视频汇流环的设计与研究

作者在文献[1]中从理论上阐明了视频汇流环的小型化设计。本文着重介绍视频汇流环的电器设计和它的测试方法。     

高阶非线性时滞方程振动的充要条件及比较定理

本文首先给出了高阶非线性时滞微分方程所有解振动的充要条件。然后利用该结果，得到了一些振动的比较定理，解决了张炳根猜想。     

关于Sauer引理的一个推广

Sauer引理是统计学习理论中的基本结论．在许多实际问题中，需要研究N类模式识别问题．本文将Sauer引理推广到N类分类问题．     

模糊Riemann-Stieltjes积分的收敛定理

模糊Riemann-Stieltjes积分是模糊分析中的一类重要的模糊积分,但相应的积分序列的收敛定理尚未见到.将给出模糊数值函数列关于实函数和模糊数值函数关于实函数列的两类模糊Riemann-Stiehjes积分序列的收敛定理.     

化学键参数函数与标准电极电位

采用多元线性回归方法对常用元素的结构参数及其标准电极电位对定量结构性质相关(QSPR)模型进行研究,结果显示,电负性、电离能等结构参数与元素标准电极电位之间有较好的线性相关性.     

铁路货运营销综合信息平台研究

针对货运营销综合数据仓库的构建提出一整套完整的解决方案。通过构建货运营销数据仓库，形成完整、一致、正确的数据集合，实现对历史数据的积累，并将成为铁路货运营销部门统一的、高质量的基础信息数据库。     

葡萄酒月度价格指标的季节ARIMA时间序列分析

以时间序列分析为工具,研究了法国葡萄酒价格月度指标,使用基于周期图的Fisher检验证实该数据指标具有潜在周期,最后发现(1,0,0)×(1,0,0)12模型能较好地拟合数据.在此基础上给出相应的预测.     

A Brief Discussion on Streaming Teaching for Non-English Majors in Vocational & Technological Colleges

Streaming teaching is adopted gradually for non-English majors in some vocational & technological colleges,and in this thesis the advantages and problems of the method are discussed according to the teaching practice.Furthermore,as a consideration of the streaming teaching,much more progress is expected to be made in the future English teaching with the help of the thesis.     

A theoretical model for mid-and low-latitude ionospheric electric fields in realistic geomagnetic fields

The geomagnetic fields, which play important roles in the ionospheric dynamo, can greatly affect the global distribution of ionospheric electric fields, currents and other ionospheric electrodynamics phenomena. In the study of ionospheric electrodynamics phenomena, such as the longitudinal variations of ionospheric electric fields, the non-dipolar component of the geomagnetic fields must be taken into account. In this paper, we deduce a theoretical electric field model for ionospheric dynamo at mid- and low-latitude which adopt a modified magnetic apex coordinates system. In the new electric field model, the geomagnetic fields can be calculated from either the IGRF model or the dipole field model, and the neutral winds and conductivities are calculated based on empirical models. Then the dynamo equation for the electric potential is finally solved in terms of the line-by-line iteration method, and the ionospheric electric fields and currents are derived from the calculated potential. Our model can reproduce the main features of the ionospheric electrodynamics processes, so it will be a useful tool for the investigation of the upper atmosphere and ionosphere.