基于宏观基本图的路网多子区状态一致协同控制

针对基于宏观基本图(MFD)的路网多子区协同控制未考虑各子区拥堵状态差异性及均衡性的问题，本文提出以多子区状态可达一致为目标的子区边界状态反馈控制设计方法. 首先，基于路网 MFD模型建立路网多子区协同模型；进一步，基于部分变量稳定性理论，设计多子区状态可达一致的边界状态反馈控制律.在此基础上，考虑子区拥堵状态的差异性，设计了子区间的协同控制策略，快速缓解子区拥堵状态；同时，提出子区边界输入流的分配优化策略.最后，以潍坊市实际路网为背景建立仿真模型.实验结果表明，本文方法可实现子区交通流分布的均衡性，快速缓解子区拥堵状态，较大幅度地提升路网运行效率.     

基于孔隙结构的土体未冻水含量滞回效应研究

冻结特征曲线（SFCC）是描述负温与土体内部未冻水含量之间的关系曲线，是非饱和冻土研究的重要基础。冻融循环是冻土研究的关键因素。以粉土和黏土为试验对象，采用低场核磁共振（NMR）技术，测得了土体在冻融循环作用下的冻结特征曲线和孔隙结构分布图，研究土体在冻融循环作用下冻结特征曲线的变化。试验结果表明：随着循环次数的增加，土体孔隙分布发生了变化，进而导致冻结特征曲线滞回圈和特征温度点的变化，冻结特征曲线变化的本质是孔隙结构的变化；从微观结构出发得到了基于孔隙结构的SFCC表达式，指出融化过程的冻结特征曲线是主冻结特征曲线；结合试验数据的对比分析，模型有效展示了多次冻融循环下土体冻结特征曲线的滞回效应，适用于多次循环下的非饱和冻土。     

磁吹灭弧在五十铃700P车起动继电器上的应用

对2011年的700P载货汽车用起动继电器的结构和原理进行分析,对该起动继电器的磁吹灭弧装置进行计算、验证。该磁吹灭弧装置首次在汽车电器领域应用,开拓了国产起动继电器的设计思路。     

奇摄动三阶非线性边值问题

利用微分不等式技巧和Volterra型积分算子，研究了三阶非线性奇摄动边值问题εx^(3)=f(t,x,x′,w(ε）x^(3)，ε），g（x′（0），x″（0）=0，x（1）=A，x′（1）=B的存在性及渐近估计。     

Fe—21Ni—4Mn合金磁场诱发马氏体形貌和惯习面

本文采用强脉冲磁场、光学显微镜和 H.R.Pak 等提出的惯习面确定方法研究了 Fc-21Ni-4Mn 合金中磁场诱发马氏体形貌和惯习面.结果表明,Fe-21Nj-4Mn 合金冷却形成板条马氏体,而在 Ms 温度以上,磁场诱发形成多片状而少板条马氏体,且随温度升高,磁场诱发马氏体形貌为蝶状.磁场诱发马氏体惯习面与冷却形成的马氏体相同,均为(225),对于蝶状马氏体发现了一种新的对称面(110).     

表面损伤斜拉索雷诺数临界区气动力与流场分析

斜拉索由于具有自身质量轻、结构刚度差、结构阻尼小和自身长细比大的特点，极容易发生风（雨）致振动，对桥梁结构的安全性能产生很大的影响，而斜拉索作为斜拉桥的重要受力构件，准确掌握其风荷载对于桥梁抗风设计具有重要意义，特别是斜拉索在生产、运输和安装过程中表面可能受到损伤，该斜拉索在临界雷诺数区的气动力特性和流场特性更是值得研究的问题。针对此种状况，通过同步测力风洞试验，对表面无损伤斜拉索模型和表面损伤斜拉索模型在不同风攻角下的升力系数进行时程分析，得到边界层转捩的3个区域；将升力系数时程进行快速傅里叶变换计算得到升力时程频谱图，并通过频谱图分析随机信号的频域特征；对比从雷诺数亚临界、临界到超临界区表面无损伤和表面损伤斜拉索的流场变化，并从周围流场变化的角度分析雷诺数临界区斜拉索气动稳定性及可能的机理。研究结果表明：表面无损伤和表面损伤模型的升力系数随雷诺数的变化规律基本一致，二者的升力时程在TrBL0向TrBL1阶段和TrBL1向TrBL2阶段过渡过程中会出现双稳态现象，损伤会影响斜拉索尾流区旋涡脱落的情况，进而对不同雷诺数下的Strouhal数值变化产生一定的影响。     

桥梁结构连同地基的整体计算方法

本文提出将桥梁上部结构、下部结构和基础连同地基整体计算的方法     

Kondo 绝缘体的能隙形成机制

采用格林函数退耦合方法研究了非对称周期性Ａｎｄｅｒｓｏｎ模型．结果表明，在相干区随杂化作用的增强体系有能隙产生，且能隙具有较强的温度依赖．体系的磁化率随温度非单调变化．上述结果与Ｋｏｎｄｏ绝缘体的行为一致．     

Initial results from long-term measurements of atmospheric humidity and related parameters in the marine boundary layer at two locations in the Gulf of Mexico

Measurements of boundary layer moisture have been acquired from Rotronic MP-100 sensors deployed on two NDBC buoys in the northern Gulf of Mexico from June through November 1993. For one sensor, which was retrieved approximately 8 months after deployment, the post- and precalibrations agreed closely and fell well within WMO specifications for accuracy. The second sensor operated continuously from June 1993 to February 1997 (3.5 years). Buoy observations of relative humidity and supporting data were used to calculate specific humidity and the surface fluxes of latent and sensible heat. Specific humidities from the buoys were compared with observations of moisture obtained from nearby ship reports, and the correlations were generally high (0.7–0.9). Surface gravity wave spectra were also acquired. The time series of specific humidity and the other buoy parameters revealed three primary scales of variability, small (h), synoptic (days), and seasonal (months). The synoptic variability was clearly dominant and occurred primarily during September, October, and November. Most of the synoptic variability was due to frontal systems that dropped down into the Gulf of Mexico from the continental US followed by air masses which were cold and dry. Cross-correlation analyses of the buoy data indicated that: (1) the moisture field was highly coherent over distances of 800 km or more in the northern Gulf of Mexico; and (2) both specific humidity and air temperature served as tracers of the motion associated with propagating atmospheric disturbances. These correlation analyses also revealed that the prevailing weather systems generally entered the buoy domain from the South prior to September, but primarily from the North thereafter. Spectra of the various buoy parameters indicated strong diurnal and semidiurnal variability for barometric pressure and sea surface temperature (SST) and lesser variability for air temperature, wind speed and significant wave height. The surface fluxes of latent and sensible heat were dominated by the synoptic events which took place from September through November with the transfer of latent heat being primarily from the ocean to the atmosphere. Finally, an analysis of the surface wave observations from each buoy, which included calculations of wave age and estimates of surface roughness, indicate that major heat and moisture flux events coincide with periods of active wave growth, although the data were insufficient to identify any causal relationships.