The origin of low-frequency maxima in the spectra of seismic noise |
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Authors: | V K Sidorov M V Tarantin |
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Institution: | 1. Institute of Mining, Ural Branch, Russian Academy of Sciences, Perm, Russia
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Abstract: | The evidence attesting to the possibility of the largest spectral maximum in seismic noise with a peak frequency of 0.14–0.22 Hz to form as a result of low-frequency dissipation of elastic wave energy in rocks is presented. According to this mechanism, elastic wave energy in rock, which can be considered as a two-component medium (solid matrix + pore water), is dissipated in the form of low-frequency pulses whose energy is the lower the smaller the coefficient of porosity. It is assumed that weak seismic events continuously occur in the frequency range above 6 Hz, and their dissipated energy is a source of the low-frequency noise. |
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