单洞双线铁路隧道仰拱施工质量控制技术研究

为有效解决和控制仰拱厚度不够、强度不足、施工缝翻浆冒泥及上拱等施工质量问题,保障隧道工程建设和运营安全,依托渝昆高铁昭通隧道工程,采用隧道扫描系统检测仰拱开挖断面,确保仰拱厚度满足设计要求;采用液压自行式整体仰拱栈桥,优化仰拱弧形模板,实现分段分层浇筑和振捣工艺,提高混凝土施工质量;采用分离式仰拱端头钢模板,预铺仰拱端头弧形带并安装橡胶背贴和中埋止水带,提高了施工缝质量,减少了施工缝翻浆冒泥现象;设置隧底纵向排水管及逆向导水管等优化隧底排水设计措施,解决了水害造成的仰拱上拱问题;制定并落实隧道仰拱施工质量管理措施。通过在渝昆高铁昭通隧道施工中采取以上措施,实现了仰拱零欠厚,仰拱混凝土强度满足设计要求,施工缝质量零缺陷。     

蒸汽调节阀手自动转换装置优化及试验

对汽轮机蒸汽调节阀手动自动转换装置进行优化改进和试验研究,提高了装置的使用寿命以及汽轮机运行安全性和可靠性,具有重要意义。     

基于键图理论的汽车平顺性仿真分析

探讨键图理论用于汽车平顺性仿真分析的方法,将所建立的汽车四自由度振动键图模型与Matlab的Simulink仿真工具箱仿真方框图相连接,直接利用Simulink的可视化功能,实现汽车平顺性可视化仿真。键图模型和Simulink仿真工具箱的连接可使键图理论在汽车系统仿真分析研究中更为简便、快捷。     

用于儿童头部损伤生物力学研究的碰撞理论模型建立及验证

机动车事故和跌落等碰撞工况是造成儿童头部受伤的重要原因,研究碰撞过程中儿童头部的动力学响应对于头部损伤的预测具有重要意义。头部动力学模型能够快速预测不同碰撞场景下头部动态响应结果并进而预测头部损伤风险。首先,建立考虑颅骨及皮肤厚度和形态曲率的儿童头部碰撞理论模型用于预测儿童头部在碰撞工况下的响应。然后,通过儿童头部CT扫描提取颅骨及皮肤几何结构,对颅骨和皮肤三维重建后进行分割和定量离散,分别得到能描述颅骨内侧、颅骨外侧及皮肤形态的离散点集群,通过计算得到碰撞点周围的平均曲率与厚度,基于建立的头部碰撞理论模型可计算不同碰撞位置(不同厚度和曲率)的碰撞力。最后,通过碰撞试验对建立的碰撞理论模型进行验证,使用不同年龄的小型猪头部作为儿童头部的代替品进行碰撞试验,将试验结果与上述建立的理论模型对小型猪头部碰撞响应的预测结果(基于小型猪头部的真实的形态曲率、皮肤和颅骨厚度数据)进行对比。研究结果表明：建立的理论模型可以较为准确地预测碰撞脉宽和最大碰撞力;提出的儿童头部碰撞动力学理论模型能够快速预测头部不同碰撞位置的动力学响应,可以为儿童头部损伤的进一步研究提供参考和理论支撑。     

直线电机运载系统整体道床力学特性研究

利用ANSYS有限元分析软件,建立直线电机运载系统无碴轨道的空间计算模型,将整体道床的受力变形结果与不考虑磁吸力的结果进行对比分析,得出磁吸力对整体道床的影响规律.理论分析表明,在考虑直线电机的磁吸力后,将增加整体道床的内力和位移值,据此对整体道床的设计提出建议.     

