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利用频变地震反射系数识别含气储层
引用本文:许多,甘其刚,唐建明,李勇.利用频变地震反射系数识别含气储层[J].西南石油大学学报(社会科学版),2014,34(2):37-42.
作者姓名:许多  甘其刚  唐建明  李勇
作者单位:1. 中国石化多波地震技术重点实验室,四川德阳6180002. 中国石化西南油气分公司研究院德阳分院,四川德阳6180003. 成都理工大学地球物理学院,四川成都610059
摘    要:地震波在孔隙介质中传播的渐进方程可用于在地震频带内计算法向入射反射系数,这个频变的反射系数可用一个无量纲的参数ε 来表示,ε 可表示为储层流动性参数(即粘滞性的倒数)、流体密度和信号频率的乘积。利用该表达式,对中国新场气田的实际数据进行了计算,新场气田的储层大多为超致密的砂岩并且渗透率很低。在计算结果上观测到了砂岩储层内过渡区的气水界面上反射系数在地震频带内随频率变化的现象。利用该研究结果指导了地震反演并提取了相应的地震属性,这些属性被首先用于进行的流体(气或水)辨别,最后,在此基础上进行了含气和含水储层的识别。

关 键 词:弹性孔隙介质    法向反射系数    渐进方程    气水界面    混沌反演

Frequency-dependent seismic Reflection Coefficient forDiscriminating Gas Reservoirs
Xu Duo,Gan Qigang,Tang Jianming,Li Yong.Frequency-dependent seismic Reflection Coefficient forDiscriminating Gas Reservoirs[J].Journal of Southwest Petroleum University(Social Sciences Edition),2014,34(2):37-42.
Authors:Xu Duo  Gan Qigang  Tang Jianming  Li Yong
Institution:1. The Key Laboratory of Multicomponents Seismic Technology,SINOPEC,Deyang,Sichuan 618000,China2. Deyang Branch Institute,Southwest Oil & Gas Branch SINOPEC,Deyang,Sichuan 618000,China3. College of Geophysics,Chengdu University of Technology,Chengdu,Sichuan 610059,China
Abstract:The asymptotic equation of wave propagation in fluid-saturated porous media is available for calculating the normalreflection coefficient within seismic frequency band. This frequency-dependent reflection coefficient is expressed in terms ofa dimensionless parameter ,which is the product of the reservoir fluid mobility (i.e. inverse viscosity),fluid density,and thefrequency of the signal. In this paper,we apply this expression to Xinchang gas-field,China,where reservoirs are super intight sands with very low permeability. We demonstrate that the variation in reflection coefficient at gas/water contacts is asa transition zone within a sand formation observable within seismic frequency band. Then we conduct seismic inversion togenerate attributes which first indicate the existence of fluid (either gas or water),and then discriminate a gas reservoir from awater reservoir.
Keywords:poroelastic media                                                                                                                        normal reflection coefficient                                                                                                                        asymptotic equation                                                                                                                        gas/water contact                                                                                                                        chaotic inversion
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