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wave propagation相关的网络例句

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与 wave propagation 相关的网络例句 [注:此内容来源于网络,仅供参考]

With the algebraic result in form of piecewise function expressions, the excitation and propagation processes of stress waves, including the longitudinal wave, the transverse wave, and Rayleigh-wave, are discussed in detail.

基于该分段函数形式的代数结果,纵波、横波、Rayleigh波等应力波成分在弹性表面的激发和传播过程得到详尽分析,其中很多结论是已有的解析积分结果或者数值计算结果不曾得到的。

To research the propagation characteristics of travelling wave along transmission line in depth, the authors establish a mathematical model of travelling wave along lossless transmission line with the format of discrete time and space mesh lines, derive the stable condition and boundary condition of the wave equations using numerical solution of partial differential equation, and attempt the simplification of the boundary condition to realize full decoupling of voltage and current.

为深入研究行波在配电线路上的传播特性,建立了时间-空间网格线离散格式的无损传输线行波数学模型,采用偏微分方程的数值解法推导了波动方程的稳定条件和边界条件,并尝试对边界条件进行简化,以实现电压和电流的完全解耦。

Based on the basic principle of reflection and transmission in the process of the propagation of logitudinal wave, this paper recounts a new theory and method for the application of pile body completeness inspection data with reflection wave method to the quantitative determination of apparent reflection coefficients and the round travelling time of reflection wave.

摘要从纵波传播过程的反射和透射的基本原理出发,介绍了反射法桩身完整性检测数据在频率域中定量确定视反射系数和反射波往返时间的一种新的理论和方法。

It has been proven that, from the propagation process of the tidal waves and wave energy rates, the whole radial sandbanks area is controlled by the progressive tidal wave in the south and the rotational standing tidal wave in the north.

另外还研究了辐射沙脊群海域的余流及余流量的分布,发现在潮流沙脊两侧存在平面余环流,余环流将有利于泥沙在脊顶沉积,与潮流沙脊的维持发育密切相关。

The mechanism of spallation is analyzed as a result of the interaction of the unloading wave and reflected stress wave. The propagation of laser-induced stress wave is also further investigated, and the influences of film thickness on spall thickness as well as the time when spallation begins are predicted.

分析了层裂机制,得出靶材是在卸载波及被反射的压力波的共同作用下发生层裂;探讨了激光诱导压力波的传播规律,预测了不同靶厚下的层裂厚度及其对层裂开始时间的影响。

The evolution of the half-peak width of the relative density increment pulse with respect to slow wave also demonstrates the close relation to Δp. Its minimum w〓 decreases with the increase of Δp, which means, slow wave will steepen with the enhancement of Δp and may evolve into slow shock eventually. Numerical results also indicate that the propagation velocity of fast and slow wave increase when Δp increases.

对强扰动情形(Δp=5),通过考察相关物理量的径向分布,并借助于对物理量沿波动阵面法向分布的讨论,可以初步判断出由强扰动所造成的慢模磁声波在传播过程中逐渐陡变而演化为慢激波,慢激波在进入日冕前已在色球层中形成,并在此后的传播过程中始终保持这一性质。

But the symmetric axis of TI formation is parallel to the borehole axis in the thesis, the propagation velocity of SV-wave and SH-wave are the same in vertical direction, we can't see the splitting phenomena of shear wave.

本文中地层对称轴和井轴平行,SV波和SH波在竖直方向上的传播速度是相同的,本文地层模型下的井孔中是观测不到横波劈裂现象的。

Based on the fact that the different modes of Rayleigh wave have different propagation velocities, the signals of Rayleigh wave which superposes in time domain can be separated in frequency-wave-number domain, different modes of Rayleigh wave are separated and extracted by Fourier transform.

摘 要:应用Fourier变换法分离提取地震记录中不同模态的瑞雷面波,其原理是:利用瑞雷面波各模式传播速度的差异,将时间域中叠加在一起的瑞雷面波信号在频率波数域中分开,以此实现分离提取各阶模态瑞雷面波。

The application of the modified Rytov's method to the study of the optical-wave oblique propagation is discussed in this paper. The fluctuation index of the plane wave and the spherical wave is obtained.

将修正的Rytov方法推广应用于研究斜程传输问题,推导了平面波和球面波斜程传输时的闪烁指数,并根据ITU-R湍流大气结构模型,对平面波和球面波在不同传播高度、近地面风速、近地面大气结构常数、零内尺度以及非零内尺度下的闪烁指数进行了理论据导,做出了具体的数值分析。

The results show that when gravity wave's propagating in the homogenous winds, the nonlinearity is stronger in the fair wind than in the contrary wind, the background winds change the propagation velocity and path, and when gravity wave's propagating in the homogenous winds, the vertical wavelength decreases, the average upgoing energy flux reduces which implies the ambient winds absorb the energy of the wave, realizes coupling of the different atmosphere layers.

结果表明,当重力波在均匀风场中传播时,非线性效应在顺风场中比在逆风场中更显著,背景风会改变重力波在水平方向的传播速度和传播路径;当重力波在剪切风场中传播时,重力波在垂直方向上平均能流随高度的增高而减少,表明背景吸收了重力波的能量,在重力波向上传播的过程中,实现了大气各层之间的耦合。

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