地球科学进展 ›› 2006, Vol. 21 ›› Issue (03): 242 -249. doi: 10.11867/j.issn.1001-8166.2006.03.0242

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双相介质AVO方程及参数简化研究
雍学善 1,2,马海珍 2,高建虎 2   
  1. 1.石油大学资源与信息学院,北京 100083;2.中国石油勘探开发研究院西北分院,甘肃 兰州 730020
  • 收稿日期:2005-08-16 修回日期:2005-12-13 出版日期:2006-03-15
  • 通讯作者: 雍学善 E-mail:yxs321@263.net

A Study of AVO Equation in Dual-phase Medium and Parameter Simplification

Yong Xueshan 1,2,Ma Haizhen 2,Gao Jianhu 2   

  1. 1. Faculty of Resource and Information China University of Petroleum, Beijing 100083,China;2. PetroChina Exploration&Development Research Institute(Northwest),Lanzhou 730020,China
  • Received:2005-08-16 Revised:2005-12-13 Online:2006-03-15 Published:2006-03-15

基于2种双相介质分界面的反射系数和透射系数方程组,推导出了单相/双相分界面(储层顶界面)、双相/单相分界面(储层底界面)和单相/单相分界面(两种致密岩层分界面)3种类型分界面的反射系数和透射系数方程组,形成了从单相介质到双相介质较全面的AVO方程组;推导出了双相介质参数(ANQRρ11ρ12ρ22Ø)与纵波速度、横波速度、密度、孔隙度以及流体类型(油、气、水)之间的关系式,为双相介质AVO理论走向实用进行了有益的探索。设计了3种类型的岩性分界面,分别用双相介质AVO方程和Zeoppritz方程计算了各类界面的快纵波反射系数曲线,证实了Zoeppritz方程是双相介质AVO方程的一个特例。

Based on the equation group of reflection coefficient and transmission coefficient in the interface of two types of dual-phases mediums, three equation groups of reflection coefficient and transmission coefficient in three kinds of interfaces have been derived, which are the interface between one-phase and dual-phase medium that is the top of reservoir, dual-phase and one-phase that is the bottom of reservoir, one-phase and one-phase medium that is the interface of two tight rocks. The AVO equation group from one-phase to dual-phase has been produced comprehensively. The relationship formula have been built between parameters(A, N, Q, R, ρ11, ρ12, ρ22, Ø) of the dual-phase medium and prime wave velocity, second wave velocity, density, porous and kind of fluid that include brine, oil and gas. All of these studies have made a beneficial exploration of AVO theory in dual-phase medium to practice. Three kinds of lithological interfaces have been designed. The reflection coefficient curves of different interfaces have been calculated respectively by dual-phase medium AVO equation and Zeoppritz equation, which provedhat Zeoppritz equation is a special case of dual-phase medium AVO equation.

中图分类号: 

[1] Biot M A. Theory of propagation of elastic waves in a fluid-saturated porous solid,part I: Low-frequency range[J]. Journal of the Acoustical Society of America, 1956,28(2):168-178.

[2] Biot M A. Theory of propagation of elastic waves in a fluid-saturated porous solid,part II: Higher-frequency range[J]. Journal of the Acoustical Society of America, 1956, 28 (2):179-191.

[3] Mu Yongguang. Reservoir Geophysics[M]. Beijing: Petroleum Industry Press,1996.[牟永光.储层地球物理学[M].北京:石油工业出版社,1996.]

[4] Greertsma J,Smith D C. Some aspects of elastic wave propagation in fluid saturated porous solids[J]. Geophysics,1961,33(2):169-181.

[5] Amos Nur, et al. Wave Propagation in Dual-phase Medium[M]. Xu Yun,translated. Beijing: Petroleum Industry Press,1986.[Amos Nur等著.双相介质中波的传播[M].许云译.北京:石油工业出版社,1986.]

[6] Wang Shangxu. The Finite Element Numerical Solution of Elastic wave in Dual-phase Medium and AVO Problem[D]. Beijing: China University of Petroleum,1990.[王尚旭.双相介质中弹性波问题有限元数值解和AVO问题[D].北京:中国石油大学,1990.]

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