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首页> 外文期刊>Advances in civil engineering >Brittle Characteristic and Microstructure of Sandstone under Freezing-Thawing Weathering
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Brittle Characteristic and Microstructure of Sandstone under Freezing-Thawing Weathering

机译:冷冻解冻风化下砂岩脆性特征和微观结构

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摘要

As an important property of rock material, brittleness plays a vital role in rock engineering. This paper raised the concept of elastic strain energy release rate and proposed an elastic strain energy release rate based brittleness index based on the most acceptable definition of brittleness. Mechanical and Nuclear Magnetic Resonance parameters of sandstone under various Freezing-Thawing (F-T) cycles are also acquired and analyzed. Then, the proposed brittleness index is used to compare with two recently proposed brittleness indices to verify its correctness and applicability. Finally, the brittleness index is applied to evaluate the brittle behavior of F-T cycles treated sandstone under uniaxial compression. The results show that elastic modulus, value of the postpeak modulus, and peak stress decrease with F-T cycles, and the porosity and microstructure develop with F-T cycles. The proposed brittleness index is highly related to F-T cycles, peak stress, porosity, and elastic modulus of sandstone that suffered recurrent F-T cycles. It declines exponentially with F-T cycles and porosity increase while growing exponentially with peak stress and elastic modulus increase.
机译:作为岩石材料的重要特性,脆性在岩石工程中起着至关重要的作用。本文提出了弹性应变能释放速率的概念,提出了基于脆性最可接受的脆性的弹性应变能释放率的脆性指数。还获取和分析了各种冻融(F-T)循环下的砂岩机械和核磁共振参数(F-T)循环。然后,建议的脆性指数用于与最近提出的两个脆性指数进行比较,以验证其正确性和适用性。最后,应用脆性指数来评估单轴压缩下F-T循环处理砂岩的脆性行为。结果表明,随着F-T循环的弹性模量,后斑量模的值和峰值应力降低,并且具有F-T循环的孔隙率和微观结构。所提出的脆性指数与遭受复发的F-T循环的砂岩的F-T循环,峰值应力,孔隙度和弹性模量高。它在峰值应力和弹性模量增加的同时呈指数增长的循环和孔隙率呈指数下降。

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