在各向异性介质中磁向量势的多极矩展开

本文给出在线性各向异性介质中磁向量势(?)的多极展开,指出它的特点,并由此导出相应的各级磁场,为研究磁各向异性的磁场提供一个范例.     

岩心磁组构分析古水流方向的原理与应用

目的针对鄂尔多斯盆地天环拗陷南段延长组开展磁组构古水流研究。方法通过测量岩心样品的磁化率各向异性,分析磁组构特征,结合矿物岩石学特征综合开展岩心古水流方向判识。结果延长组碎屑岩的古水流方向为NE—SW,NW—SE和NS向,分别代表西南、西北和北部3个方向的物质供给。结论磁组构分析古水流方向与轻重矿物组合法判断的物源方向一致,表明应用磁组构分析钻井岩心古水流方向的方法是可行、可靠的,利用磁组构分析方法恢复古水流方向,判识物源具有较好的应用前景。     

非晶Tb-Gd-Co合金薄膜特性研究

磁光存储材料的研充,最重要的是探求实用化磁光介质薄膜材料和制备工艺.非晶稀土-过渡金属(以下缩写为RE-TM)材料,适于使用制作磁光盘已崭露头角,由三元合金Gd-Fe-Co或Tb-Fe-Co膜做成的磁光盘样机已经问世.在以(Tb,Gd)_x-(Fe,Co)_(1-x)为基础的合金薄膜系列里,Tb-Gd-Co比Gd-Fe-Co有更大的矫顽力,这对提高存储密度是有利的.此外,Tb-Gd-Co材料还可以提供稍大的克尔(Kerr)旋转角θ_k和宽温特性.近年来,人们很重视非晶Tb-Gd-Co膜的研究,Togami首先报道Tb-Gd-Co膜,随后,Luborsky等人从实验肯定Tb-Gd-Co膜用作磁光介质的稳定性.为使Tb-Gd-Co材料达到实用化,本文研究了溅射参数对非晶Tb-Gd-Co合金薄膜特性的影响,获得了比较好的     

Optimization of Permeability Tensor Characteristics of Anisotropic Reservoir and Well Pattern Parameters

The problems of well pattern arrangement, well array direction, and well array spacing ratios for anisotropic reservoirs were studied using tensor analysis. The problems were formulated as a bilevel programming model which was solved using a genetic algorithm. The results show that if the permeability in one direction is much higher than in another direction, the wells should be aligned along the high permeability direction. The analysis provides a theoretical foundation for well pattern arrangement in fractured reservoirs as well as in channel sand reservoirs.     

Exchange-coupling interaction, effective anisotropy and magnetic property of nano-magnetic materials

The theories and models of exchange-coupling interaction between grains in nanocrystalline magnetic materials are introduced here. Their insufficiencies and distinctions from the experimental results are pointed out, and some revisions are made. The effects of the phase component ratio, the grain size and microstructure on the effective anisotropy and magnetic properties in the nanocomposite permanent materials and the improved models are discussed in detail.     

Velocity Modeling and Inversion Techniques for Locating Microseismic Events in Unconventional Reservoirs

A velocity model is an important factor influencing microseismic event locations. We re-view the velocity modeling and inversion techniques for locating microseismic events in exploration for unconvent...     

粘弹性方程各向异性有限元方法的超收敛分析

克服了传统有限元要求剖分网格满足正则假设(或拟一致假设)的限制,在一种新定义的各向异性网格———广义拟一致网格上,分析了粘弹性方程双线性有限元解的超逼近性质,并给出相应的超收敛结果。     

C_4~(2+)分子的E_g b_(1g)系统的Jahn-Teller效应及其各向异性现象

依据Jahn-Teller效应理论与量子理论,利用群论和对称性分析的方法探讨了C42+分子的Eg b1g系统的Jahn-Teller效应及其各向异性现象,构建了Eg b1g系统的电声耦合哈密顿量,借助幺正平移变换计算出了系统的电子基态与激发态及其能量.结果表明,由于电声耦合作用的缘故,系统发生了Jahn-Teller畸变,畸变使得系统在其势能面上形成了两个具有D2h对称性势阱.无论系统处在哪一个势阱中,系统的二重简并的电子基态能级都将发生分裂,因此畸变导致系统电子基态的简并性完全被消除.经过Jahn-Teller畸变,C42+分子就会从D4h对称性降低到D2h对称性,同时C42+分子的振动频率发生分解,频率的分解就意味着C42+分子的各向同性遭到破坏而呈现出各向异性.     

髋关节内置假体设计方法

提出一种新的内置假体设计方法.先利用股骨CT图像数据,通过提取股骨外形及髓腔轮廓线并进行封闭、光顺处理,然后根据股骨髓腔几何解剖状态设计个体股骨假体.利用股骨CT图像中每个象素的CT值和ANSYS软件提供的参数设计语言APDL进行二次开发并形成自主开发的材料属性赋值程序.有限元分析时调用研发的材料属性赋值程序,将股骨有限元模型的每一单元赋予相应的材料属性,实现股骨有限元模型每个单元材料正确的非均匀及各向异性描述,在此基础上进行有限元计算和接触有限元计算,对比置换前后股骨的应力分布情况及大小,检验假体设计的合理性.研究结果表明这种假体设计和分析方法更为合理、可靠.     

Crust-mantle coupling in North China: Preliminary analysis from seismic anisotropy

Data from the CASN (Capital Area Seismograph Network), NSNC (National Seismograph Network of China), and IRIS (Incor-porated Research Institutions for Seismology) are compared with data from a temporary North China Seismic Array to obtain the background orientation of the horizontal crustal principal compressive stress at NE 95.1°±15.4° in North China. Data are corrected for disturbances of faults and irregular tectonics, and are used to constrain the fast SKS polarization at NE 110.2°±15.8° in North China. Individual station analyses suggests that there is consistently more than 10° difference between the polarizations of fast shear-wave in the crust and those of fast SKS phases. Azimuthally anisotropic phase velocities of Rayleigh waves at different periods also indicate an orientation change for fast velocity with depth. It suggests the crust-mantle coupling in North China follows neither the simple decoupling model nor the strong coupling model. Instead, it is possibly some inhomogeneous combination of two models or some gradual-change model of physical characteristics. This study shows that anisotropy in the crust and mantle could be multiply characterized more correctly and crust-mantle coupling could be analyzed further, if increasing near-field shear-wave splitting data that indicate crustal anisotropy, combined with the azimuthal anisotropy of Rayleigh waves, besides the result of SKS splitting travelling through lithosphere and surface GPS measurements.