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饱和砂岩在温度和频率域的衰减和速度频散

Attenuation and dispersion of saturated rocks in temperature and frequency domains

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【作者】 席军宛新林周城光杜赟席道瑛

【Author】 Xi Jun;Wan Xinlin;Zhou Chengguang;Du Yun;Xi Daoying;School of Mechanical Engineering,Beijing Institute of Petrochemical Technology;The Civil Engineering School,Anhui University of Architecture;Key Laboratory of Noise and Vibration ResearchInstitute of Acoustics,Chinese Academyof Sciences;Mengcheng National Geophysical Observatory,School of Earth and Space Science,University of Science and Technology of China;

【机构】 北京石油化工学院机械工程学院安徽建筑工业学院土木工程学院中国科学院噪声与振动重点实验室中国科学技术大学地球和空间科学学院蒙城地球物理国家野外观测站

【摘要】 利用Metravib热机械分析仪,在天然地震的频率和温度范围内,首次对泵油和甘油饱和两种孔隙度的彭山砂岩的衰减和速度频散进行了实验研究.结果表明,①泵油饱和彭山砂岩对频率和温度的依赖呈热激活弛豫规律;②杨氏模量和弹性波速度与孔隙度、温度呈负相关,与饱和液体的黏滞系数、频率呈正相关;③频散效应因频率上升而增强,因温度增高而减弱.这一规律性的结果为地震波理论研究提供了实验基础.

【Abstract】 Experiments are performed by Metravib dynamic mechanical analyzer about the attenuation and dispersion of pump-oil and glycerol saturated Pengshan sandstones with two kinds of porosities.The frequency and temperature of tests are natural earthquake.The results show:① The attenuation peak of pump-oil saturated Pengshan sandstone appears to be thermo-activated relaxation.② Young’s modulus and elastic wave velocity of saturated Pengshan sandstones reduce with porosity and temperature increasing,and rise with viscosity coefficient of saturated liquid and frequency increasing.③ Frequency dispersion attenuates as temperature increases,enhances as frequency rises.The data provides the experiment foundation for theoretical research of seismic waves.

【关键词】 饱和砂岩衰减模量速度频散
【Key words】 saturated rockattenuationmodulusdispersion of velocity
【基金】 国家自然科学基金项目(40874093)资助
  • 【文献出处】 地震学报 ,Acta Seismologica Sinica , 编辑部邮箱 ,2013年06期
  • 【分类号】P631.4
  • 【网络出版时间】2013-11-13 08:41
  • 【下载频次】86
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