波形记录仪触发延迟线性的实验研究

提出了使用正弦波激励评价触发延迟线性度和触发抖动的新方法，通过一个波形在有触发延迟和无触发延迟时，采集序列间的相位差对应的时间差来最终判定触发延迟结果。用该方法实现的触发延迟线性度测量方法，将触发延迟直接溯源到激励信号的频率量上，无需额外的精密延时器等装置，减少了测量环节，并且可以实现任意延迟的精确测量。以不同频率、不同触发延迟、不同采集速率下的实验结果的对比给出了触发延迟线性校准的结论性意见，同时验证了所述方法的有效性和切实可行性。     

大滞后温度智能控制系统的研究与实现

本文研究的是以MCS-51系列单片机为核心的计算机控制系统,用以实现化工催化剂活性检测过程床层温度程序控制。被控对象是具有3～8分钟的纯滞后,时变,非线性特性的催化剂电加热炉。控制难度大。 采用了广义最小方差自校正控制算法,具有时变滞后的极点自校正PID算法,极点对消直接PID三种算法进行了仿真与现场试验研究。前两种,由于工作过程允许的信号对系统激励不够充分,对象在线辩识有困难,试验结果表现,不能实现预期的控制要求。最终采用了极点对消直接PID算法,成功地实现了催化剂活性温度自动控制。该系统工作稳定、可靠,控制精度达到了检测标准要求。     

延误航班停机坪作业运行控制研究

随着航班航次的增加，机场变得越来越繁忙．地面作业操作不当所导致的飞机地面事故日益增加：在介绍航班停机坪作业的基础上，分析了地面作业的特点，在此基础上，根据航班延误时在作业资源充足和不足情况下，研究了航班停机坪作业的一般方法。在资源充足情况下，航班延误的地面作业控制主要采用AOE方法，缩短关键路线的作业时间。而资源不足情况下，除了控制关键路线作业时间外，还要根据排序算法合理分配关键作业的资源，以实现缩短延误时间的目的。     

含纳米金属粉的推进剂点火实验及燃烧性能研究

利用CO2激光点火系统对含有纳米铝粉和纳米镍粉的AP／HTPB推进剂进行激光点火实验,测量了推进剂在不同激光功率和压强下的点火延迟时间,对推进剂的燃速、常压点火温度和爆热也进行了测量。同时,利用氧化还原滴定法测定燃烧残渣中活性铝含量。结果表明,纳米铝粉(n—Al)的点火阀值比普通铝粉(g-A1)的点火阀值小几个数量级,加入纳米铝粉可有效地缩短推进剂点火延迟时间。而在纳米镍粉为催化剂的协同作用下,推进剂燃速明显提高,点火延迟时间也大大减少,Al在推进剂燃烧过程中的燃烧效率得以提高,同时燃烧残渣中活性铝含量也明显降低。     

45°(N)纬度带的Klobuchar like电离层延迟季节修正模型与评估

电离层延迟是全球卫星导航系统（GNSS）的主要误差源之一。对于装配GNSS单频接收机的航空器,选择简单有效的Klobuchar广播电离层模型来改正电离层延迟误差,其修正率为50%～60%。针对45°（N）纬度带,提出了更高电离层修正需求。考虑到季节因素对中高纬度地区电离层的显著影响,利用GIMs（Global Ionospheric Maps）分析了昼夜中TEC（Total Electron Content）的峰值和谷值随季节（年积日）的变化,建立了一种适用于45°（N）纬度带的Klobuchar like电离层模型。该模型不增加广播模型系数,新模型的夜间和VTEC高峰时电离层修正率分别达到了82%和80%,表明在穿刺点集中的45°(N)纬度地区使用该模型可以更精确地描述该地区的电离层,帮助航空器实现更高精度的定位。     

Establishment of atmospheric weighted mean temperature model in the polar regions

