Pore-network model to quantify internal structure and hydraulic characteristics of randomly packed grains with different morphologies

被引:6
|
作者
Xiong, Yunwu [1 ,2 ]
Dong, Li [1 ]
Long, Xiaoxu [1 ]
Chen, Minghong [1 ]
Huang, Guanhua [1 ,2 ]
机构
[1] China Agr Univ, Coll Water Resources & Civil Engn, Ctr Agr Water Res China, Beijing 100083, Peoples R China
[2] China Agr Univ, Chinese Israeli Int Ctr Res & Training Agr, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
Fourier analysis; X-ray computed tomography; Intrinsic permeability; Hydrodynamic dispersion; Grain angularity; POROUS-MEDIA; CAPILLARY-PRESSURE; TRANSPORT; PERMEABILITY; DIFFUSION; GEOMETRY; DENSITY; SCALE; PRECIPITATION; CONDUCTIVITY;
D O I
10.1007/s10035-021-01174-7
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The flow and transport in porous media are highly dependent on the internal structure and morphology of the pore space. The pore structure is determined by the size and geometrical shape of the solid particles, as well as their distribution and arrangement. In this study, the effect of grains surface morphology on the internal pore structure as well as the flow and transport properties of porous media were quantitatively analyzed using the pore-network approach, with angular quartz sand and round glass beads used as the test substrates. The surface morphology of the grains was visualized through scanning electron microscopy and quantified by Fourier morphological analysis. The pore structure of randomly packed quartz sand and glass beads was visualized using X-ray computed tomography and quantified using the network parameters. The surface morphology of grains with different angularities was distinguished by the shape and angularity parameters calculated from the Fourier representations. The network parameters, including mean coordination numbers, mean pore-body radii, and mean pore-throat radii, of randomly packed angular sand were larger than those of round beads within the same sieving size range. The intrinsic permeability and longitudinal dispersivity in the vertical direction were smaller than those in the horizontal direction, which indicates anisotropic compaction. The intrinsic permeability nonlinearly (power-law) varied with the pore and throat radii of the different extracted networks. The relation between intrinsic permeability and porosity of anisotropic porous media with different grain morphologies followed the Kozeny-Carman equations. Breakthrough curves in the representative elementary volumes of angular sand and round beads exhibited Fickian behavior. The longitudinal dispersivity decreased with an increase in the coordination number regardless of the grain morphology. Graphic abstract
引用
收藏
页数:18
相关论文
共 11 条
  • [1] Pore-network model to quantify internal structure and hydraulic characteristics of randomly packed grains with different morphologies
    Yunwu Xiong
    Li Dong
    Xiaoxu Long
    Minghong Chen
    Guanhua Huang
    Granular Matter, 2022, 24
  • [2] Impact of pore structure and morphology on flow and transport characteristics in randomly repacked grains with different angularities
    Xiong, Yunwu
    Long, Xiaoxu
    Huang, Guanhua
    Furman, Alex
    SOILS AND FOUNDATIONS, 2019, 59 (06) : 1992 - 2006
  • [3] Dependency of continuum model parameters on the spatially correlated pore structure studied by pore-network drying simulations
    Lu, X.
    Kharaghani, A.
    Tsotsas, E.
    IDS'2018: 21ST INTERNATIONAL DRYING SYMPOSIUM, 2018, : 307 - 314
  • [4] Using a pore-scale model to quantify the effect of particle re-arrangement on pore structure and hydraulic properties
    Dikinya, Oagile
    Lehmann, Peter
    Hinz, Christoph
    Aylmore, Graham
    HYDROLOGICAL PROCESSES, 2007, 21 (08) : 989 - 997
  • [5] Influence of pore structure parameters on flow characteristics based on a digital rock and the pore network model
    An, Senyou
    Yao, Jun
    Yang, Yongfei
    Zhang, Lei
    Zhao, Jianlin
    Gao, Ying
    JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING, 2016, 31 : 156 - 163
  • [6] Porosity-permeability properties generated with a new 2-parameter 3D hydraulic pore-network model for consolidated and unconsolidated porous media
    Acharya, RC
    van der Zee, SEATM
    Leijnse, A
    ADVANCES IN WATER RESOURCES, 2004, 27 (07) : 707 - 723
  • [7] Variations in the CT-measured pore structure and hydraulic characteristics of coastal saline soils with different reclamation periods
    Han Xiao
    She Dongli
    Sun Xiaoqin
    Fei Yuanhang
    Gao Lei
    JOURNAL OF SOILS AND SEDIMENTS, 2023, 23 (03) : 1332 - 1344
  • [8] Variations in the CT-measured pore structure and hydraulic characteristics of coastal saline soils with different reclamation periods
    Han Xiao
    She Dongli
    Sun Xiaoqin
    Fei Yuanhang
    Gao Lei
    Journal of Soils and Sediments, 2023, 23 : 1332 - 1344
  • [9] Modeling and simulation of the dynamic behavior of monoliths. Effects of pore structure from pore network model analysis and comparison with columns packed with porous spherical particles
    Liapis, AI
    Meyers, JJ
    Crosser, OK
    JOURNAL OF CHROMATOGRAPHY A, 1999, 865 (1-2) : 13 - 25
  • [10] Modeling and simulation of the dynamic behavior of monoliths Effect of pore structure from pore network model analysis and comparison with columns packed with porous spherical particles (vol 865, pg 13, 1999)
    Liapis, AI
    Meyers, JJ
    Crosser, OK
    JOURNAL OF CHROMATOGRAPHY A, 2000, 873 (02) : 301 - 301