Study of inversion for third order elastic constants and in situ stress by multifrequency dispersion of cross dipole sonic logging

被引:7
作者
Chen Hao [1 ]
Wang Xiu-Ming [1 ]
Zhao Li-Xin [2 ,3 ]
机构
[1] Chinese Acad Sci, State Key Lab Acoust, Inst Acoust, Beijing 100190, Peoples R China
[2] China Petr Univ Beijing, Beijing 102249, Peoples R China
[3] China Offshore Oil Corp Ltd, Beijing 100010, Peoples R China
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2009年 / 52卷 / 06期
关键词
Acoustoelasticity; Third order elastic constant; Cross-dipole sonic logging; Dispersion curve; In situ stress; Anisotropy; PRESTRESSED FORMATION; COMPRESSIONAL WAVES; ANISOTROPY; BOREHOLE; VELOCITY; ROCKS; PRESSURE; CRACKS;
D O I
10.3969/j.issn.0001-5733.2009.06.030
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Based on acoustoelastic theory, the method of inversion for third order elastic constants (TOECs) and in situ stress from the multi-frequency phase velocity of cross dipole sonic logging data and the effect of different signal to noise ratio (SNR) on the inversion result is studied. Qualitative and quantitative analysis shows that the contribution of the terms in acoustoelastic velocity-stress model not containing TOECs to the total velocity variation can be neglected, when compared to the contribution of the terms containing TOECs. This means that the inversion of TOECs and in situ stress is a severely ill-posed problem or an indeterminate one when only using the data at one time. The inversion stability is simulated for every accurate and approximate inversion model at different level SNR. Numerical result shows that the result inverted from the cross logging data at one borehole pressure using accurate model is affected heavily by noise. Both accurate model and approximate one in the inversion of data gotten at two different borehole pressures have the same accuracy. Thus, the latter can take place of the former to improve the computation speed and to simplify the model. The result also shows that the two-step method can give a better estimation of TOECs and in situ stress.
引用
收藏
页码:1663 / 1674
页数:12
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