Finally, the method of wave motion input is established.
最后，建立了相应的波动输入方法。
This also is a not small wave motion undoubtedly to the market.
这对市场无疑也是一个不小的波动。
The Vibration and wave motion are basic states of material motion.
振动和波动是物质运动的基本形态。
The vibration in the air and in the other media travels as a wave motion.
空气及其他介质中的各种振动都是以波动的形式传播的。
Light is to be considered as some kind of wave motion of electromagnetic origin.
我们应该把光看成是某种电磁性质的波动。
The EB model is applicable to nonlinear and irregular wave motion in large area.
EB模型则可用于求解广阔海域内非线性不规则波浪的运动和变形过程。
It is noted that this is a quantum mechanical analogy of the stochastic wave motion.
指出它是随机波动过程的量子力学模拟。
Just as sound is a wave motion, light in the same sense, may be regarded as a wave motion.
正如声音是一种波动一样，光也同样可以看作是一种波动。
Wave motion response of tunnel lining embedded in unbounded nonuniform soil medium is studied.
研究了不均匀岩土介质中隧洞衬砌的波动响应。
This phenomenon, peculiar to the two - dimensional wave motion, is sometimes called diffusion.
二维波所特有的这种现象，有时叫做弥散现象。
Be this kind of relation and its motion, brought about the periodic wave motion of real economy.
正是这种关系及其运动，导致了现实经济的周期性波动。
The elastic vibration of spacecraft with beam like appendages is studied as wave motion in this paper.
将带梁式柔性附件航天器的附件振动作为波动研究。
This paper studies the wave motion in rubble mound breakwater by discarding the homogeneous assumption.
本文抛弃均质渗流假定，对抛石防波堤内波浪运动的问题进行了研究。
The harmonic analysis can reveal the characteristics of wave motion in various scales at different latitudes.
谐谱分析便于揭示不同纬圈上不同尺度的波动特征。
A cork floating on water is not swept along with the water. Rather, it moves up and down with the wave motion.
漂在水面上的软木塞没有随波流走。相反，它随波上下浮动。
The theory of waves propagation in inhomogeneous damaged zone and inversion of wave motion equations are studied.
研究了波在非均匀损伤介质中的传播及波动方程的反演。
The Psychological Wave Motion is inevitable for the players in games, and it affects the players 'actions directly.
篮球运动员在比赛中心理波动是不可避免的，它直接影响运动员在比赛中的表现。
Numerical test study about the stability and precision of the method is made by discussing the solution of SH wave motion.
对采用该方法求解点源出平面波动问题时的数值稳定性和精度进行了数值试验研究。
John Mitchell, an English physicist and astronomer, was inspired by it to put forward the first theories of wave motion in the earth.
约翰·米切尔，英国物理及天文学家，由此得到灵感并提出了第一个地球内部波动理论。
In the last, we make some suggestion about the study of seismic wave motion, detection and it's application in anisotropic medium.
最后对我国在各向异性介质中地震波动、检测和应用等研究提出了一些看法。
It is popular in many countries around the world where appropriate conditions exist-an expanse of water unaffected by wave motion.
它在世界很多国家流行，只要他们有平静的广阔的水域这种条件。
Accuracy of the boundary in frequency do, main is first discussed and demonstrated in terms of one dimensional model of wave motion.
首先讨论了频域透射边界的精度，并用一维波动模型详细论证了它的精度和可行性。
They are merely a reproduction of what your physical eyes see and record in wave motion in your brain, to be recalled at a later time.
它们只不过是你的肉眼所看见并记录在你的大脑中的波动里的一个复制品，在之后被忆起。
Visual field analysis is interfered by HM fundus dystrophy, also relationship with study curve, long wave motion and short wave motion.
视野分析要结合眼底情况，排除高度近视的影响因素，并注意初检者的学习曲线及视野的短期、长期波动特点。
The numerical wave flume is an effective method in wave study and able to simulate the wave motion better while the NS equation is used.
数值波浪水槽是研究波浪问题的有效数值方法，采用考虑流体粘性的NS方程建立数值波浪水槽，能更好的模拟波浪在近岸的运动过程。
The results given by the present method are in good agreement with results from the linear wave theory which can not give the history of wave motion.
本文计算结果与线性波理论的结果很一致，但后者不能给出波运动的过程。
The group velocity(U) corresponds to the net result from the addition of all elements with different periods and different velocities within the wave motion.
而群速度（U）符合于波动的不同周期，不同速度的各种因素叠加的净结果。
A local transmitting boundary is combined with a lumped-mass finite element technique to form a mechanical model simulating the near field steady wave motion.
本文将局部透射边界和集中质量有限元技术结合起来形成一个模拟稳态近场波动的力学模型。
A new input methods of wave motion dealing with soil-structure interaction is also proposed which can be used to exactly simulate incident seismic wave from any Angle.
文中同时给出了一种结构-地基动力相互作用中地震波动输入方法，可以准确模拟任意角度入射的地震行波的输入。
A new input methods of wave motion dealing with soil-structure interaction is also proposed which can be used to exactly simulate incident seismic wave from any Angle.
文中同时给出了一种结构-地基动力相互作用中地震波动输入方法，可以准确模拟任意角度入射的地震行波的输入。
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