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Voronoi杂交渗流通量有限元方法研究

罗超 张蕊 郭然 盖文海

罗超, 张蕊, 郭然, 盖文海. Voronoi杂交渗流通量有限元方法研究[J]. 应用数学和力学, 2026, 47(6): 712-722. doi: 10.21656/1000-0887.460148
引用本文: 罗超, 张蕊, 郭然, 盖文海. Voronoi杂交渗流通量有限元方法研究[J]. 应用数学和力学, 2026, 47(6): 712-722. doi: 10.21656/1000-0887.460148
LUO Chao, ZHANG Rui, GUO Ran, GAI Wenhai. Investigation of a Voronoi-Based Hybrid Seepage Flux Finite Element Method[J]. Applied Mathematics and Mechanics, 2026, 47(6): 712-722. doi: 10.21656/1000-0887.460148
Citation: LUO Chao, ZHANG Rui, GUO Ran, GAI Wenhai. Investigation of a Voronoi-Based Hybrid Seepage Flux Finite Element Method[J]. Applied Mathematics and Mechanics, 2026, 47(6): 712-722. doi: 10.21656/1000-0887.460148

Voronoi杂交渗流通量有限元方法研究

doi: 10.21656/1000-0887.460148
(本刊编委郭然来稿)
基金项目: 

国家自然科学基金 12062007

云南省“兴滇英才”支持计划基金 12072135

详细信息
    作者简介:

    罗超(1997—),男,硕士生(E-mail: 20232110004@stu.kust.edu.cn)

    通讯作者:

    张蕊(1982—),女,教授,博士生导师(通信作者. E-mail: zrui0310@163.com)

  • 中图分类号: O343

Investigation of a Voronoi-Based Hybrid Seepage Flux Finite Element Method

(Contributed by GUO Ran, Member of the Editorial Board of AMM)
  • 摘要: 针对土石混合体和各向异性特征的天然土质坝基,将其视为一种复合多孔介质土体模型,假定渗流为二维Darcy流,水头在土石混合体内连续. 构建了考虑土石界面的非均质土石混合体渗流场和各向异性均质坝基渗流场的杂交渗流通量有限元(HS-FEM)求解模型,该模型在单元域内假设独立的高阶渗流通量变量,同时在单元边界上给定水头值,仅需少数单元即可模拟考虑土石界面的承压渗流工况,避免了传统有限元法在界面处进行密集网格细化的弊端,亦可解决二维正交各向异性稳态线性渗流问题. 验证算例表明:该方法在保持稀疏离散化的前提下,获得了与传统密集网格有限元相当的计算精度.
    1)  (本刊编委郭然来稿)
  • 图  1  单元域划分

    Figure  1.  Unit domain divisions

    图  2  土石混合体模型对比

      为了解释图中的颜色,读者可以参考本文的电子网页版本,后同.

    Figure  2.  Comparison of soil-rock mixture models

    图  3  水头及渗流通量分布云图对比

    Figure  3.  Comparative contour plots of hydraulic head and seepage flux

    图  4  工况条件下的各向异性均质坝基模型

    Figure  4.  The anisotropic homogeneous dam foundation model under operational conditions

    图  5  坝基模型对比

    Figure  5.  Comparison of dam foundation models

    图  6  水头等值线对比

    Figure  6.  Comparison of hydraulic head contours

    图  7  渗流通量云图对比

    Figure  7.  Comparison of seepage flux contours

    图  8  y=58 m渗流通量路径比较

    Figure  8.  Comparison of seepage fluxes paths at y=58 m

    图  9  基函数矩阵P项数对渗流通量qx的影响

    Figure  9.  Influences of the basis function matrix P term number on seepage components qx

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出版历程
  • 收稿日期:  2025-08-19
  • 修回日期:  2025-09-12
  • 刊出日期:  2026-06-01

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