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- General Method of Obtaining Double Inverse Scattering Wave Function in Axisymmertric Stationary Einstein Vacuum Field 求取稳态轴对称引力场中二重逆散射方法的非对角波函数
- scattering wave function 散射波函数
- Such a simplified dressed wave function is useful in the calculation of laser-assisted scattering, especially in the laser-assisted rearrangement collisions. 此波函数适用于计算激光辅助的散射过程,特别是重排过程。
- The molecular electronic wave function is perturbed. 分子的电子波函数受到了微扰。
- We now show how to calculate molecular dipole moments from wave function. 我们现在说明如何从波函数来计算分子的偶极矩。
- For complex heterogeneous medium, the distribution and characteristics of its heterogeneity can be studied by seismic scattering wave. 对于复杂非均匀介质,可以利用地震散射波来研究其分布和性质。
- If so we shall have a wave function that satisfies our new postulate. 如果事实确是如此,我们就得到了一个满足新假设的波函数。
- If so we shall have a wave function that satisfies our new postulate . 如果事实确是如此,我们就得到了一个满足新假设的波函数。
- These wave functions correspond to states of constant energy E. 这些波函数对应于具有恒定能量E的态。
- The angular part of a continuum wave function is, of course, a spherical harmonic. 连续谱波函数的角度部分当然是球谐函数。
- These wave functions correspond to states of constant energy E . 这些波函数对应于具有恒定能量e的态。
- In the quantum world, objects are described by wave functions. 在量子的世界中,物体都是以波函数来描述。
- The parity of the eigenfunction is found by determining what happens to the wave function when r is replaced by -r. 本征函数的宇称可以这样确定:当r用-r代替时看波函数的变化。
- Aim To recover the impedance coefficient from the far field pattern of the scattered wave of the acoustic scattering problem with impedance boundary condition. 目的从阻尼边界条件声波散射问题的散射场的远场模式出发去反演阻尼系数。
- Wave function, Schrodingger equation, infinite deep potential well in one dimension. 波函数;薛定谔方程;一维无限深势阱;
- Let's have a look at an interesting feature of the ground-state wave function, Eq(6. 120). 让我们来看基态函数(6.;120)式的有趣图象。
- We start by considering the wave function, ignoring the antisymmetry requirement. 我们先考虑波函数,而暂不顾及它的反对称性要求。
- In this paper, I present three studies on high-frequency seismic attenuation and propose that the physical mechanism results from the interference of elastic microscopic multiple scattering waves. 通常认为地震波高频衰减的物理机制主要是滞弹性的吸收,本文通过如下三方面的研究认为地震波高频衰减的物理机制主要是弹性的微观多次散射波的相互干涉。
- If desired, the perturbed wave function may be normalized at the end of the calculation. 当需要时,可在计算最后将微拢波函数归一化。
- Although the approximate wave function is qualitatively useful, it is gravely lacking in quantitative accuracy. 虽然近似的波函数是定性地有用,然而它严重的缺少定量的准确性。