Lattice Boltzmann meso-seepage research of reconstructed soil based on the quartet structure generation set

• Published in: Shuiwen Dizhi Gongcheng Dizhi Vol. 49; no. 2; pp. 33 - 42
• Main Authors: Peichen CAI, Yun QUE, Zhenliang JIANG, Pengfei YANG
• Format: Journal Article
• Language: Chinese
• Published: Editorial Office of Hydrogeology & Engineering Geology 01.03.2022
• Subjects: lattice boltzmann; meso-seepage; permeability; quartet structure generation set; soil particle size
• ISSN: 1000-3665
• DOI: 10.16030/j.cnki.issn.1000-3665.202106036

Reconstruction of the porous media model is the basis and key to the study of the meso-seepage mechanism of soil. The soil models are constructed by the quartet structure generation set (QSGS), and the lattice Boltzmann method (LBM) is used to examine the meso-seepage mechanism of the reconstructed soil under different conditions through MATLAB self-programming. The results show that the degree of pore connectivity increases significantly as the model size increases. The 300×300 grid size model has the largest increase in the connected porosity (34.38%). If the model size continues to be expanded, the increase is not obvious. Fluid particles can form the main seepage channel in the area with good pore connectivity and large pore size, and there is a fingering effect. The flow velocity in the middle of the pore channel is the largest, up to 0.0324. The flow velocity is getting smaller and smaller when it gets closer and closer to the pore wall. The velocity of the large porosity soil is larger than that of the