Ⅲ—Ⅴ族四元固溶体中原子近邻及次近邻的键长表达方式

基于ＦＤＵＣ模型和Ⅲ－Ⅴ族元素共价半径不变的假设，本文出了Ⅲ－Ⅴ族固溶体中原子近邻和次近邻的键长表达式。这套键长表达式除依赖于四个Ⅲ－Ⅴ族元素的含量（ｘ，ｙ）外，只与四个纯化合物的晶胞参数或这四个Ⅲ－Ⅴ族元素的共价半径有关。而且也含盖了相应的伪二元固溶体的情况。本文还对其他的理论模型作了进一步的比较和讨论。     

基于SPM的航空转包生产能力研究

针对国际航空转包对航空制造企业生产能力的要求,分析了航空转包能力的评价构成要素,基于供应商绩效测量标准体系SPM建立了转包能力的模型和转包能力的三维体系结构,并通过三维能力模型的能力分区分层评价对航空企业的转包能力进行分析。该模型及方法能对企业转包能力进行全面评价,发现企业转包生产的能力优势和能力薄弱环节,为企业提高转包能力指明了纠正和完善的方向。     

薄壁结构固有频率的p型有限元数值计算收敛性研究

通过使用MSC．Patran／Nastran中的p型有限元评价多种典型薄壁结构构件动力学品质分析中的特征值计算收敛问题，并对高阶形函数的作用进行了深入分析，从而说明高阶p型体元在薄壁结构建模中的优越性。     

泡沫铝合金镀镍工艺研究

本文研究了在高硅铸铝制备的泡沫铝合金样品上镀镍工艺，提出了一种确定泡沫铝合金表面积的方法。讨论了主盐、还原剂、络合剂、缓冲剂等配方主要成份和ｐＨ 值、温度等工艺条件对化学镀镍的沉积速度和镀层质量的影响，优化了前处理方法，从而得到了适合于泡沫铝合金的镀镍工艺。     

圆柱筒轴向载荷下单元尺寸效应数值模拟

利用显式非线性有限元方法对薄壁圆柱筒轴向载荷下的动力学响应进行了研究,模拟了圆柱筒在轴向冲击作用下的动力屈曲变形及其发展过程。分析比较了不同单元尺度下冲击模型的数值计算解与理论解,揭示了在进行有限元模拟时存在的网格尺寸效应,为研究有限元网格尺寸与有限元求解精度的内在联系提供参考;为在保证数值解满足工程实际精度要求的前提下,确定合理的单元尺度,提高有限元分析效率进行了有益的探索。     

英语学习策略与大学英语四级通过情况的相关性研究——以桂林航天工业高等专科学校为例

论文通过对桂林航天工业高等专科学校部分学生的英语学习策略调查问卷及相关数据进行SPSS数据分析,分析通过大学英语四级的学生英语学习策略使用情况,及通过分析调查对象的英语学习策略使用情况,是否知道学习策略对于学习策略的选择的影响,各学习策略之间的关系等提出,指导学生,提高大学英语四级通过率。     

基于内禀属性的扇区复杂性评估

为了定量描述空域扇区的复杂性,引入交通内禀性概念,通过计算扇区内航空器间的逼近时间、侵略函数、关系矩阵、相关度函数,建立扇区的复杂性测度模型；并通过仿真算例,对扇区复杂度影响因素进行了分析.研究结果表明:复杂性值大小反映了扇区内飞机数量及汇聚、分散程度,复杂性值曲线拐点数量反映了扇区交通有序/无序程度,复杂性值曲线突变反映了扇区交通数量变化情况,可为管制员的监视和冲突解脱方案选择提供一定支持.     

Atmospheric response to a Hot SST Event in November 2006 as observed by the AIRS instrument

Using Atmospheric Infrared Sounder (AIRS) products of atmospheric temperature and geopotential height, we investigate the atmospheric response to HE0611, which was found and investigated by [Qin, H., Kawamura, H., Sakaida, F., Ando, K. A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array. J. Geophys. Res. 113, C08045, doi: 10.1029/2007JC004640, 2008]. HE0611 was formed by connecting two very high SST areas, HE0611-East and HE0611-West. The period-mean atmosphere temperatures at levels of 925 and 850 hPa in HE0611-West are higher, by about 0.5 K, than those in WE0611-East while the atmospheric temperatures at middle to high levels (700–300 hPa) are higher in HE0611-East. The period-mean geopotential heights HE0611-East are much lower than those in HE0611-West for the levels from the surface to 400 hPa. The mean geopotential heights from 400 hPa to 200 hPa are higher in HE0611-East. In the middle and high layers over HE0611-West, the atmosphere temperatures gradually decrease from 7th to 17th, and then increase significantly. The increase in HE0611-East starts from 15th November, which is earlier than that of HE0611-West. The geopotential heights in the high layer of both the areas also show corresponding behaviors. The lagged atmospheric response in the western part is confirmed by the correlation analysis. It emerges that the atmospheric response to HE0611 is well organized and associated with deep convention in HE0611-East and subsidence in HE0611-West. These are also consistent with the HE0611 features and evolution revealed by earlier HE studies.     

Mathematical modeling of heat transfer process in a variable domain

In this paper, a brief review and generalization of studies on the heat transfer and heat conduction problem in a variable domain are presented. The equations of the process, where the boundary displacement velocity is the control, are obtained taking into account heat inflow. This article was submitted by the authors in English.