Preprints
https://doi.org/10.5194/egusphere-2026-5413
https://doi.org/10.5194/egusphere-2026-5413
21 Sep 2026
 | 21 Sep 2026
Status: this preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).

Regional spectral decay model for the Sichuan, China: Application in ground motion simulation of the Ms 6.0 Changning earthquake

Pengfei Dang, Bingyan Zhao, Qifang Liu, Jie Cui, and Xinjian Jia

Abstract. 4260 recordings of 165 events by 168 stations were used to calculate the spectral decay kappa parameter. The kappa values of the two horizontal components were similar and generally larger than those of the vertical component. The impact of magnitude and site condition on the κ0 value was also investigated, which showed that κ0 increased with magnitude, indicating that κ0 is influenced by source effects. In addition, the results showed that softer sites have higher κ0 values, indicating that site conditions significantly affect κ0 estimates. The single-station κ0 values showed little difference between the two horizontal components, both of which were significantly greater than the κ0 value of the UD component. Furthermore, the relationships between κ0 and Vs30 were derived, which indicates that κ0 value decreases with increasing parameter Vs30. Moreover, the logκ0-logf0 correlations estimate the κ0 better than the lnVs30-κ0 correlation does. Finally, we performed ground motion simulations at 16 stations to validate the derived site-based kappa model. Ground motion simulations at 16 stations demonstrate that both site- and event-related κ₀ mainly affect high-frequency amplitudes. These findings provide a basis for seismic attenuation study and refined ground motion simulation in the study region.

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Pengfei Dang, Bingyan Zhao, Qifang Liu, Jie Cui, and Xinjian Jia

Status: open (until 02 Nov 2026)

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Pengfei Dang, Bingyan Zhao, Qifang Liu, Jie Cui, and Xinjian Jia
Pengfei Dang, Bingyan Zhao, Qifang Liu, Jie Cui, and Xinjian Jia

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Short summary
Spectral amplitude drops at high frequencies beyond a threshold, always modeled by kappa.  Using Sichuan ground motion data, we studied event κ vs epicentral distance, magnitude, and site conditions. Conclusions: (1) κ0 increases with magnitude. (2) Vs30 from empirical equation weakly correlates with κ0; however, Vs30-k corrections derived from drilling and PEER agree. (3) κ0 relates to short-period amplitude; at f<1Hz, simulated FAS differ from observed.
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