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Sandstone Dynamical Characteristics Influenced by Water-Rock Interaction of Bank Slope

机译:岸坡水岩相互作用对砂岩动力特性的影响

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During the long-term reservoir operation, the seismic capability and dynamic response characteristics of the bank slope are of great importance to its safety evaluation content. Aimed at typical bank slopes, considering reservoir water level fluctuation and soaking-air drying cyclic interaction, an experiment has been designed and conducted. In addition, the cyclic loading test with different stress amplitudes was carried out in different water-rock cycles. The laboratory results indicate that (1) during the immersion-air dry circulation process, the damping ratio and damping coefficient of sandstone gradually increased while the dynamic elastic modulus decreased. It is obvious that the dynamic elastic modulus of sandstone decreases dramatically during the immersion-air dry circulation process, especially in the first six periods. Also, its variation curve fits with the logarithmic curve. (2) When the cyclic load stress amplitude increases from 10MPa to 35MPa, the damping ratio and coefficient of the rock sample gradually decreased while dynamic elastic modulus increased. each dynamic parameter shows a more obvious variation trend when the stress amplitude is lower than 25MPa. (3) During the water-rock interaction process, the closely knit microstructure of rock gradually becomes loose and porous, which resulted in the degradation of macroscopic physical and mechanical properties of sandstone. (4) In the analysis of the seismic response of the bank slope, the actual water-rock interaction process and the seismic level of the bank slope should be more considered. To find out further accurate reflection in the earthquake resistance and dynamic response of the bank slope, it is necessary to select the reasonable dynamic parameter to carry out seismic research.
机译:在长期储层作业中,岸坡的抗震能力和动力响应特性对其安全评价内容具有重要意义。针对典型的岸坡,考虑水库水位的波动和浸泡空气干燥循环的相互作用,设计并进行了试验。另外,在不同的水岩循环中进行了不同应力幅值的循环荷载试验。实验结果表明:(1)在浸入式空气干循环过程中,砂岩的阻尼比和阻尼系数逐渐增大,而动弹性模量减小。显然,砂岩的动态弹性模量在浸入空气干循环过程中会急剧下降,特别是在前六个时期。而且,其变化曲线与对数曲线吻合。 (2)当循环载荷应力幅值从10MPa增加到35MPa时,岩石样品的阻尼比和系数逐渐减小,而动弹性模量则增加。当应力幅值小于25MPa时,各动态参数的变化趋势更加明显。 (3)在水-岩相互作用过程中,紧密结合的岩石微观结构逐渐变得疏松多孔,导致砂岩宏观物理力学性能下降。 (4)在对岸坡地震反应的分析中,应考虑实际的水岩相互作用过程和岸坡的地震水平。为了进一步准确地反映出岸坡的抗震性和动力响应,有必要选择合理的动力参数进行地震研究。

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