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isotropic相关的网络例句

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与 isotropic 相关的网络例句 [注:此内容来源于网络,仅供参考]

The results of 3-D numerical modeling of the transversely isotropic media with horizontal symmetry axis and the orthorhombic symmetry media showed that quasi P wave,quasi-SV wave and quasi-SH wave occurred during elastic wave propagation in 3-D anisotropic media. Meanwhile, the special phenomena such as the S wave splitting, the blind zone of S wave splitting and quasi-SV wave-front triplication were clearly observed. In addition, the elastic wave-fronts are spatially changed, and the coupled relations among the quasi-P wave,quasi-SV wave and quasiSH wave in 3-D anisotropic media are very complex.

对方位各向异性介质模型和正交各向异性介质模型中弹性波的传播进行的三维数值模拟结果表明,弹性波在三维各向异性介质中传播时存在拟P波、拟SV波和拟SH波,并出现横波分裂、横波分裂盲区、波面三分叉等特殊现象,另外,性波场在空间是变化的,其拟P波、拟SV波和拟SH波的耦合关系比较复杂。

In contrast to the situation for a homogeneous isotropic neo-Hookean sphere, it is shown that not only there exists a secondary turning bifurcation point on the cavitated bifurcation solution which bifurcates locally to the left from trivial solution, and also the critical load is smaller than that for the material with no perturbations, as the parameters belong to some regions.

与均匀各向同性的neo-Hookean球体的情况相比,证明了当摄动参数属于某些区域时,从平凡解局部向左分岔的空穴分岔解上存在一个二次转向分岔点,空穴生成时的临界载荷会比无摄动的材料的临界载荷小。

Novel uncoupled and 24 fully-isotropic solutions are obtained.

得到了24种新型无耦合并联机构方案和24种完全各向同性并联机构方案。

Then,two geologic models were designed,including layered model and interface undulated model,which were used to carry out post-stack reverse time migration by spectral element method on forward modeling results in anisotropic and isotropic medium.

设计了层状和界面起伏两个地质模型,分别在各向异性介质和各向同性介质条件下对正演模拟结果进行了谱元法叠后逆时偏移。

Based on the principle of plastic work equivalent per unit volume, Drucker flow rule and isotropic hardening model, a new expression of stress-strain relationship of biaxial tension for different loading paths, which used firsthand uniaxile tension test data, were derived from existing yield criteria such as Hill48, Hill90, Barlat89, Hosford and Mises yield criteria.

根据单位体积塑性功相等原理,基于Druker公设以及等向强化模型,利用比例加载的特点,推导出板料在无卸载比例加载路径下的双向拉伸本构模型,并给出几种不同屈服准则下的本构模型。

An electromagnetic wave is propagating along the z-axis in an isotropic medium.

在一各向同性的介质中,电磁波沿z-轴传播。

As the aeolotropism development of cracks in carbonate reservoir, so far not a very good seismic reservoir crosswise prediction method application for the aeolotropism carbonate reservoir, especially in the seismic, logging joint inversion, is mainly continues to use the reservoir crosswise prediction method that suitable for the isotropic clastic rock reservoir.

由于碳酸盐岩储层裂缝发育的非均质性,到目前为止还没有一套推广应用很好的针对碳酸盐岩非均质性储层进行地震储层横向预测的方法,尤其是在地震、测井联合反演方面,主要是沿用适合于较均质的碎屑岩储层地震横向预测技术。

Secondly, 4 methods of azimuth estimation based on vector hydrophone according to forms of nosie and signal are brought forward. The principles of these 4methods are set forth, simulating them by computer. Acoustic intensity averager can effectively suppress isotropic non-coherent interference; DOA based on line-spectra can effectively detect the target radiating line-spectra and estimate its azimuth angle; Bar graph approach can suppress line-spectra coherent interference and distinguish different targets radiating line-spectrum. Weighted bargraph approach can detect target in broadband coherent interference and estimate its azimuth angle.

其次,根据背景干扰和信号样式的不同,提出了单矢量水听器方位估计的4种方法;阐述了这4种方法的原理,并进行了计算机仿真,指出平均声强器方位估计适用于各向同性噪声场背景干扰,讨论了平均声强器的处理增益;目标辐射噪声中有线谱时,线谱方位估计有很好的性能,其中的LOFAR线谱和高频解调得到的DEMON线谱都是目标的特征谱线,可以利用它们进行方位估计,详细讨论了利用特征线谱单个矢量水听器分辨多目标的性能;直方图方位估计能抗强线谱相干干扰;加权直方图方位估计可以抗宽带相干干扰。

Amorphous alloys have gained much attention as novel catalytically active materials due to their unique isotropic structural and chemical properties.

非晶态合金由于具有独特的结构和化学特性,作为一种新型催化材料,已引起人们的广泛重视。

By simulating and spitting of the line atδ145, we were able to show five isotropic components at δ134.6,δ139.6,δ145.1,δ147.9 and δ149.1, and the numbers the inequivalent sp2 carbons neatly dovetailed with the integral areas of the every line.

我们利用拟合分峰的方法得出了这五个不等价的碳原子的峰的位置,分别位于δ134.6、δ139.6、δ145.1、δ147.9 以及δ149.1,这五个不等价的碳原子数目上的比例关系和核磁共振曲线的积分面积吻合。

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