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应用地球物理  2011, Vol. 8 Issue (4): 344-354    DOI: 10.1007/s11770-011-0296-y
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随机弹性介质中地震波散射衰减分析
刘炯1,2,3,魏修成1,2,季玉新1,2,陈天胜1,2,刘春园1,2,张春涛1,2,戴明刚2
1. 中国石化多波地震技术重点实验室,北京 10083;
2. 中国石化石油勘探开发研究院,北京 100083;
3. 中国石油大学(北京)地球物理与信息工程学院,北京 102249
An analysis of seismic scattering attenuation in a random elastic medium
Liu Jiong1, 2,3, Wei Xiu-Cheng1,2, Ji Yu-Xin1,2, Chen Tian-Sheng1,2, Liu Chun-Yuan1,2, Zhang Chun-Tao1,2, and Dai Ming-Gang2
1. Sinopec Key Laboratory of Multi-Component Seismic Technology, Beijing 10083, China.
2. Exploration & Production Research Institute, SINOPEC, Beijing 10083, China.
3. Resource and Communication College, China University of Petroleum (Beijing), Beijing 102249, China.
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摘要 地震波衰减一直是许多学科研究的热点,因为可以反映介质的特性。导致地震波衰减的因素很多,如:传播过程中由于能量扩散导致的几何衰减,固体岩石内部晶粒间相对滑移导致的摩擦衰减,岩石结构不均匀引起的地震波散射衰减。本文主要从统计的观点出发,通过多次数值模拟的方法研究纵波因为散射在随机弹性介质中的所引发的衰减。首先用随机理论建立了二维空间随机弹性介质模型,然后用错格伪谱法的数值方法模拟了波在随机介质中的传播,再通过波场中虚拟检波器的记录,用谱比法估计了弹性波在随机介质中的散射衰减。不同非均匀程度随机弹性介质中的数值结果表明:介质不均匀程度越高,散射衰减越大;在散射体尺寸小于波长的前提下,不同散射体尺寸的计算结果说明:散射体尺寸越大,弹性波衰减越明显。最后提出了一种不均匀孔隙介质中流体流动衰减的方法。通过对随机孔隙介质中地震波的总衰减和散射衰减分别进行了计算,并定量得出了随机孔隙介质中流体流动衰减,结果表明:在实际地震频段下,当介质不均匀尺度101 米量级时,散射衰减比流体流动衰减要大,散射衰减是地震波在实际不均匀岩石孔隙介质中衰减的主要原因。
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刘炯
魏修成
季玉新
陈天胜
刘春园
张春涛
戴明刚
关键词散射衰减   随机弹性介质   谱比法     
Abstract: Seismic attenuation has been an interesting topic of research, for it refl ects the inherent media characteristics in which seismic waves propagate. There are many factors that cause seismic wave attenuation, such as geometry attenuation caused by energy dissipating during propagation, friction attenuation by relative sliding among rock grains, and scattering attenuation by rock heterogeneity. In this paper we study P-wave scattering attenuation in a random elastic medium by numerical simulations from a statistical point of view. A random elastic medium model is built based on general stochastic process theory. Then a staggered-grid pseudo-spectral method is used to simulate wave propagation. Scattering attenuation is estimated by the spectral ratio method based on virtual detector records. Random elastic media numerical scatter results with various heterogeneity levels show that the higher heterogeneous levels cause greater scattering attenuation. When the scatter sizes are smaller than a wave length, the larger scatters give a greater attenuation. Finally, we propose a method to evaluate fluid-flow attenuation in porous media. The fluid-flow attenuation is derived from total attenuation and scattering attenuation in random porous media and the attenuation is estimated quantitatively. Results show that in the real seismic frequency range when the heterogeneous scale is about 101 meters (less than one wave length), scattering attenuation is larger than fluid-flow attenuation in random porous media and scattering attenuation is the main factor of seismic attenuation in real heterogeneous porous media
Key wordsscattering attenuation   random elastic medium   the spectral ratio method   
收稿日期: 2011-01-07;
基金资助:

国家自然科学基金重点项目“海相碳酸盐岩储层多波地震预测方法研究”资助。

引用本文:   
刘炯,魏修成,季玉新等. 随机弹性介质中地震波散射衰减分析[J]. 应用地球物理, 2011, 8(4): 344-354.
LIU Jiong,WEI Xiu-Cheng,JI Yu-Xin et al. An analysis of seismic scattering attenuation in a random elastic medium[J]. APPLIED GEOPHYSICS, 2011, 8(4): 344-354.
 
没有本文参考文献
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