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饱和砂岩的黏弹行为的实验研究
引用本文:席道瑛,徐松林,席军,易良坤,杜赘.饱和砂岩的黏弹行为的实验研究[J].地球物理学报,2011,54(9):2302-2308.
作者姓名:席道瑛  徐松林  席军  易良坤  杜赘
作者单位:1. 中国科学技术大学蒙城地球物理国家野外观测站 地球和空间科学学院,合肥 230026; 2. 中国科学技术大学 中国科学院材料力学行为和设计重点实验窒,合肥 230027; 3. 北京石油化工学院 机械工程学院,北京 102671; 4. 中国石油集团 东方地球物理公司研究院,河北涿州 072750
基金项目:国家自然科学基金项目(40874093)资助.
摘    要:通过Metravib热机械分析仪,用正弦波进行加载,实验时固定静载为100 N,正弦波动载荷恒为60 N,将总载荷控制在屈服点以下;在温度为-50~125℃,升温速率为1℃/min,频率为5~1000 Hz的条件下,对泵油饱和长石砂岩、彭山砂岩样品进行单轴循环加载实验,求取泵油饱和长石砂岩和彭山砂岩的衰减、耗散角、模量...

关 键 词:正弦波加载  饱和岩石  热弛豫规律  衰减和频散
收稿时间:2010-12-06

Experimental research on viscoelastic behavior for saturated rocks
XI Dao-Ying,XU Song-Lin,XI Jun,YI Liang-Kun,DU Yun.Experimental research on viscoelastic behavior for saturated rocks[J].Chinese Journal of Geophysics,2011,54(9):2302-2308.
Authors:XI Dao-Ying  XU Song-Lin  XI Jun  YI Liang-Kun  DU Yun
Abstract:Experiments are performed by Metravib Dynamic Mechanical Analyzer (DMA+450) under sine wave loading to simulate the seismic wave. The static load is fixed to 100N, and the dynamic load of the sine wave is 60N so that the total loading force is controlled under yield stress. Temperature is controlled between -50℃ and 125℃, and the heating speed is 1℃ per minute. The frequency range is from 5 Hz to 1000 Hz. Pump-oil saturated arkoses and Pengshan sandstones are tested under uniaxial cyclic loading. The variations of attenuation, phase angle, modulus, and velocity with temperature or frequency are obtained. The attenuation peak and the phase angle peak shift to higher temperatures or higher frequencies when the frequency or temperature increases, which can be considered as thermal relaxation regularities. The increasing of attenuation with frequency can be explained by low-frequency resonance. The move of the attenuation peak and increasing of attenuation with frequency can be explained by damping. The aspect ratio of the micro cracks in rock samples would increase with the fatigue loading. The variation of aspect ratio can explain the phenomenon that the attenuation peak value decreases when the frequency increases and the peak shifts to higher frequencies. The experimental results and phenomena are similar to the low-frequency resonance standing wave experiments. Thus the thermal relaxation regularities generally exist for saturated porous rocks. The Young's modulus and velocity increase with frequency and decrease when temperature increases. There is obvious frequency dispersion, and the dispersion weakens when temperature increases. This investigation is very helpful to study of theoretical model and seismic data interpretation.
Keywords:Sine wave loading  Saturated rock  Thermal relaxation regularities  Attenuation and dispersion
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