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APPLIED GEOPHYSICS  2012, Vol. 9 Issue (1): 73-79    DOI: 10.1007/s11770-012-0316-6
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Fractional S transform – Part 1: Theory*
Xu De-Ping and Guo Ke
Key Laboratory of Geomathematics of Sichuan Province, Chengdu University of Technology, Chengdu 610059, China.
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Abstract The S transform, which is a time-frequency representation known for its local spectral phase properties in signal processing, uniquely combines elements of wavelet transforms and the short-time Fourier transform (STFT). The fractional Fourier transform is a tool for non-stationary signal analysis. In this paper, we defi ne the concept of the fractional S transform (FRST) of a signal, based on the idea of the fractional Fourier transform (FRFT) and S transform (ST), extend the S transform to the time-fractional frequency domain from the timefrequency domain to obtain the inverse transform, and study the FRST mathematical properties. The FRST, which has the advantages of FRFT and ST, can enhance the ST fl exibility to process signals. Compared to the S transform, the FRST can effectively improve the signal timefrequency resolution capacity. Simulation results show that the proposed method is effective.
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XU De-Ping
GUO Ke
Key wordsfractional S transform   fractional Fourier transform   time-frequency analysis     
Received: 2011-12-30;
Fund:

This work was supported by Scientifi c Research Fund of Sichuan Provincial Education Department and the National Nature Science Foundation of China (No. 40873035)

Cite this article:   
XU De-Ping,GUO Ke. Fractional S transform – Part 1: Theory*[J]. APPLIED GEOPHYSICS, 2012, 9(1): 73-79.
 
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