Creep behavior of dry and saturated medium-grain sandstone and its relationship with conventional mechanical properties

IF 3.9 2区 工程技术 Q3 ENERGY & FUELS Geomechanics and Geophysics for Geo-Energy and Geo-Resources Pub Date : 2024-02-22 DOI:10.1007/s40948-024-00771-z
Qingheng Gu, Yunliang Tan, Guangming Zhao, Xiangrui Meng, Xiang Cheng
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Abstract

With the large scale mining of coal and the increase of abandoned goafs under weakly cemented aquifer strata in Western China, it is urgent to study the time dependent mechanical properties of water sensitive aquifer strata. In this paper, creep behavior of dry and saturated medium-grain sandstone, which represent two limit states affected by water, were studied and compared. The results showed that water greatly weakens the compressive strength of medium-grained sandstone, but the difference in axial strain between dry and saturated rock samples decreases with the increase of confining pressure. The creep compression volume of rocks decreases with the increase of deviatoric stress, and only under low confining pressure does the creep volume of rocks exhibit expansion. There is an order of magnitude difference in creep strain between medium grained sandstone and other common rocks. The instantaneous elastic modulus has a negative exponential relationship with deviating stress. The creep rate has a positive exponential relationship with deviating stress. Based on Burges model with exponential damage variables, the law of the influence of confining pressure on creep model parameters has been discussed. The linear relationship between elastic modulus of medium-grained sandstone and parameters of Burgers model with damage was found. The research results are conducive to the convenient prediction of creep behavior of medium grained sandstone engineering and the long-term stability control of the surrounding rock.

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干燥和饱和中粒砂岩的蠕变行为及其与常规力学性能的关系
随着中国西部地区煤炭的大规模开采和弱胶结含水层下废弃岩体的增加,研究水敏感含水层地层的时间相关力学性质迫在眉睫。本文对代表受水影响两种极限状态的干燥中粒砂岩和饱和中粒砂岩的蠕变行为进行了研究和对比。结果表明,水极大地削弱了中粒砂岩的抗压强度,但干燥岩石样本与饱和岩石样本之间的轴向应变差异随着约束压力的增加而减小。岩石的蠕变压缩量随偏差应力的增加而减小,只有在低约束压力下,岩石的蠕变体积才会膨胀。中粒砂岩与其他普通岩石的蠕变应变相差一个数量级。瞬时弹性模量与偏差应力呈负指数关系。蠕变速率与偏差应力呈正指数关系。根据具有指数破坏变量的 Burges 模型,讨论了约束压力对蠕变模型参数的影响规律。发现中粒砂岩的弹性模量与布尔格斯模型参数之间存在线性关系。研究成果有利于方便地预测中粒砂岩工程的蠕变行为和围岩的长期稳定性控制。
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来源期刊
Geomechanics and Geophysics for Geo-Energy and Geo-Resources
Geomechanics and Geophysics for Geo-Energy and Geo-Resources Earth and Planetary Sciences-Geophysics
CiteScore
6.40
自引率
16.00%
发文量
163
期刊介绍: This journal offers original research, new developments, and case studies in geomechanics and geophysics, focused on energy and resources in Earth’s subsurface. Covers theory, experimental results, numerical methods, modeling, engineering, technology and more.
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