On the Method of Adaptive Waveform Inversion with Zero-Offset VSP Data

2009 ◽  
Vol 52 (6) ◽  
pp. 1369-1380
Author(s):  
Jing-Huai GAO ◽  
Chao WANG ◽  
Wei ZHAO
Author(s):  
Chao Jin ◽  
Danping Cao ◽  
Xingyao Yin

Abstract Waveform inversion of Vertical Seismic Profiling (VSP) data, including upgoing and downgoing wavefields, is a challenging technique for building an accurate model. During the inversion process, upgoing and downgoing wavefields have different contributions to the objective function due to an energy imbalance between them that may cause the upgoing field to not be used effectively. Therefore, we propose a method of joint waveform inversion with the separated upgoing and downgoing wavefields of VSP data based on the establishment of a multiobjective function without introducing weight coefficients. The separating step with direct simulation of upgoing and downgoing wavefields of VSP data by the reflectivity method simplifies the complexity of separating wavefields. Specially, the zero-offset VSP data can be obtained in the τ−p domain to reduce computational cost greatly. Establishment of a multiobjective function of the difference between upgoing and downgoing wavefields can overcome the energy imbalance problem for them. The joint inversion step with a multiobjective optimization method avoids insufficient or incomplete information from just using an upgoing or downgoing wavefield alone. Numerical tests applied on synthetic models indicate that this method has the potential to increase the accuracy of estimating the velocity and density.


Geophysics ◽  
2009 ◽  
Vol 74 (6) ◽  
pp. WCC141-WCC148 ◽  
Author(s):  
Yushan Yang ◽  
Yuanyuan Li ◽  
Tianyou Liu

Wave attenuation is an important physical property of hydrocarbon-bearing sediments that is rarely taken into account in site characterization with seismic data. We present a 1D viscoelastic waveform inversion scheme for determining the quality factor [Formula: see text] from the normal-incidence surface seismic and zero-offset vertical seismic profile (VSP) data simultaneously. The joint inversion problem is solved by the damped least-squares method, and the inversion result is successful using synthetic data. The effects of initial model thickness, [Formula: see text] value, and the existence of noise were studied through a synthetic example. By extracting all of the information contained in the waveforms, the waveform inversion of the seismic reflection and transmission data becomes a powerful tool for estimating [Formula: see text]. For a more comprehensive image of [Formula: see text], the tomographic inversion of [Formula: see text] is applied to the walkaway VSP and prestack surface seismic data, using the waveform inversion result as the initial model. Results from applying the method to a real seismic line and zero-offset VSP data from the Nanyang oilfield, central China, indicate that [Formula: see text] from the tomographic inversion of reflection and transmission data contains useful information on medium properties, which can aid in reservoir appraisal.


Geothermics ◽  
2021 ◽  
Vol 94 ◽  
pp. 102095
Author(s):  
David Li ◽  
Lianjie Huang ◽  
Benxin Chi ◽  
Kai Gao ◽  
Clay Jones ◽  
...  

2014 ◽  
Vol 101 ◽  
pp. 51-67 ◽  
Author(s):  
Jing Zhao ◽  
Jinghuai Gao ◽  
Daxing Wang ◽  
Mengli Zhang

Author(s):  
G.L. Zhang ◽  
X.M. Wang ◽  
Z.H. He ◽  
F. Li ◽  
Y.B. Zhang ◽  
...  
Keyword(s):  
Q Factor ◽  
Vsp Data ◽  

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