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A Study of the Characteristics of Scattering Attenuation by Physical Modelling

散射特性之物理模型研究

並列摘要


Scattering attenuation (1/Q(subscript s)) depends not only on wave frequency but also on scatterer size. Using void holes as scatterers in a thin duralumin plate, and with the kα value (k is the wave number, α the scatterer radius) being changed systematically from 0.05 to 5, the fluctuation of direct waves between a homogeneous and a scattering medium are observed in order to calculate the scattering attenuation by 2-D physical model experiments. The experimental results show that 1/Q(subscript s)has a peak around kα=0.5. At high frequency, 1/Q(subscript s) is proportional to (kα)^(-1), whereas at low frequency the decay of 1./Q(subscript s) relative to (kα)^4 is steeper than predicted by Rayleigh scattering. The medium can be considered to be a quasi-homogeneous one, and the scattering effect can be neglected when kα<0.05. The velocity fluctuation has a sharp change at kα=0.5. The velocity of the scattering medium doesn't change when 0.5<kα, is less than that in a homogeneous medium and exhibits a constant fluctuation when kα<0.5. Whether the wave length is smaller or greater than the scatterer size, the P-and S-waves have the same scattering attenuation coefficients if they have the same kα value.

被引用紀錄


曾美綺(2017)。地表地形對地震震波反應影響之數值模擬〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU201702675
陳俊甫(2015)。地形對地表放大效應之影響〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU.2015.01796
藍詩婷(2014)。地形對地震震波反應之影響〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU.2014.01284

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