Study on seepage characteristics of 3D fracture network of rock mass based on equivalent pipe network

被引:0
|
作者
Li G. [1 ]
Luo C. [1 ]
Wu X. [1 ]
Liu H. [1 ]
机构
[1] School of Civil and Transportation Engineering, Henan University of Urban Construction, Pingdingshan
基金
中国国家自然科学基金;
关键词
Equivalent path permeability coefficient(EPC); Fracture connection path; Gas drainage; Representative element volume(Rev); Rock fracture;
D O I
10.13199/j.cnki.cst.2021.10.012
中图分类号
学科分类号
摘要
The lower rock mass is filled with fissures, which is of great significance for oil and gas resource development, groundwater resource utilization, pollutant migration, carbon dioxide storage, and nuclear waste geological disposal. Nuclear waste repository has extremely strict requirements for geological environment. However, the natural fractures in rock mass may be the potential channel for nuclide migration. Therefore, it is necessary to evaluate the impact of fractures on rock permeability. In general, there are three methods to analyze the fracture connectivity and seepage characteristics through the disc-shaped fracture network seepage model: the finite element method; the discrete element method; the DFN is converted into a plane crack with similar network pipes with effective connectivity and hydraulic characteristics are also called “pipe network models”. In this paper, the granite outcrop of Xinchang high-level radioactive waste repository in China is studied. Variable-section equivalent pipes to simulate the permeability characteristics of rock fractures is used. The complex fissure disk network is equivalent to a pipe network model. An equivalent path permeability coefficient is proposed to objectively study the permeability characteristics of the seepage path of the fractured rock mass. When the fresh fractures are exposed to a certain depth by cutting the surface rocks, some fractures in the strike range belong to open type, others belong to the cemented closed type. The calculation results of equivalent path permeability coefficient under different conditions show that the average values of equivalent path permeability coefficient are 10-7 m/s and 10-3 m/s respectively when the fracture is cemented and partially cemented. On this basis, the representative unit volume(REV) of fissured rock mass in the study area is determined to be about 25 m3. Through the matrix in the rotation model, the spatial permeability tensor(including permeability value and main direction) of the area is obtained, and the predicted results are within the range of borehole data, which can provide reference for related projects. © 2021 Meitan Kexun Jishu/Coal Science and Technology (Peking). All rights reserve.
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页码:85 / 90
页数:5
相关论文
共 21 条
  • [1] CHEN S, FENG X, ISAM S., Numerical estimation of rev and permeability tensor for fractured rock masses by composite element method, International Journal for Numerical and Analytical Methods in Geomechanics, 32, 12, pp. 1459-1477, (2010)
  • [2] SHI Zhijun, YAO Ke, YAO Ningping, Et al., Development and rospect of underground tunnel drilling technology and equipment in China for 40 years[J], Coal Science and Technology, 48, 4, pp. 1-34, (2020)
  • [3] ZHANG Pingsong, XU Shiang, GUO Liquan, Et al., Research progress and prospect of monitoring technology for deformation and failure of surrounding rock in stope, Coal Science and Technology, 48, 3, pp. 14-48, (2020)
  • [4] GOC R L, DREUZY J R D, DAVY P., An inverse problem methodology to identify flow channels in fractured media using synthetic steady-state head and geometricaldata, Advances in Water Resources, 33, 7, pp. 782-800, (2010)
  • [5] HANEBERG W C., Using close range terrestrial digital photogrammetry for 3-d rock slope modeling and fracture mapping in the unitedstates, Bulletin of Engineering Geology and the Environment, 67, 4, pp. 457-469, (2008)
  • [6] NEUMAN S P., Trends, prospects and challenges in quantifying flow and transport through fracturedrocks, Hydrogeology Journal, 13, 1, pp. 124-147, (2005)
  • [7] GUO L, LI X, ZHOU Y, Et al., Generation and verification of threedimensional network of fractured rock masses stochastic discontinuities based on digitalization, Environmental Earth Sciences, 73, 11, pp. 7075-7088, (2015)
  • [8] KARRA S O, MALLEY D, HYMAN J, Et al., Modeling flow and transport in fracture networks using graphs, Physical Review, 97, 3, pp. 33-40, (2018)
  • [9] WANG M, KULATILAKE Phsw, UM J, Et al., Estimation of rev size and three - dimensional hydraulic conductivity tensor for a fractured rock mass through a single well packer test and discrete fracture fluid flow modeling, International Journal of Rock Mechanics and Mining Sciences, 39, 7, pp. 887-904, (2002)
  • [10] TSANG Y, TSANG C., Flow channeling in a single fracture as a two-dimensional strongly heterogeneous permeable medium, Water Resources Research, 25, 9, pp. 2076-2080, (1989)