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Wave propagation in transversely isotropic generalized thermoelastic half-space with voids under initial stress

机译:横观各向同性广义热弹性半空间在初始应力作用下的波传播

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Purpose - The purpose of this paper is to study the wave propagation in transversely isotropic generalized thermoelastic half-space with voids under initial stress. Design/methodology/approach - The authors analyze the wave propagation and reflection of plane waves incident at the stress free, thermally insulated or isothermal surface of a homogeneous, transversely isotropic generalized thermoelastic half-space with voids. The graphical representation is given for amplitude ratios of various reflected waves to that of incident waves for different direction of propagation. The phase velocities and attenuation coefficients of plane waves are also computed and presented graphically for various incident angles. Findings - The phase velocities and attenuation coefficients of these plane waves are computed along various direction of wave propagation and the reflection characteristics of these waves, stress free, thermally insulated or isothermal boundary conditions are considered. The amplitude ratios of various reflected waves to that of incident waves have been obtained numerically. Originality/value - Wave propagation in an elastic medium is of great practical importance. Since valuable organic and inorganic deposits beneath the earth surface are difficult to detect by drilling randomly, wave propagation is the simplest and most economic technique and does not require any drilling through the earth. Almost all the oil companies rely on seismic interpretation for selecting the sites for exploratory oil wells because seismic wave methods have higher accuracy, higher resolution and are more economical, compared to drilling, which is expensive and time consuming. The study described in this paper would be very useful for those involved in signal processing, sound system and wireless communication.
机译:目的-本文的目的是研究在初始应力下具有孔隙的横向各向同性广义热弹性半空间中的波传播。设计/方法/方法-作者分析平面波在均匀,横向各向同性的广义热弹性半空间的无应力,绝热或等温表面入射的平面波的传播和反射。对于不同的传播方向,给出了各种反射波与入射波的振幅比的图形表示。还计算了平面波的相速度和衰减系数,并以图形方式显示了各种入射角。发现-这些平面波的相位速度和衰减系数是沿着波传播的各个方向计算的,并且考虑了这些波的反射特性,无应力,隔热或等温边界条件。已经通过数值获得了各种反射波与入射波的振幅比。原创性/价值-弹性介质中的波传播非常重要。由于很难通过随机钻探来探测地下表面的有价值的有机和无机沉积物,因此波传播是最简单,最经济的技术,不需要在地球上进行任何钻探。几乎所有的石油公司都依靠地震解释来选择勘探油井的地点,因为与钻井相比,地震波方法具有更高的精度,更高的分辨率和更经济,因此昂贵且费时。本文所描述的研究对于信号处理,声音系统和无线通信领域的人员将非常有用。

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