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循环载荷下破碎煤体渗透率及迂曲度演化研究

张天军 田嘉伟 张磊 庞明坤 潘红宇 孟伟 贺绥男

岩土力学2025,Vol.46Issue(5):1409-1418,1428,11.
岩土力学2025,Vol.46Issue(5):1409-1418,1428,11.DOI:10.16285/j.rsm.2024.0894

循环载荷下破碎煤体渗透率及迂曲度演化研究

Permeability and tortuosity evolution of crushed coal under cyclic loading

张天军 1田嘉伟 1张磊 1庞明坤 2潘红宇 2孟伟 1贺绥男1

作者信息

  • 1. 西安科技大学安全科学与工程学院,陕西西安 710054
  • 2. 西安科技大学安全科学与工程学院,陕西西安 710054||西安科技大学能源学院,陕西西安 710054
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摘要

Abstract

Cyclic loading significantly affects coal seepage;however,the quantitative characterization of seepage channels in fractured coal under cyclic loading is inadequate,and a matrix structure model for the fractured coal is absent.Therefore,seepage tests involving pore pressure and confining pressure cyclic loading were conducted on fractured coal with different grading conditions.The results indicate:1)Under both pore pressure and confining pressure cyclic loading,the initial permeability of the coal mass varies with grading.As the Talbol power exponent increases,permeability successively increases,exhibiting clear stratification.2)The sensitivity of effective stress to permeability K under cyclic loading is represented by effective stress variation △σSe.It is observed that the value of △σSc decreases in an"L-shaped"manner as permeability K increases during pore pressure cyclic loading.When K≤0.75×10-12m2,the smaller Talbol power exponent corresponds to a lower the value of △σSe is.3)A method to calculate the average seepage pore area of graded coal is proposed,and a tortuosity model is developed to describe the evolution of tortuosity in fractured coal under cyclic loading.This research provides a theoretical basis for understanding the permeability evolution mechanism of fractured coal under cyclic loading and establishing a seepage model.

关键词

渗透率/循环载荷/有效应力/敏感系数/迂曲度模型

Key words

permeability/cyclic loading/effective stress/sensitivity coefficient/tortuosity model

分类

矿山工程

引用本文复制引用

张天军,田嘉伟,张磊,庞明坤,潘红宇,孟伟,贺绥男..循环载荷下破碎煤体渗透率及迂曲度演化研究[J].岩土力学,2025,46(5):1409-1418,1428,11.

基金项目

国家自然科学基金项目(No.52374228) (No.52374228)

国家自然科学基金青年基金项目(No.52104216,No.52304253).This work was supported by the National Natural Science Foundation of China(52374228)and the National Natural Science Foundation for Young Scientists of China(52104216,52304253). (No.52104216,No.52304253)

岩土力学

OA北大核心

1000-7598

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