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饱和级配破碎泥岩压实与粒度分布分形特征试验研究 被引量:23
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作者 郁邦永 陈占清 +2 位作者 吴疆宇 李樯 丁其乐 《岩土力学》 EI CAS CSCD 北大核心 2016年第7期1887-1894,共8页
通过饱和级配破碎泥岩的压实试验,得到了不同级配下试样轴向位移和粒度分布分形维数随轴向应力变化曲线,分析了Talbol幂指数对饱和破碎泥岩压实变形与粒度分布的影响规律,建立了一种饱和破碎泥岩压缩模量与轴向应力的关系式。试验结果表... 通过饱和级配破碎泥岩的压实试验,得到了不同级配下试样轴向位移和粒度分布分形维数随轴向应力变化曲线,分析了Talbol幂指数对饱和破碎泥岩压实变形与粒度分布的影响规律,建立了一种饱和破碎泥岩压缩模量与轴向应力的关系式。试验结果表明,饱和破碎泥岩的压实过程可分为2个阶段,即0~4 MPa的快速变形阶段和4 MPa后的缓慢变形阶段。其中,约80%的变形发生在快速变形阶段。轴向位移、压缩模量与粒度分布分形维数均可用轴向应力的指数函数拟合。相同轴向应力下,Talbol幂指数越大,试样轴向位移越大,粒度分布分形维数越小。轴向应力大于8 MPa后,各级配试样的粒度分布分形维数相差很小,且随着轴向应力的进一步增大,各级配试样的分形维数差异将继续减小,最终,分形维数将趋于一致。在加载初期,试样压实变形主要以岩石颗粒移位为主;而在加载后期,试样的压实变形则以颗粒破碎为主。 展开更多
关键词 饱和破碎泥岩 级配 Talbol幂指 粒度分布分形维数 轴向应力
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不同浸水时间级配破碎煤样的粒度分布分形特征 被引量:8
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作者 张天军 陈佳伟 +3 位作者 包若羽 蒋兴科 周敖 葛迪 《采矿与安全工程学报》 EI CSCD 北大核心 2018年第3期598-604,共7页
含水条件下破碎岩体的变形及压实是引发采空区地表沉降的因素之一。为探究浸水时间、级配、轴向压缩位移3种因素对承载破碎岩体粒度分布分形特征及压实特性的影响规律,采用轴向压缩位移控制的方法,进行了小位移情况下5组不同配比破碎煤... 含水条件下破碎岩体的变形及压实是引发采空区地表沉降的因素之一。为探究浸水时间、级配、轴向压缩位移3种因素对承载破碎岩体粒度分布分形特征及压实特性的影响规律,采用轴向压缩位移控制的方法,进行了小位移情况下5组不同配比破碎煤样的侧限压实试验。结果表明:1)在轴向压缩位移较小的情况下,随着浸水时间的增加,同级配破碎煤样粒度分布分形维数呈减小趋势;2)浸水时间与粒径分布分形维数曲线可用指数函数拟合;3)随着配比指数n的增大,粒度分布分形维数逐渐减小;4)随着轴向压缩位移的增加,同级配破碎煤样粒度分布分形维数与轴向应力都呈增加趋势,可以分为0~15 mm的缓慢增加阶段和15 mm后的快速增加阶段。基于破碎煤样在不同浸水时间条件下承载能力与粒度分布特征的变化规律,得出其承载能力随浸水时间增加而降低,而粒度分布分形维数呈减小趋势,从而为进一步研究破碎岩体承载条件下的强度、变形及粒度分布特征提供依据。 展开更多
关键词 小位移 浸水时间 粒度分布分形维数 级配 破碎煤样
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Characterizations of PSD Fractal of Porous Medium 被引量:3
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作者 黄国强 徐世民 李鑫钢 《Transactions of Tianjin University》 EI CAS 2003年第3期170-173,共4页
A volume-based method for measuring particle-size distribution (PSD) fractal dimensions of porous mediums was developed by employing laser size-analyzing technology. Compared with conventional approaches of using hydr... A volume-based method for measuring particle-size distribution (PSD) fractal dimensions of porous mediums was developed by employing laser size-analyzing technology. Compared with conventional approaches of using hydrometer or screen to determine PSD, this method can avoid calculation errors and measure smaller size-scale porous medium. In this paper the experimental porous mediums were brown soil, kaolin and sand soil. A micro-order of magnitude (10 -5 m) in particle-size interval could be shown in PSD results of brown soil and kaolin. The experiments indicated that brown soil had a nearly mono-fractal PSD character, while kaolin and sand soil showed multi-fractal PSD characters. By the adsorption isotherm experiments, the PSD fractal dimensions of the sand soil were also found to keep a linearly increasing relation with the linear adsorptive parameters of the soils in different intervals to adsorb benzene from aqueous solution. 展开更多
关键词 FRACTAL porous medium particle-size distribution ADSORPTION
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Steady-State Properties of Driven Polydisperse Granular Mixtures
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作者 李睿 张端明 +1 位作者 肖明 李志浩 《Communications in Theoretical Physics》 SCIE CAS CSCD 2011年第12期1145-1148,共4页
We represent a two-dimensional model of polydisperse granular mixtures with a power-law size distribution. The model consists of smooth hard disks in a rectangular box with inelastic collisions,driven by a homogeneous... We represent a two-dimensional model of polydisperse granular mixtures with a power-law size distribution. The model consists of smooth hard disks in a rectangular box with inelastic collisions,driven by a homogeneous heat bath at zero gravity.The width of particle size distribution is characterized by the only parameter,namely,the fractal dimension D.The energy dissipation of the mixture is increased as D increases or as e decreases.Furthermore,it is found that the steady-state properties of the mixture such as the collision rate,granular temperature,kinetic pressure and velocity distribution depend sensitively on size distribution parameter D. 展开更多
关键词 fractal dimension polydisperse mixtures
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Temperature Properties in Polydisperse Granular Mixtures
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作者 李睿 肖明 +1 位作者 李志浩 张端明 《Communications in Theoretical Physics》 SCIE CAS CSCD 2013年第2期229-232,共4页
Numerical simulations are employed to consider the problem of determining the granular temperatures of the species of a homogeneous heated granular mixture with a power-law size distribution. The partial granular temp... Numerical simulations are employed to consider the problem of determining the granular temperatures of the species of a homogeneous heated granular mixture with a power-law size distribution. The partial granular temperature ratios are studied as functions of the fractal dimension D, the restitution coefflcient e, the rescaled viscosity time, the average occupied area fraction φ, the total particle number N and the number fraction. Different species of particles in a power-law system typically do not have the same mean kinetic energy, namely the granular temperature. It is found that the extent of nonequipartition of kinetic energy is determined by the fractal dimension D, the restitution coemcient e and the rescaled viscosity time, while is insensitive to the total particle number N, the area fraction φ and the number fraction. 展开更多
关键词 nonequipartition granular temperature continuous size
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