在这样的界面上电磁波、热波、光波和声波能够反射。
Waves of electromagnetism, heat, light and sound can be reflected at such an interface.
在由非水平裂隙构成的界面上，P-P波反射系数会出现更多的极值而变得较为复杂，且不能直接指示裂隙走向。
On the interface where there are non-horizontal fractures, reflection coefficient of P-P wave has more extrema to show complexity and to fail to directly indicate fracture strike.
该算法使用射线追踪计算传播时间，应用波场界面方程计算反射振幅。
This algorithm USES ray tracing to calculate traveltime, and DE - rives reflection amplitude from wave field interface equation.
研究简谐弹性波在一般各向异性介质单侧接触界面上的反射和折射问题。
Reflection and refraction of harmonic elastic waves at a unilateral frictional contact interface is studied theoretically in this paper.
因为晶格振动的波在达到界面时会被反射，所以镜面反射边界条件与循环边界条件相比更符合晶格振动的特点。
Lattice wave will be reflected when it reaches the boundary so that the reflecting boundary condition is more reasonable than cyclic boundary.
我们看到，(7.7.6)代表平面SH波在分界面上的反射和折射。
We see that (7.7. 6) represents the reflection and refraction of plane SH-waves from the interface.
本文提出了一种利用反射波走时曲线计算垂向非均匀介质速度和反射界面深度的方法。
A method is presented, which makes it possible to calculate velocity and interface depth of the reflected wave in a vertically inhomogeneous medium.
导电介质中的平面电磁波在介质的分界面上也发生反射与透射。
The plane electromagnetic wave in an electric medium also reflects and transmits on the interfaces.
DMO方法能够使来自不同倾斜界面的反射波同时得到有效叠加。
DMO method can cause satisfactory stack result of the reflection waves which come from different dip reflectors.
本文讨论了声学介质与弹性介质在单界面和多层介质情况下平面波反射系数的实质。
This paper deals with the essence of the reflection coefficient of planar wave in terms of acoustic and elastic media in the single-boundary and multilayered medium.
分析有限声波束从平面液-固界面上散射的困难主要发生在平面波反射系数的处理上。
For scattering of a bounded acoustic beam from a liquid-solid interface, the principal difficulty comes from the treatment of tie plane wave reflection coefficient.
理论上，各向同性介质中三维倾斜界面P波反射时距是双曲线。 在一定。
The time-distance curve is a hyperbola when the P-wave is reflected from a 3D dipping interface in isotropic media .
据此，就三维地震反射面接收，本文对三维倾斜界面以及各向异性对P波时距特征的影响做计算讨论。
This thesis attempts to evaluate the effects of a 3D dipping interface within anisotropic media for the time-distance features of reflected P-wave.
研究结果表明，该区不同界面的首波和反射波具有不同的特征。
The result shows that the head waves and reflected waves from different interfaces in this region possess different characteristics.
从理论上计算了同一强度的入射冲击波在不同材料界面上产生的反射冲击波强度。
For an incident shock wave, the strength of reflected shock waves from the boundary of different materials are calculated theoretically.
再往南从35公里深度来的反射波是来自印度半岛的莫霍界面。
Even further south, reflections from 35 km depth may correspond to the Moho of peninsular India.
利用FDTD法和PML技术计算分析了平面分界面对脉冲波的反射和折射，充分而形象地描绘平面界面对脉冲波反射的时域过程。
The reflection and the refraction of the pulse electromagnetic waves at a dielectric interface were calculated and analyzed based on the FDTD method and PML technique.
对于严重缺陷的反射波特征，重点区别了同一缺陷界面的多次反射和多缺陷反射在反射波曲线上的差别；
To study the curve characteristics of shallow severe defects, I distinguished the multi-defective pile from the same defect interface.
考虑入射波在两种介质界面上会产生反射和透射，故在总场边界上引入入射波、反射波和透射波。
Owing to the presence of interface of dielectric and air, it is required to impose three waves, including incident plane wave, reflected and transmitted waves at the total-scattered field boundary.
文中给出了该区P波反射法探测基岩界面、溶洞、断层和溶蚀带分布的应用实例。
A case history of the application of the P-wave reflection method in that area to investigate the bedding plane of bedrock, karst cave, fault and the distribution of the dissolution belt is given.
利用子波分析了SIR - 10雷达所测得的隧道衬砌数据，在某一尺度上清楚地得到了三个界面的反射波。
The data measured by SIR-10 radar are analyzed by wavelets. The three reflected waves can be so clearly distinguished and the tunnel-lining thickness and void size are easily detected.
一般来说，波在传播过程中遇到位势间断或界面时会发生折射反射。
In general, waves would be re? Ected and transmitted when crossing the discontinuous potential or medium interface.
巷道对各道直达波能量分布及波列形状有明显影响；煤岩分界面主要影响反射波能量分布。
The shape and energy distribution of direct wave is mainly influenced by drift, while the energy distribution of reflected wave is influenced mainly by the interface between coal and rock.
再往南从35公里深度来的反射波是来自印度半岛的莫霍界面。
Even further south, reflections from 35km depth may correspond to the Moho of peninsular India.
再往南从35公里深度来的反射波是来自印度半岛的莫霍界面。
Even further south, reflections from 35km depth may correspond to the Moho of peninsular India.
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