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梁越, 陈亮, 陈建生. 考虑流固耦合作用的管涌发展数学模型研究[J]. 岩土工程学报, 2011, 33(8): 1265-1270.
引用本文: 梁越, 陈亮, 陈建生. 考虑流固耦合作用的管涌发展数学模型研究[J]. 岩土工程学报, 2011, 33(8): 1265-1270.
LIANG Yue, CHEN Liang, CHEN Jian-sheng. Mathematical model for piping development considering fluid-solid interaction[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(8): 1265-1270.
Citation: LIANG Yue, CHEN Liang, CHEN Jian-sheng. Mathematical model for piping development considering fluid-solid interaction[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(8): 1265-1270.

考虑流固耦合作用的管涌发展数学模型研究

Mathematical model for piping development considering fluid-solid interaction

  • 摘要: 根据质量守恒定律,针对单元体中移动颗粒的质量守恒,得到了管涌过程中移动颗粒的连续性方程;颗粒的运动与流体的流动相互关联,结合渗流的连续性方程,得到了管涌发展过程中的流固耦合模型;根据颗粒流失与渗流场变化的相互关系,对渗透系数、单位流失量、孔隙率等参数的联系进行量化,结合初始条件与边界条件,即可实现耦合模型的求解。最后,针对一维管涌情况,利用分时步法对模型进行解耦,以有限差分法对模型进行离散并成功求解,分析了管涌过程中颗粒流失、流速、孔隙率以及剩余颗粒量等参数的变化规律;在不同水力梯度下进行重复试验,分析了水力梯度在管涌发展中对各参数变化规律的影响。

     

    Abstract: Based on the law of conservation of mass, the conservation of mass of transporting particles in the cell body is determined, from which a continuity equation of the transporting particles is derived. Particle transporting is associated with the fluid flow. So the calculation should combine the continuity equation of flow in the seepage field. Then a fluid-solid interaction model is proposed. Based on the relations between the particle loss and the change of the seepage field, the relationship among the permeability coefficient, losses quantity, porosity and other parameters is quantified. The coupled model can be solved combined with the initial conditions and boundary conditions. Finally, a one-dimensional piping problem is simulated by means of the proposed model. Decoupled by a time-step method, the model is solved successfully by use of the finite difference method. From the calculated results, the variations of the particle loss, seepage velocity, porosity and the remaining particle volume in the piping proceeding are analyzed. The impact of the hydraulic gradient is discussed as well with repeated calculation under different hydraulic gradients.

     

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