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In addition, we also investigated polarization anisotropy and SKS wave spliting for comparison.

此外,我们还对面波的偏振各向异性作了探讨,用SKS波分裂方法作了各向异性的对比研究。

Correlation of drillability anisotropy index of the roller cone bit and PDC bit, the difference between drillability of the roller cone bit in perpendicular and horizontal directions of the bedding plane with the P-wave velocity anisotropy coefficient are studied respectively by means of mathematical statistics. A mathematical model is established for predicting drillability anisotropy index by using P-wave velocity anisotropy coefficient.

用数理统计方法研究分析了牙轮钻头岩石可钻性各向异性指数、牙轮钻头垂直于和平行于地层层面方向岩石可钻性差值和PDC钻头岩石可钻性各向异性指数与纵波波速各向异性系数的相关关系,建立了用纵波波速各向异性系数评价地层可钻性各向异性的模型。

A second-order symmetric fabric tensor is introduced to the model, such as the stiffness of the contact planes, the hardening parameter, the dilatant/ contractant coefficient are made dependent of the orientation of the contact plane in order to capture the inherent and stress induced anisotropic behavior of clay.

在上述考虑微结构的饱和软粘土的弹塑性本构模型的基础上将考虑组构的各向异性的二阶组构张量引入接触面上的刚度、硬化参数、剪胀系数等参数中,由此反映材料引起的各向异性和应力引起的各向异性。

In addition, the stress anisotropy in the Gd-Fe alloy thin films was calculated by the magnetostriction effect, and the mechanisms for the origin of perpendicular anisotropy was also discussed.

另外,还通过磁致伸缩效应计算了Gd-Fe膜的应力各向异性能,并对垂直各向异性的产生机制作了讨论。

Optically anisotropic PDLC films can be acted as scattering polarizers with optimal electro-optical properties. The optical anisotropy characters of oriented PDLC films are analyzed.

对PDLC的光学各向异性进行了研究,并给出了要获得低阈值电压、高各向异性的聚合物分散液晶各向异性膜的盒厚、摩擦强度以及光照强度等条件。

In Chapter 5, we study three dimensional elasto-plastic frictional contact problems with orthotropic friction law. Parametric variational principle and parametric quadratic programming method are applied to analyze this class of complicated mechanics problems. A linear complementarity problem formulation is derived.

在第五章,我们采用正交各向异性摩擦定律模型对三维弹塑性摩擦接触问题进行分析,将正交各向异性的摩擦定律线性化后,将参变量变分原理和参数二次规划法应用到这一复杂的力学问题中来,最终将问题化为线性互补问题模型。

ADP is applied to model the different distributions of clay in shaly sand, and the effect of different distribution of clay is studied. Three anisotropic effective medim models are developed according to different distribution of clay.

应用双重孔隙各向异性有效介质模型分别对三种不同泥质分布形式的泥质砂岩进行了数值模拟,考察了不同分布形式的泥质对泥质砂岩的影响,分别建立了相应的各向异性有效介质模型,并对三种分布形式的泥质对泥质砂岩各向异性的影响进行了分析。

Our investigation has shown that:ⅰ there was an interference effect between the incident and reflected matter waves as all the atoms in BECs were coherent;ⅱ considering the rotation of a vortex, the nonuniform velocity distribution along the surface would play an important role in the quantum reflection process. For example, they would change the characteristics of the interference fringes between the incident and reflected matter waves;ⅲ the reflected vortex became unstable for sufficiently low incident velocity or strong interaction. This sort of instability physically originated from dynamics excitations induced by the atomic interaction in the quantum reflection process.

我们的研究表明:ⅰ由于相干性质的存在,在涡旋与固体表面相互作用的过程中,被固体表面反射回去的部分与正在入射的部分在空间叠加后一定会产生清晰的干涉条纹;ⅱ由于各向异性的速度分布,涡旋的反射率也呈各向异性,因此反射回来的部分与入射部分形成的干涉条纹宽度以及疏密程度与入射速度以及速度各向异性的程度有关;ⅲ由于玻色凝聚体中原子间相互作用的存在,反射过程中凝聚体会产生激发,破坏涡旋的结构,使得反射后的涡旋不再是中心对称。

The method is deployed to process the crossed dipole data, thus to identify the types of anisotropies from the dispersion characters of fast and slow flexural waves, those types include:①the coincidence of dispersion curves of anisotropic formation;②the parallel of dispersi...

用该方法处理了某井正交偶极资料,从快、慢弯曲波的频散特性中识别出各向异性的类型:①各向同性地层频散曲线重合;②固有的各向异性地层频散曲线平行;③应力引起的各向异性地层频散曲线交叉。

Moreover, strong anisotropy is observed in the north and southcentral Tien Shan. Fast Pn velocity in the southcentral Tien Shan is nearly in NS directions, which is consistent with the SKS wave anisotropy concerning mantle flow. However, fast Pn velocity directions in the northcentral Tien Shan show a southward rotation variation. We estimate that it is probably related to the inserting of the crust of the Chu basin from the southern Kazakhstan platform to the central Tien Shan, which caused a change of stress fields and lithosphere deformation.

中天山北部和南部的各向异性也存在一定的差异,南部各向异性的快波方向为近南北方向,与SKS波的各向异性特征基本一致,反映了地幔物质的迁移方向;北部各向异性的快波方向呈向南凸出的旋转趋势,估计与哈萨克地台南缘楚河盆地地壳块体向天山挤入造成应力场的改变和岩石层变形有关。

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