首页|天然含水与饱和状态砂岩静力学特性三轴试验研究

天然含水与饱和状态砂岩静力学特性三轴试验研究

Triaxial test study on static properties of sandstone with natural moisture content and saturation state

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通过开展不同围压条件下三轴压缩试验,研究了天然含水与饱和状态下中风化砂岩的静力学特性,探讨了试样从天然含水到饱和的状态变化对其强度参数、峰值应力、峰值应变及弹性模量的影响规律.试验结果表明,当中风化砂岩试样从天然含水状态转变为饱和状态时,其峰值应力和峰值应变降低,但弹性模量几乎无变化.基于侧向应变响应(LSR)法,通过测量试样体应变最大时的应力值,确定了天然含水及饱和状态下中风化岩石的裂纹损伤应力.分析表明砂岩试样裂纹损伤应力约为起裂应力的2倍,且为峰值应力的60%~95%.随着围压增大,砂岩破坏后的主裂隙逐渐从竖向分布转变为水平向分布.
This paper investigates the mechanical properties of natural moist and saturated moderately weathered sandstone through triaxial compression tests.The study analyzes the effects of transitioning from a natural moist state to a saturated state on key parameters such as sample strength,peak stress,peak strain,and elastic modulus.The experimental results indicate that when the sample changes from a natural to a saturated state,both peak stress and peak strain decrease,while the elastic modulus remains unchanged.Using the lateral strain response(LSR)method,the stress value associated with crack propagation in both natural and saturated moderately weathered sandstone samples is determined by measuring the stress magnitude at maximum volumetric strain.The stress associated with crack propagation is found to be approximately twice that corresponding to crack initiation and ranges between 60%and 95%times the peak stress.Additionally,as confining pressure increases,the primary fracture orientation during the post-failure stage shifts from vertical to horizontal.

moderately weathered sandstonemechanical propertiytriaxial testfailure characteristics

刘烈帅、刘先林、邵羽、唐正辉、薛大为、吕玺琳

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同济大学土木工程学院,上海 200092

广西交通设计集团有限公司,广西南宁 530029

同济大学岩土及地下工程教育部重点实验室,上海 200092

中风化砂岩 力学特性 三轴试验 破坏特征

2024

广西大学学报(自然科学版)
广西大学

广西大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.767
ISSN:1001-7445
年,卷(期):2024.49(6)