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深部煤层力学各向异性特征与深度效应OA

Mechanical anisotropy and depth effects of deep coal seams

中文摘要英文摘要

[目的]煤层力学性质控制深部煤储层稳定性、可改造性和压裂效果.随埋深增加,煤体所受地应力增强,深部煤在损伤行为、关键力学参数和破裂机制上区别于浅部煤,并表现出显著力学各向异性.[方法]以鄂尔多斯盆地东缘临县地区9号煤为研究对象,开展60 ℃、不同围压条件下的三轴压缩各向异性试验.通过比较面割理方向、端割理方向和垂直层理方向煤样的全应力-应变曲线、关键力学参数和破坏模式,揭示深部煤层力学响应的围压效应与方向差异,并构建相应的各向异性破坏判据.[结果和结论]结果表明:在围压0、20 MPa条件下,煤样弹性阶段线性特征明显,进入塑性阶段后应变快速增长,破坏以张拉劈裂为主;在围压30~60 MPa条件下,应力-应变曲线斜率增大,破坏模式由张拉主导向剪切主导转变.三方向对比显示,煤样变形能力由强到弱依次为垂直层理方向、端割理方向和面割理方向;强度与刚度则整体表现为面割理方向最高、端割理方向次之、垂直层理方向最低.抗压强度、残余强度和弹性模量总体随围压升高而增加,高围压阶段增幅趋缓;泊松比整体呈减小趋势,但具有一定离散性.相关性分析表明,弹性模量和残余强度与抗压强度呈正相关,泊松比与抗压强度的关系具有明显方向差异.基于三方向三轴压缩数据和Mohr-Coulomb剪切破坏准则,确定了不同方向的内摩擦角与黏聚力参数,并建立了深部煤层各向异性剪切破坏准则.研究结果表明,深部应力水平升高会增强煤层承载能力并改变破坏方式,但结构方向差异仍然显著.所得结果可为深部煤储层稳定性分析、可改造性评价、压裂参数设计和剪切破坏判定提供力学依据.

[Objective]The mechanical properties of coal seams determine the stability,fracability,and fracturing per-formance of deep coal reservoirs.Since the in situ stress applied to coal increases with burial depth,deep coal differs from its shallow counterpart in damage behavior,key mechanical parameters,and failure mechanism.Furthermore,deep coal exhibits pronounced mechanical anisotropy.[Methods]Focusing on the No.9 coal seam in the Linxian area along the eastern margin of the Ordos Basin,this study carried out triaxial compression tests at 60℃ under different confining pressures to determine the mechanical anisotropy of deep coal.By comparing the full stress-strain curves,key mechanic-al parameters,and failure modes of coal specimens with sampling directions parallel to face cleats,parallel to butt cleats,and perpendicular to beddings,this study revealed the confining-pressure effects and directional differences in the mech-anical responses of deep coal.In addition,the anisotropic failure criterion for deep coal was established.[Results and Conclusions]The results indicate that,under confining pressures of 0 MPa and 20 MPa,the coal specimens showed dis-tinct linear stress-strain relationships in the elastic deformation stage and then underwent rapidly growing strain in the plastic deformation stage,with coal failure dominated by tensile splitting.Under confining pressures ranging from 30 MPa to 60 MPa,the slopes of the stress-strain curves increased,with the failure mode shifting from tensile-dominated to shear-dominated failure.Comparison reveals that the deformability of the coal specimens with three sampling directions decreased in the order of bedding-perpendicular,butt-cleat-parallel,and face-cleat-parallel directions,while their strength and stiffness decreased in the order of face-cleat-parallel,butt-cleat-parallel,and bedding-perpendicular direc-tions.The compressive strength,residual strength,and elastic modulus of the coal specimens generally increased as the confining pressure rose,with amplitudes increasing at lower rates under high confining pressures.The Poisson's ratios of the coal specimens showed an overall downward trend but dispersed to some extent.Correlation analysis indicates that the elastic modulus and residual strength of the coal specimens were positively correlated with their compressive strength,while the relationship between the Poisson's ratio and compressive strength of the samples exhibited pro-nounced directional differences.Based on triaxial compression data in the three sampling directions and the Mohr-Cou-lomb shear failure criterion,this study determined the internal friction angles and cohesion in different directions and es-tablished an anisotropic shear failure criterion for deep coal.The results indicate that increasing deep in situ stress would enhance the load-bearing capacity of the coal seam and change its failure mode,while directional mechanical differ-ences remained significant.The results of this study will provide a mechanical basis for the stability analysis,fracability evaluation,fracturing parameter design,and shear failure determination of deep coal reservoirs.

梅小凡;王聪;王凯峰;唐书恒;张松航;郗兆栋

中国地质大学(北京)能源学院,北京 100083中国地质大学(北京)能源学院,北京 100083||山西省煤系矿产综合勘查技术创新中心,山西太原 030000中海油研究总院有限责任公司,北京 100028中国地质大学(北京)能源学院,北京 100083||山西省煤系矿产综合勘查技术创新中心,山西太原 030000中国地质大学(北京)能源学院,北京 100083||山西省煤系矿产综合勘查技术创新中心,山西太原 030000中国地质大学(北京)能源学院,北京 100083||山西省煤系矿产综合勘查技术创新中心,山西太原 030000

天文与地球科学

深部煤层力学各向异性深度效应高温三轴压缩试验摩尔-库仑剪切破坏准则

deep coal seammechanical anisotropydepth effecthigh-temperature triaxial compression testMohr-Cou-lomb shear failure criterion

《煤田地质与勘探》 2026 (9)

116-128,13

国家自然科学基金项目(42430805)山西省中央引导地方科技发展资金项目(YDZJSX2025D083)

10.12363/issn.1001-1986.26.03.0120

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