Due to the special geographical location and extreme climate environment, the polar regions (Antarctic and Arctic) have an important impact on global climate change. Atmospheric weighted mean temperature (Tm) is a crucial parameter in the retrieval of precipitable water vapor (PWV) from the zenith wet delay (ZWD) of ground-based Global Navigation Satellite System (GNSS) signal propagation. In this paper, the correlation between weighted mean temperature and surface temperature (Ts) is studied firstly. It is shown that the correlation coefficients between Tm and Ts are 0.93 in the Antarctic and 0.94 in the Arctic. The linear regression Tm model and quadratic function Tm model of the Antarctic and the Arctic are established respectively using the radiosonde profiles of 12 stations in the Antarctic and 58 stations in the Arctic from 2008 to 2015. The accuracies of the linear regression Tm model, the quadratic function Tm model and GPT2w Tm model which is a state-of-the-art global Tm model are verified using the radiosonde profiles from 2016 to 2018 in the Antarctic and Arctic. Root Mean Square (RMS) errors of the linear regression Tm model, the quadratic function Tm model and GPT2w Tm model in the Antarctic are 3.07 K, 2.87 K and 4.32 K respectively, and those in the Arctic are 3.53 K, 3.38 K and 4.82 K, which indicates that the quadratic function Tm model has a higher accuracy compared to linear regression Tm model, and the accuracies of the two regional Tm models are better than that of GPT2w Tm model in the polar regions. In order to better evaluate the accuracy of Tm in the PWV retrieval, the PWV values of radiosondes are used for comparisons as the reference value. The RMS errors of PWV derived from the two Tm models are similar for 1.28 mm in the Antarctic and 1 mm in the Arctic respectively. In addition, the spatial and temporal variation characteristics of Tm are analyzed in the polar regions by spectral analysis of Tm data using fast Fourier transform. The results show that the Tm has obvious seasonality and annual periodicity in the polar regions, and the maximum difference between warm season and cold season is about 63 K. After comparing and analyzing the influences of latitude, longitude and elevation on the Tm in the polar regions, it is found that latitude and elevation have a greater influence on the Tm than the longitude. As the latitude and elevation increase, the Tm decreases, and vice versa in the polar regions.     

Maximal admissible mode decision delay in terminal guidance

Mode decision-maker is a critical component in the logic-based Integrated Estimation and Guidance(IEG) system. For the best possible estimation and guidance performance, the mode decision delay of the mode decision-maker should be limited to a range as small as possible. This paper presents a numerical method for computing the maximal admissible mode decision delay that varies with time-to-go. Particular attention has been paid to highly maneuvering target interception in terminal guidance. The results of this research offer useful guidelines for the design of the mode decision-maker in IEG systems.     

基于飞行资源分离的航班延误传播研究

在航班串设计及机组排班过程中,经常涉及飞行资源(飞机、机组)分离的问题。而延误航班的飞行资源分离将导致共享资源的衔接航班发生延误,并传播至后续航班串。本文考虑带有飞行资源分离的航班串,利用基于贝叶斯网络的比例风险回归模型,对资源分离后的航班离港延误进行分析。对比两种不同时刻飞机与机组资源分离方案下,各延误因素对衔接航班离港延误,以及整个后续航班串延误时间的影响,结果表明,不同时刻分离方案会造成不同的延误传播效果。本文为飞机、机组资源分离时刻的选择提供了定量分析方法,结果表明,资源分离时刻的不同对衔接航班的离港延误,以及整个后续航班串延误波及时间的影响都不同。     

Statistical study of the time delay of ionospheric TEC storms to geomagnetic storms in Taoyuan,Taiwan

We have studied the time delay of ionospheric storms to geomagnetic storms at a low latitude station Taoyuan (25.02°N, 121.21°E), Taiwan using the Dst and TEC data during 126 geomagnetic storms from the year 2002 to 2014. In addition to the known local time dependence of the time delay, the statistics show that the time delay has significant seasonal characteristics, which can be explained within the framework of the seasonal characteristics of the ionospheric TEC. The data also show that there is no correlation between the time delay and the intensity of magnetic storms. As for the solar activity dependence of the time delay, the results show that there is no relationship between the time delay of positive storms and the solar activity, whereas the time delay of negative storms has weakly negative dependence on the solar activity, with correlation coefficient −0.41. Especially, there are two kinds of extreme events: pre-storm response events and long-time delay events. All of the pre-storm response events occurred during 15–20 LT, manifesting the Equator Ionospheric Anomaly (EIA) feature at Taoyuan. Moreover, the common features of the pre-storm response events suggest the storm sudden commencement (SSC) and weak geomagnetic disturbance before the main phase onset (MPO) of magnetic storms are two main possible causes of the pre-storm response events. By analyzing the geomagnetic indices during the events with long-time delay, we infer that this kind of events may not be caused by magnetic storms, and they might belong to ionospheric Q-disturbances.     

考虑测试性设计缺陷修正延时的测试性增长模型建模与评价方法

针对现有测试性增长模型忽略了测试性设计缺陷的修正延时过程，进而导致测试性增长模型（TGM）跟踪与预计精度低的问题，提出了一种考虑测试性设计缺陷修正延时的测试性增长模型建模理论与方法。首先分析测试性设计缺陷识别与修正之间的延时机理，得到剩余测试性设计缺陷（TDL）具有先增后减的铃形变化趋势；在此基础上，分别以Gamma、Raleigh和Delay-S 3种曲线拟合剩余测试性设计缺陷（RTDL）变化趋势，研究建立基于以上3种曲线考虑修正延时的测试性增长模型；最后，以某机载稳定跟踪平台测试性增长试验数据验证测试性增长模型拟合、跟踪及预计效能。研究结果表明：基于该测试性增长试验数据，Gamma曲线可以精确地拟合剩余测试性设计缺陷变化规律，测试性增长模型跟踪和预计精度可达到10^-2数量级。