地震动时频分析在隧道动力响应分析中的应用

为了了解影响隧道动态内力峰值出现位置的相关因素.利用希尔伯特—黄变换,对E1 Centro等4条天然地震波和某隧道人工波(简称LBG地震波)进行了时频分析,结果表明:1)地震波各频段内所含能量的大小是影响隧道动态响应的主要因素;2)地震波中所包含的瞬时能量和总能量在时域上的分布决定了隧道内力及塑性应变最大峰值的出现时间;3)隧道内力峰值及最大塑性应变出现的位置与隧道断面形状及周围介质对衬砌的约束状态有关,与地震波的类型无关.     

Constitutive equations and finite element implementation of strain localization in sand deformation

A recently proposed model coupling with the solid-fluid of the saturated sand was utilized to study the deformation band. Based on the critical state plasticity model by Borja and Andrade, the hydraulic conductivity tensor was naturally treated as a function of the spatial discretization matrix about the displacement and the stress field, allowing a more realistic representation of the physical phenomenon. The fully Lagrangian form of the Darcy law was resolved by Piola algorithm, and then the flow law was gained, leading to the implementation of a modified model of the saturated sand. Then the criterion for the onset of localization was derived and utilized to detect instability. The constitutive model was implemented in a finite element program coded by FORTRAN, which was used to predict the formation and development of shear bands in plane strain compression of saturated sand. At last, the formation mechanism of the shear band was discussed. It is shown that the model works well, and the simulation sample bifurcates at 1.18% axial strain, which is in a good qualitative agreement with the experiment. The pore pressure greatly affects the onset and development of the deformation band, and it obviously increases around the localization-prone regions with the direction toward the outer side of the normal of the shear band, while the pore stress flows nearly horizontally and is distributed equally far away the shear band region. Foundation item: Project(2006G007-C) supported by the Foundation of the Science and Technology Section of Ministry of Railway of China; Project(77206) supported by the Excellent PhD Thesis Innovation Foundation of Central South University, China     

论传统文化中色彩元素与视觉传达的关系

传统文化包含众多的元素,作者对传统文化元素中的色彩元素在现代视觉传达设计中的运用与影响进行了研究,分别就中国传统色彩在包装设计、标志设计以及环境设计中的运用进行了论述,并阐释了如何实现现代元素与传统文化元素在现代视觉传达设计中的完美统一,最终达到在现代视觉传达设计中传承和发展优秀传统文化的目的.     

Nd8-xDyxFe82Co6B4纳米复合永磁材料的磁性能

针对NdFeB纳米复合永磁材料的矫顽力偏低的现状,采用熔体快淬法制备了Nd8DyxFe82Co6B4（x=0,0．4,0．8,1．2,1．6）纳米复合永磁材料,研究了Dy和Co的添加对NdFeB纳米复合永磁材料的磁性能的影响．研究结果表明,Dy的添加可提高材料的各向异性场,提高矫顽力,但是Dy元素的添加使材料的剩磁降低,结晶温度升高,因此添加量不宜过多;复合添加Co原子不仅可以提高材料的剩磁和矫顽力,而且可以弥补只添加Dy元素使材料的结晶温度升高的缺陷．在最佳的热处理条件下,Dy含量x=0．8时的样品表现出最佳的磁性能,矫顽力jHc=524kA／m,剩磁Br=1．11T,最大磁能积（BH）max=158kJ／m^3．     

二维弹性问题线性单元边界元法奇异积分问题的处理

采用线性单元的二维弹性问题边界元法具有计算精度高的优点。但当点力所在结点与单元的端结点重合时,出现了奇异积分问题。本工作提出了解决奇异积分问题的一个方法,编制了二维弹性问题线性单元边界元法程序,并给出了两个算例。算例中讨论了角结点附近面力的处理问题。结果表明,本工作编制的边界元法程序是可靠的。     

基于折射定律的摄像机标定模型

传统的摄像机标定是基于针孔模型,把镜头简化为凸透镜,得出的是光学元件的集总参数,精确度低.为提高精度,根据折射定律提出基于折射定律的摄像机标定模型.上述模型细化了摄像机镜头的组成,把镜头分为三个透镜部分,并且应用折射定律定性研究光线在透镜边界面的折射情况.改进模型充分考虑了摄像机镜头的透镜组成,大大提高了标定的精确度.仿真结果表明,新模型与针孔模型相比,平均误差值明显降低.并且比较了摄像机与物体的距离不同时,误差值的变化,确定了标定时的最佳距离.     

