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Mechanical and electrical properties of coarse-grained soilaffected by cyclic freeze-thaw in high cold regions 被引量:12
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作者 QU Yong-long NI Wan-kui +3 位作者 NIU Fu-jun MU Yan-hu CHEN Guo-liang LUO Jing 《Journal of Central South University》 SCIE EI CAS CSCD 2020年第3期853-866,共14页
To evaluate the geotechnical properties of coarse-grained soil affected by cyclic freeze-thaw,the electrical resistivity and mechanical tests are conducted.The soil specimens are prepared under different water content... To evaluate the geotechnical properties of coarse-grained soil affected by cyclic freeze-thaw,the electrical resistivity and mechanical tests are conducted.The soil specimens are prepared under different water contents,dry densities and exposed to 0?20 freeze-thaw cycles.As a result,the stress?strain behavior of the specimen(w=14.0%andρd=1.90 g/cm^3)changes from strain-hardening into strain-softening due to the freeze-thaw effect.The electrical resistivity of test specimen increases with the freeze-thaw cycles change,but the mechanical parameters(the unconfined compressive strength qu and the deformation modulus E)and brittleness index decrease considerably at the same conditions.All of them tend to be stable after 7?9 cycles.Moreover,both the dry density and the water content have reciprocal effects on the freeze-thaw actions.The failure and pore characteristics of specimens affected by freeze-thaw cycles are discussed by using the image analysis method.Then,an exponential function equation is developed to assess the electrical resistivity of specimens affected by the cyclic freeze-thaw.Linear relations between the mechanical parameters and the electrical resistivity of specimens are established to evaluate the geotechnical properties of the soil exposed to freeze-thaw actions through the corresponding electrical resistivity. 展开更多
关键词 coarse-grained soil freeze-thaw cycle unconfined compressive strength electrical resistivity electrical resistivity model
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冻结粗粒砂岩和中粒砂岩的力学行为及能量演化机制 被引量:4
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作者 屈永龙 杨更社 +3 位作者 奚家米 倪万魁 丁潇 吴丙权 《Journal of Central South University》 SCIE EI CAS CSCD 2023年第6期2018-2034,共17页
复杂地应力和低温环境条件下白垩系弱胶结红砂岩的力学特性和变形本质是西北地区冻结井筒工程安全建设的关键。通过低温单轴和三轴压缩试验,研究了不同低温、不同围压条件下饱和白垩系粗粒砂岩和中粒砂岩的强度和变形特性,查明了冻结砂... 复杂地应力和低温环境条件下白垩系弱胶结红砂岩的力学特性和变形本质是西北地区冻结井筒工程安全建设的关键。通过低温单轴和三轴压缩试验,研究了不同低温、不同围压条件下饱和白垩系粗粒砂岩和中粒砂岩的强度和变形特性,查明了冻结砂岩加载变形过程中的能量演化规律和影响因素,并基于扫描电镜(SEM)揭示了两种砂岩的微观结构特征。结果表明:冻结白垩系砂岩的应力-应变关系呈应变软化型,其受温度、围压和岩性的影响显著,具有明显的孔隙压密变形阶段;冻结砂岩的三轴压缩强度随着温度和围压的增加分别呈非线性减小和增大规律,且各因素之间相互影响。两种砂岩的弹性模量随着温度的降低而非线性增大,但泊松比的变化与之相反。此外,冻结白垩系弱胶结红砂岩的总应变能、弹性能和耗散能具有不同的演化规律,揭示了冻结砂岩的变形破坏内部机制;基于能量比提出了冻结砂岩的损伤因子,评价了两种冻结砂岩的损伤力学特征。最后,从宏观物理特性和微观结构特征等多角度解释了两种砂岩力学和能量特性差异的内在原因。研究成果将为我国寒区矿山建设和深部地下工程的稳定性控制提供理论依据。 展开更多
关键词 冻结砂岩 低温 力学特性 能量演化 内部机制
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