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开挖作用下的节理岩体边坡能量演化规律研究

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为研究在采深及强度折减系数增加情况下的节理岩体边坡能量演化规律。结合现场调查及室内试验结果,利用3DEC建立云南某顺层边坡三维模型,并基于热力学原理及离散单元法对节理岩体边坡能量变化规律及塑性区进行分析。随着采深的增加,弹性应变能、重力势能变化量逐渐下降,耗散能逐渐上升后趋于平缓,动能先上升后下降。随着强度折减系数的增加,弹性应变能、耗散能、重力势能变化量逐渐上升,动能呈现先上升后下降再上升再下降的波动趋势。节理岩体边坡塑性区逐渐扩大,坡顶出现张拉破坏区域,剪切屈服沿结构面、坡面附近贯通分布,边坡整体发生失稳。当采深及强度折减系数增加时,除动能近似保持静力平衡外,边坡其余各项能量均呈现出一定的变化规律。研究结果揭示了边坡发生破坏时各项能量的变化规律,为今后的边坡失稳预警研究提供了新的思路。
Study on the energy evolution law of jointed rock slopes under excavation action
To study the energy evolution of the jointed rock slope under increasing mining depth and strength reduction factor.In this paper,combined with the field investigation and indoor test results,3DEC was used to establish a three-dimensional model of a smooth-layer slope in Yunnan,and the energy and plastic zone of the jointed rock slope based on the principle of thermodynamics and the discrete unit method were analyzed.With the increase of mining depth,the changes of elastic strain energy and gravitational potential energy gradually decreased,the dissipation energy gradually increased and then leveled off,and the kinetic energy firstly increased and then decreased.With the increase of strength reduction coefficient,elastic strain energy,dissipation energy and gravitational potential energy changes gradually rise,and kinetic energy shows a fluctuating trend of firstly rising,then falling,then rising and then falling.The plastic zone of the jointed rock slope gradually expanded,the tensile damage area appeared at the top of the slope,the shear yielding was distributed along the structural surface and near the slope surface through,and the slope was destabilized as a whole.When the mining depth and strength reduction factor increase,except for the kinetic energy to keep the static equilibrium,the rest of the energy of the slope shows a certain rule of change.Significance:This paper reveals the change rule of various energies when slope damage occurs,and provides new ideas for future slope instability early warning research.

gradual slopejointed rockthermodynamicdiscrete element methodmine depthreduction factor

陈祯、陈俊智、任春芳、魏行、杨立新

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昆明理工大学 国土资源工程学院,昆明 650032

顺层边坡 节理岩体 热力学 离散单元法 采深 折减系数

2025

有色金属(矿山部分)
北京矿冶研究总院

有色金属(矿山部分)

影响因子:0.779
ISSN:1671-4172
年,卷(期):2025.77(1)