无人机栖落机动建模与轨迹优化

对固定翼无人飞行器栖落机动的纵向运动进行了气动特性建模与轨迹优化设计。通过运动捕捉系统测量获得试验滑翔机实时飞行数据,并结合统计学原理和平板气动理论建立了气动模型和动力学模型。针对所建立的模型采用GPOPS优化工具箱设计了栖落机动标称轨迹。优化结果表明,不同初始速度条件下执行栖落机动的空间需求不同,但最终都可以实现以相同的栖落速度落到同一位置。     

含间隙运动控制系统中的定位抖动和 速率波动原因分析及解决措施

针对一类含间隙大惯量非直驱转动系统中出现的速率波动现象,利用描述函数法和计算仿真的方法进行了原因分析.在通常的解决措施如双电机消隙、机械消隙方法之外,针对一类间隙可测量的运动控制系统,提出了解决该类问题的新思路,即通过间隙的间接测量,利用反馈机制进行间隙补偿,并用小增益定理证明了其稳定性.实现了部分电气消隙的作用,在适当降低跟踪精度的情况下,消除了定位抖动,提高了速率平稳性.     

一种线运动扰动环境下基于惯性凝固系抗干扰自对准优化算法研究

传统惯性凝固性对准技术可有效隔离角运动干扰环境对捷联惯导自对准精度的影响,但对线运动环境下的抗干扰能力不足.据此,在深入分析线运动干扰对捷联惯导惯性凝固系下自对准精度影响途径之上,对线运动干扰环境划分为速度周期波动、突跳以及速度短期线性漂移.提出采用积分降噪、载体惯性系速度递推拟合与基于带遗忘因子递推最小二乘的速度慢漂提取技术相结合的抗干扰自对准优化算法,并进行了试验验证.试验结果表明,本算法可在5min内实现1.3mil的抗干扰自对准精度.     

高超声速飞行器地面颤振评估技术研究

针对高超声速飞行器飞行过程中颤振边界变动范围大、试验测试难的问题,本文开展了考虑气动热效应的翼面结构地面颤振试验技术研究。首先基于工程法对结构所受的气动加热进行了分析,在此基础上开展了结构的热颤振特性评估并作为地面颤振试验结果的参考标准。考虑实际飞行中结构温升效应影响,建立了基于多工况点的气动力综合优化降阶算法,确保了整个温升过程的气动力模拟的精度。通过建立基于模糊逻辑比例、积分和微分（Proportional integral derivative,PID）控制的多点协调控制系统,实现了温升过程中时变系统的激振力控制器设计。最终搭建了地面颤振试验系统,按照典型飞行状态对结构的热颤振特性进行了测试,试验测试结果与仿真结果对比相对误差约10%。     

地源热泵技术在建筑节能中的应用

本文探讨如何通过地源热泵技术实现建筑节能。研究通过地源热泵来实现一机多用,使其既能用于冬季供暖,又可以用于夏季制冷。同时也讨论了如何与太阳能相配合,来实现地热平衡。文中还给出了通过插值法和曲线拟合法对测量数据进行处理获得变温带和增温带的温度-深度曲线的方法。     

电子对抗有效载荷地面测试与评估技术

描述电子对抗有效载荷地面测试系统的设计内容,介绍了测试系统的主要组成、功能及测试工作原理,常有的测试项目、测试方法,载荷的数据整理、评估与分析等,为以后电子对抗载荷地面系统搭建提供参考借鉴作用。     

关于进行程序管制一体化模拟练习的设想

在程序管制模拟练习中，存在着塔台管制服务、进近管制服务和区域管制服务互不衔接，不能系统地模拟整个管制过程的问题。针对这一情况提出了程序管制一体化模拟练习和程序和管制一体化模拟机的结构设计。     

球形粒子在流体中的跟随性

本文从Maxey和Riley的粒子运动基本方程出发,得到了球形固体粒子在相对流动雷诺数很小情形下的分析解。讨论了粒子跟随性对外力、初始条件和流场性质的依赖关系;对均匀湍流场,分析了不同密度比和扰动频率对跟随性的影响     

Vertical motions in Thailand after the 2004 Sumatra–Andaman Earthquake from GPS observations and its geophysical modelling

Following previous findings from ongoing GPS research in Thailand since 2004 we continue to exploit the GPS technique to monitor and model land motions induced by the Sumatra–Andaman Earthquake. Our latest results show that up to the end of 2010, Thailand has been co-seismically displaced and is subsequently undergoing a post-seismic horizontal deformation with total displacements (co-seismic plus post-seismic) ranging from 10.5 to 74.7 cm. We observed the largest horizontal displacements in the southern part of Thailand and moderate and small displacements in the central and northern parts. In addition to horizontal displacements throughout Thailand, continuous GPS measurements show that large parts of Thailand are subsiding at rates up to 1 cm/yr. It is the first time that such vertical post-seismic deformations at large distances (650–1500 km away from the Earthquake’s epicentre) have been recorded. We have investigated the physical processes leading to the observed subsidence. While after-slip on the subduction interface induces negligible or even slightly positive vertical motions, relaxation in the asthenosphere is associated with a sizable subsidence. Predictions from a 3D finite element model feature an asthenosphere with an effective viscosity of the order of 3 * 10¹⁸ Pas, fit the horizontal post-seismic data and the observed subsidence well. This model is then used to predict the subsidence over the whole seismic cycle. The subsidence should go on with a diminishing rate through the next two decades and its final magnitude should not exceed 10 cm in the Bangkok area.     

Refining DORIS atmospheric drag estimation in preparation of ITRF2008

In preparation of ITRF2008, all geodetic technique services (VLBI, SLR, GPS and DORIS) are generating new solutions based on combination of individual analysis centers solutions. These data reprocessing are based on a selection of models, parameterization and estimation strategy unique to each analysis center and to each technique. While a good agreement can be found for models between groups, thanks to the existence of the IERS conventions, a great diversity still exist for parameter estimation, allowing possible future improvements in this direction. The goal of this study is to focus on the atmospheric drag estimation used to generate the new DORIS/IGN ignwd08 time series prepared for ITRF2008. We develop here a method to inter-compare different processing strategies. In a first step, by analyzing single-satellite solutions for a few weeks of data but for a large number of possible analysis strategies, we demonstrate that estimating drag coefficient more frequently (typically every 1–2 h instead of previously every 4–8 h) for the lowest DORIS satellites (SPOTs and Envisat) provides better geodetic results for station coordinates and polar motion. This new processing strategy also solved earlier problem found when processing DORIS data during intense geomagnetic events, such as geomagnetic storms. Differences between drag estimation strategies can mostly be found during these few specific periods of extreme geomagnetic activity (few days per year). In such a case, when drag coefficient is only estimated every 6 h or less often for single-satellite solution, a significant degradation in station coordinate accuracy can be observed (120 mm vs. 20 mm) and significant biases arose in polar motion estimation (5 mas vs. 0.3 mas). In a second step, we reprocessed a full year of DORIS data (2003) in a standard multi-satellite mode. We were able to provide statistics on a more reliable data set and to strengthen these conclusions. Our proposed DORIS analysis is easy to implement in all software packages and is now already used by several analysis centers of the International DORIS Service (IDS) when submitting reprocessed solutions for ITRF2008.