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Study of effects of focal depth on the characteristics of Rayleigh waves using finite difference method

机译:用有限差分法研究焦深对瑞利波特性的影响

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This paper presents a relationship between the focal depth in terms of Rayleigh-wave wavelength and the dominant frequency of Rayleigh waves generated in a homogeneous half-space. Rayleigh waves were simulated using a (2, 4) staggered grid P-SV wave finite difference algorithm with VGR-stress imaging technique as a free surface boundary condition. VGR is an acronym for vertical grid-size reduction. The simulated seismic responses using P-wave and SV-wave sources at different focal depths revealed Rayleigh-wave generation up to certain focal depth only for the considered frequency bandwidth. A shift of normalized spectral shape of Rayleigh wave towards lower frequency with increasing focal depth was inferred. Largest spectral amplitude was obtained in the wavelength for which the ratio of focal depth to the wavelength of Rayleigh wave was around 0.17 in the case of P-wave source and 0.9 in the case of SV-wave source. An exponential decrease of spectral amplitude of Rayleigh wave with the departure of the ratio of focal depth to Rayleigh wave wavelength from the above mentioned values was obtained.
机译:本文介绍了在瑞利波波长方面的焦深与在均匀半空间中产生的瑞利波的主频之间的关系。使用VGR应力成像技术作为自由表面边界条件的(2,4)交错网格P-SV波有限差分算法模拟瑞利波。 VGR是垂直网格尺寸缩减的首字母缩写。在不同焦深下使用P波和SV波源进行的模拟地震响应显示,仅在考虑的带宽范围内,瑞利波的产生一直到一定的焦深。随着焦深的增加,瑞利波的归一化频谱形状向低频方向的偏移被推断出来。在P波源情况下,焦深与瑞利波的波长之比在0.17附近,在SV波源情况下为0.9,在该波长处获得最大光谱振幅。随着上述深度值与焦深对瑞利波波长之比的偏离,瑞利波的频谱幅度呈指数下降。

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