  • 基金资助:
    浙江省重点研发计划(2021C03016)

Discrete Element Simulation of Seabed In-Situ Cone Penetration Test

SHI Rongjun1, LIU Yisheng1, ZHANG Guoyin2   

  1. (1.School of Mechanical Engineering, Zhejiang Science and Technology University, Hangzhou 310018;
    2.Second Institute of Oceanography, MNR, Hangzhou 310027)
  • Received:2023-06-27 Revised:2023-07-04 Online:2025-08-31 Published:2025-08-27

摘要: 海底探杆贯入是一种应用广泛的海底原位测试方法。基于离散元法,对探杆贯入海底土体的原位测量过程进行离散元模型模拟分析。分别采用添加土颗粒浮力与单向流固耦合两种方式模拟海底土壤的水下饱和状态,建立干砂与两种饱和土设置的表层贯入模型,并针对深层贯入,建立采用单向流固耦合方法的200 m土层深度贯入模型。数值模拟结果表明,探杆贯入饱和土的土颗粒响应在锥尖阻力、颗粒应力等力相关结果方面与非饱和土存在较大差异;单向流固耦合方法较添加土颗粒浮力可以更好模拟土壤水下饱和状态,在锥尖阻力方面,仅考虑土颗粒浮力会产生9%的差别;在探杆的表层贯入与深层贯入中,土颗粒大应力集中在探杆锥尖等位置,土颗粒位移、旋转等相关土体扰动主要发生在距锥身一个探杆直径范围当中。


关键词: 离散元, 数值模拟, 单向流固耦合, 饱和土, 原位测试

Abstract: The submarine cone penetration test (CPT) is a widely used insitu test method on the seabed. Based on the discrete element method, a discrete element model is used to simulate and analyze the in-situ measurement process of the probe penetrating the seabed soil. The underwater saturation state of the seabed soil is simulated by adding soil particle buoyancy and one-way fluid-solid coupling respectively, as well as the surface penetration model of the dry sand and two saturated soils are established. For the deep penetration, a 200 m soil depth penetration model using one-way fluid-solid coupling method is established. The numerical simulation results show that the soil particle response of the probe penetrating the saturated soil is significantly different from that of the unsaturated soil in terms of the force-related results such as tip resistance and the particle stress. The one-way fluid-solid coupling method can better simulate the underwater saturation state of the soil than adding soil particle buoyancy. In terms of tip resistance, only considering the buoyancy of soil particles will produce a difference of 9 %. In the surface penetration and deep penetration of the probe rod, the large stress of the soil particles is concentrated at the cone tip of the probe rod, and the related soil disturbance such as the displacement and rotation of the soil particles mainly occurs within a diameter range of the probe rod from the cone shaft.

Key words: Discrete Element Method, Numerical Simulation, One-Way Fluid-Solid Coupling, Saturated Soil, In-Situ Test

中图分类号: