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Effects of Contact Geometry of Faults on Transmission Waves

机译:故障的接触几何形状对传输波的影响

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— In order to clarify the effects of contact geometry of faults on transmission waves, we have performed a series of experiments in which P and S waves with known wavelength were transmitted through an artificial fault. A pair of piezo-electric transducers (PZT) with various resonant frequency were used for the transmitter and the receiver. Parallel grooves were cut on disk surfaces and two disks were placed face to face with the grooves on one disk being perpendicular to those on the other disk. This yields evenly spaced square contacts on the fault. We regard the square contacts as asperity contacts, the size and the height of which were controlled by changing the width and the depth of the grooves. We found that the transmissivity of the waves is solely determined by the ratio of the groove depth/width to wavelength. The shallower and the narrower the groove depth and width are, the larger the amplitude of first arrival is for both P and S waves. When the groove depth is shallower than a quarter of wavelength, the effect of groove depth is negligible; deeper grooves significantly reduce the amplitude. We have made a mathematical model based on the stiffness of fault. By comparing the model calculations with the observation we found that the model has a limit at which the prediction by the model deviates from the data. The deviation occurs when the ratio of the groove depth/width to wavelength becomes 0.25. We refer to the wavelength as the critical wavelength. When the wavelength is larger than the critical wavelength, the observed data can be well explained by the model. Above this threshold, the model no longer fits the data. In this range, the amplitude of transmitted waves is found to be proportional to the real contact area. Although it is a kind of paradox that the amplitude, not the energy, is proportional to the real contact area, it is possibly explained by taking a non-uniform distribution of stress on the surface of the receiver PZT into account.
机译:—为了阐明故障的接触几何形状对传输波的影响,我们进行了一系列实验,其中已知波长的P和S波通过人工故障传输。一对具有不同谐振频率的压电换能器(PZT)用于发射器和接收器。在磁盘表面上切出平行凹槽,并将两个磁盘面对面放置,其中一个磁盘上的凹槽垂直于另一磁盘上的凹槽。这会在断层上产生均匀间隔的方形触点。我们将方形触点视为粗糙触点,其大小和高度通过更改凹槽的宽度和深度来控制。我们发现,波的透射率仅由凹槽深度/宽度与波长的比值决定。凹槽深度和宽度越浅且越窄,则P波和S波的初次到达振幅都越大。当凹槽深度小于四分之一波长时,凹槽深度的影响可忽略不计;更深的凹槽会显着降低振幅。我们基于断层的刚度建立了数学模型。通过将模型计算与观察结果进行比较,我们发现该模型具有一个极限,在该极限下,模型的预测会偏离数据。当凹槽深度/宽度与波长之比变为0.25时,会发生偏差。我们将波长称为临界波长。当波长大于临界波长时,该模型可以很好地解释观察到的数据。超过此阈值,模型将不再适合数据。在此范围内,发现发射波的振幅与实际接触面积成正比。尽管振幅而不是能量与实际接触面积成正比是一种悖论,但可以通过考虑接收器PZT表面应力的不均匀分布来解释。

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