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Seismic physical modeling and quality factor

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Abstract

Accurate Q parameter is hard to be obtained, but there is great difference between Q measurements from different measurement methods in seismic physical modelling. The influence factors, stability and accuracy of different methods are analyzed through standard sample experiment and the seismic physical modelling. Based on this, we proposed an improved method for improving accuracy of pulse transmission method, in which the samples with similar acoustic properties to the test sample are selected as the reference samples. We assess the stability and accuracy of the pulse transmission, pulse transmission insertion, and reflection wave methods for obtaining the quality factor Q using standard and reference samples and seismic physical modeling. The results suggest that the Q-values obtained by the pulse transmission method are strongly affected by diffraction and the error is 50% or greater, whereas the relative error of the improved pulse transmission method is about 10%. By using a theoretical diffraction correction method and the improved measurement method, the differences among the Q-measuring methods can be limited to within 10%.

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Acknowledgments

We thank Professors Genyang Tang and Sanyi Yuan for comments and suggestions.

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Correspondence to Jian-Xin Wei.

Additional information

This study was supported by the National Nature Science Foundation of China (No.41474112) and the National Science and Technology Major Project (No.2017ZX05005-004).

The Gao Feng graduated from a bachelor's degree in geophysics from Shandong University of Science and Technology (2011). He received a MS in exploration geophysics from China University of Mining & Technology-Beijing (2014). Currently he is studying his Ph.D. student in the College of Geophysics and Information Engineering, China University of Petroleum (Beijing). His main research interests are seismic attenuation and the physical modelling.

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Gao, F., Wei, JX. & Di, BR. Seismic physical modeling and quality factor. Appl. Geophys. 15, 46–56 (2018). https://doi.org/10.1007/s11770-018-0664-y

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  • DOI: https://doi.org/10.1007/s11770-018-0664-y

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