基于ANSYS的舰船基座抗冲击计算方法研究

利用ANSYS软件研究了用于舰船基座抗冲击的计算方法,包括静g法、谱分析法（BV043／85规定谱、DDAM）和时间历程法。从改变系统固有频率出发,对单自由度系统和多自由度系统的位移响应和加速度响应结果进行了比较分析,对几种计算方法的优缺点进行了总结,并得出了相关结论。     

利用相关分析实现低信噪比信号的相位差测量

介绍了低信噪比情况下,利用相关分析法实现相位差测量的原理以及计算机仿真。实验表明,利用相关分析法能够实现高噪声环境下的相位差测量,测量结果能达到一定的精度。     

Recent observations in the straits of the East/Japan Sea: A review of hydrography, currents and volume transports

Recent observations of hydrography, currents and volume transports in the straits of the East/Japan Sea are reviewed. It is newly found that bottom cold water in the Korea/Tsushima Strait originating from the northern region of the East/Japan Sea appears not only in summer and autumn but also in winter. Intensive observations in the Korea/Tsushima Strait revealed two distinct cores of northeastward currents in the upper layer of the western and eastern channels. Mean volume transport through the Korea/Tsushima Strait is calculated as 2.5 ± 0.5 Sv from four-year direct and indirect measurements. As continuous monitoring has started in the Tsugaru and Soya Straits, understanding of temporal variability of currents and volume transports through the straits is in progress. For the first time, simultaneous time series of volume transports are available in the Korea/Tsushima and Tsugaru Straits during the winter of 1999–2000. Ouflow through the Tsugaru Strait accounts for about 70% of inflow through the Korea/Tsushima Strait for this period.     

基于MSP430单片机的多通道数据采集系统

为实现多通道数据准确同步采集,减小温度对数据采集的影响,利用MSP430单片机实现三通道16位A/D独立采样,同时用其内嵌温度传感器测量环境温度,根据所测温度对采样结果进行修正,通过分析了温度传感器产生误差的原因,提出了解决方法并给出了温度传感器相关的C语言程序,减小了温度变化对采样结果产生的影响。     

Circulation features in the Japan/East Sea related to statistically obtained wind patterns in the warm season

A response of the circulation in the Japan/East Sea (JES) to different kinds of wind forcing is studied, with the emphasis on the warm season, using a primitive equation oceanic model. Wind forcing is based on typical patterns obtained from complex empirical orthogonal functions of 1°-gridded NCEP/NCAR 6 h winds for 1998–2005. These patterns are distinguished by a prevailing wind direction. Northwestern wind and strong cyclonic (C) curl prevail in winter, while a variety of patterns occur in the warm season, differing in the wind direction and curl. Three model runs are performed to examine the circulation in response to a prevailing C wind stress curl or an alternating C and anticyclonic (AC) curl or a strong C curl in the warm season. The simulated features are consistent with the observational evidence, in particular with thermal fronts and frequent eddy locations derived from multi-year infrared satellite imagery. The simulated C circulation intensifies and the subarctic region extends southward with the strengthening of a summer C wind stress curl over the JES. Variability of Subarctic Front (SF) in the western JES (between 130°E and 133°E) is strongly affected by summer wind stress curl. Forcing by an AC curl tends to shift SF northward, while SF shifts to the south under the forcing by a C curl, reaching the southern Ulleung Basin in the case of the strong C curl. In the northwestern JES (off Peter the Great Bay, Russia, and North Korea), the SF northwestern branch (NWSF) is simulated. It is a known feature in autumn and early winter and can also occur in the warm season. The simulation results suggest an AC wind stress curl as the forcing of the formation of the NWSF in the warm season. The Siberia Seamount and sharply bending coastline near Peter the Great Bay facilitate partial separation of the Primorye (Liman) Current from the coast. The wind stress curl can be an additional forcing of the Tsushima Warm Current (TWC) branching off the Korea Strait to the East Korea Warm Current (EKWC) and the offshore branch (OB). In the warm season, the simulated TWC bifurcation occurs farther north, the EKWC is strong, and the OB is weak under the forcing of the AC wind stress curl. The EKWC is weak and the OB is strong under the forcing of the strong C wind stress curl.