基于边界扫描技术的设计复杂性优化研究

对于边界扫描技术的电路系统,可利用现代优化算法对其进行复杂性和测试性改善度的综合优化。主要以较小的复杂性设计来实现测试性的最大化改善,以提高系统测试性优化和缩短系统的测试时间。应用模拟退火算法和模拟退火遗传算法实现系统的设计复杂性优化,相比于贪婪算法,模拟退火算法和模拟退火遗传算法能得到更好的优化率。     

基于CRF的中文评论有效性挖掘产品特征

方面级意见挖掘的任务通常包括从客户评论中抽取产品的特征、与产品特征相关联的观点词识别以及观点的极性判断三个方面。围绕如何实现中文评论的方面级意见挖掘问题,提出了利用条件随机场实现中文评论的方面级意见挖掘的四个主要步骤：数据预处理、训练集准备、为条件随机场模型定义学习函数、应用模型标注新的评论数据。在此基础上,通过以五种实际产品的中文评论语料为数据集,对该方法进行了数据实验。实验结果表明,该方法针对不同类型观点元素的抽取在评估性能指标上大部分达到或超过80%。为了进一步验证所提出方法的有效性,将研究结果进行了差异显著性检验。结果显示,用CRF对中文评论进行方面级意见挖掘和对英文评论的方面意见挖掘的性能差异不大。最后,比较了三种不同方法的方面抽取精度和情感分类精度,实验结果表明,CRF方法优于词典化的隐马尔可夫模型和关联规则挖掘方法。     

Trace element geochemistry of the Obed Mountain deposit coals, Alberta, Canada

This study reports on the elemental concentrations and vertical variation of coal seams from the Obed Mountain deposit, Alberta Foothills, Canada. Results from two sections of Seam 1 show that the major elements (i.e. Al, Fe, Mg, K, Na, Ti, and Si) have high concentrations in intervals having high ash content, with the only exception of Ca. Similarities are apparent, in both sections, in the vertical variations of Th, U, Se, and Zn; Rb, Cs, and K; Sb, Mo, and W; Mn and Sr; and Ba, Cr, Co, Hf, and Sc. These similarities are also evident among the REEs, notably between Ce and La; also between Dy, Eu, and Sm. Most elements, with the exception of Ba and Sr are slightly more concentrated in Section 2 of Seam 1, located approximately 1.5Fig. km away from Section 1. Compared to Seam 1, Seam 2 has lower mean concentrations of elements. Boron in the coal ranges from 27 to 100 ppmw, though most values are less than 50 ppmw. Boron concentrations suggest a freshwater depositional environment. The element is depleted in the sedimentary partings (12–29 ppmw only) and is enriched in the coal interval near the roof and immediately beneath the partings. This enrichment shows possible downward mobilization of boron. Vertical variations of elements are helpful in delineating the boundaries between coal and sedimentary partings in the succession. The Obed Mountain coals are “clean” by world standards and their elemental concentrations are comparable with those in coals of a lower rank from the same coal formation used for power generation in Alberta. All sedimentary partings have low concentrations of Ba, Hf, Sc, Sr, Ta, Th, U, and REEs; this, along with the absence of an Eu negative anomaly suggests a non-volcanic origin for the partings.     

Selective separation of yttrium from rare earth elements by ion interaction chromatography. Analytical and larger scale applications

ABSTRACT

New ion interaction chromatographic (IIC) method employing Kromasil 100 C₁₈ column and tetra-n-butylammonium hydroxide (TBAOH) as an ion interaction reagent (IIR) is able to separate yttrium from Rare Earth Elements (REE) as anionic complexes with nitrilotriacetic acid (NTA). New method for the chromatographic determination of Y in REE mixture was devised and validated by the analysis of the certified reference material (CRM). Potential possibilities of the new chromatographic system for larger scale applications including macro-micro events were demonstrated.