نیارش گستر ایران

ساختن دست یافتنی است!

نیارش گستر ایران

ساختن دست یافتنی است!

My M.S. Thesis Abstract


Subject:

Correction of Earthquake Records Using Wavelet Conversion with Case Study


Abstract

 

Time history analysis method is a powerful and effective method in assessing structures response to earthquake due to the influence of structural reflections at each time point during earthquake. To perform this analysis, there is a need for accelerations that are consistent with the region's seismic characteristics. But in some areas, seismic data is not well recorded. One way to solve this problem is to use Acceleration of artificial mappings for the seismic properties of the area. One of the problems with this path is the noise in the earthquake signals. One of the best ways to remove noise from earthquake signal data is wavelet transform. In this thesis, a wavelet transform-based method for generating spectral-compatible mappings is introduced. In this method, a record is decomposed by wavelet transform, for this purpose, the discrete wavelet transform of the Elsentro earthquake mapping is obtained as the input parameter and the details and approximations are derived from these mapping acceleration data, which are general, low frequency and detail, high frequency (noise). Now, if the Elsentro earthquake signal is subtracted from the details resulting from the discrete violet function output, the noise is eliminated from the earthquake mapping acceleration function. At the filtering stage, careful analysis of the data obtained from the analysis of different waves using wavelet transform is performed Will exist. Detail coefficients are small and include high frequency signals, while approximation coefficients are almost similar to the original wave and include low frequencies. By using discrete wavelet transform and noise removal, one can obtain the time of each frequency and its intensity. Also, by examining the frequency-time diagram it was observed that what frequencies are applied to the structure by earthquakes. This helps us to avoid resonance or resonance in the structure if the earthquake frequency is equal to the intrinsic frequency of the structure.