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Study on Damage Evolution Law of Rock Mechanics Parameters Under Water-Rock Interaction

机译:水-岩相互作用下岩石力学参数的损伤演化规律研究

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The open pit locating in Cangshang was closed in 2005 because the reusing of pumping water resulted in the cyclic change of slope water level. In order to study the influence of water level fluctuation on mechanics parameters of the slope rocks, two kinds of typical rocks are selected to have the uniaxial compression tests of different saturation-dehydration circulation. The damage evolution law of rock mechanics parameters under water-rock interaction is found, whose results show that the mechanical properties of rock are weakened obviously by the water-rock interaction. In addition, the stronger the water-rock interaction becomes, the more obvious the weakening phenomenon is. Due to the different sensitivity to various parameters of water-rock interaction, the extent of elastic modulus decrease is the largest and uniaxial anti-compressive strength takes the second place while Poisson's ratio is essentially constant. Moreover, the uniaxial compressive strength and modulus of elasticity present exponential distribution with times of saturation-dehydration circulation. With the increase of the saturationdehydration times, the damage value increases accordingly while the increment tends to zero. Generally, the rock mechanical properties are hardly affected by water-rock interaction in the latter period; there are differences among the damage degree of various qualities of rocks, the better the quality, the smaller the damage, and the less the times reaching 95% limit damage value.
机译:仓上露天矿于2005年关闭,因为抽水的再利用导致坡度水位的周期性变化。为了研究水位波动对边坡岩体力学参数的影响,选取两种典型岩体进行了不同饱和-脱水循环的单轴压缩试验。发现了水-岩相互作用下岩石力学参数的损伤演化规律,其结果表明,水-岩相互作用显着削弱了岩石的力学性能。另外,水岩相互作用越强,减弱现象越明显。由于对水-岩相互作用各种参数的敏感性不同,弹性模量下降的幅度最大,而单轴抗压强度次之,而泊松比则基本恒定。而且,单轴抗压强度和弹性模量随饱和-脱水循环次数呈指数分布。随着饱和脱水时间的增加,损伤值相应增加,而增加趋于零。通常,在后期,岩石的力学性能几乎不受水-岩石相互作用的影响。各种岩石的损伤程度之间存在差异,质量越好,损伤越小,达到95%极限损伤值的次数越少。

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