民用航空发动机振动配平功能设计

振动故障是航空发动机常见并且危害较大的故障,可能导致发动机运营事故或提前更换,增加航空公司运营成本,进行转子平衡是降低发动机振动的重要措施。根据民用涡扇发动机的设计特点和振动配平相关原理,设计了利用EVMU进行发动机振动配平计算的功能,并通过试验进行了验证。试验结果表明:采用根据EVMU计算出的方案配平发动机,能够有效地降低发动机N1振动值,满足航线使用需求。     

通过超实时仿真验证轨控策略方法研究

"嫦娥一号"卫星任务中轨道复杂、轨控次数多,为保证每一次轨控的成功,需要考虑各种约束条件制定最优轨控策略,并能得以验证。本文提出通过超实时仿真验证轨控策略的方法,并以某次轨控为例,详细介绍了该方法的实施步骤。通过超实时仿真验证轨控策略可以评估轨控策略的准确性,并实现在任务执行过程中对轨控相关指令的检验。     

嫦娥一号月球探测卫星技术特点分析

嫦娥一号卫星是我国的第一个月球探测卫星,将飞行至距地球380000km的月球,实现环绕月球对其遥感探测。由于任务目标不同,嫦娥一号卫星将遇到比近地轨道卫星更复杂的空间环境和飞行控制过程,所以必须解决面临的所有新技术问题。文章介绍了嫦娥一号卫星在轨道设计、月食、热设计、制导导航、测控、数传等方面的技术特点及研制验证方法。     

Chang'E-1 Lunar Mission:An Overview and Primary Science Results

Chang'E-1 is the first lunar mission in China, which was successfully launched on Oct. 24th, 2007. It was guided to crash on the Moon on March 1, 2009, at 52.36ºE, 1.50ºS, in the north of Mare Fecunditatis. The total mission lasted 495 days, exceeding the designed life-span about four months. 1.37 Terabytes raw data was received from Chang'E-1. It was then processed into 4 Terabytes science data at different levels. A series of science results have been achieved by analyzing and applicating these data, especially "global image of the Moon of China's first lunar exploration mission'. Four scientific goals of Chang'E-1 have been achieved. It provides abundant materials for the research of lunar sciences and cosmochemistry. Meanwhile these results will serve for China's future lunar missions.     

一种电离层垂直剖面物理模型及其与IRI-90模型的比较

在80-500km范围内考虑了3种中性成份的4种离子,从严格的电子和离子密度连续方程出发,对中性风和扩散效应进行了全面、连续的考虑,由此建立了一种电离层的物理模式;在此模式的基础上针对北京地区分别对太阳活动低年(F_10.7=60)、高年(F_10.7=300)的春(DOY=90)、夏(DOY=180)、秋(DOY=270)、冬(DOY=365)进行计算,并将所得结果与IRI-90进行了比较.结果表明: E层为典型的Chapman层: E-F谷区深度一般为0.2-0.5之间,比IRI要深;F₁缘在太阳活动低年的四季都出现,其中夏天最明显,已形成了一个F₁层,冬天最不明显,仅表现为一个轻微的凸缘,在太阳活动高年只有夏天出现了F₁凸缘,这与现有理论相符合,而IRI-90较少出现明显的F₁缘;F₂层的电子密度是活动高年比低年大,平均冬天比夏天大,这与观测结果也基本符合.     

嫦娥一号CCD立体相机数据光度校正

为更加精确拟合相函数系数, 得到较为准确的光度校正结果, 针对嫦娥一号CCD立体相机数据的特点, 对改进的Lommel-Seeliger模型中的Lommel-Seeliger因子进行修订, 使去除太阳入射角和传感器观测角影响的遥感图像数据能够更好地契合相位角的变化; 利用加入修订后Lommel-Seeliger因子的模型对嫦娥一号CCD立体相机数据进行逐像素光度校正; 选取同一轨道不同纬度和同一区域不同视角两组数据来验证算法的有效性和适用性. 实验结果表明, 该方法能够有效校正由于几何观测条件变化而引起的目标光谱特性的不一致性, 对于较亮和较暗区域的光度校正效果更为有效.     

嫦娥一号干涉成像光谱仪2C级图像数据质量评价

嫦娥一号干涉成像光谱仪(IIM)获取的多波段图像数据对于月表矿物成分反演具有重要意义. 从目视质量、客观参数、几何配准精度、图像质量随时间的变化情况等方面对IIM 2C级的多波段图像数据质量进行了评价. 结果显示, 其两端波段范围的图像质量较差, 不能有效识别月表单元, 中间波段图像质量较好; 自然色图像显示IIM数据存在明显的横向色调不均一性. 利用图像的客观评价指标(辐射精度、清晰度、信息量)将干涉成像光谱仪图像数据与美国Clementine UV-VIS多光谱图像数据进行对比分析, 结果表明, IIM数据清晰度好于Clementine UV-VIS, 而在方差和信息量上弱于Clementine UV-VIS. 将IIM图像数据与Clementine多光谱数据统一到相同的空间分辨率, 进行配准精度评价, 其最大控制点配准误差为0.63pixel. 此外, 还对时间跨度两个月覆盖月表同一区域的IIM图像数据从辐射精度、信息量和清晰度方面进行了评价.     

基于Sigma-Delta调制技术的高精度数字磁通门磁强计仿真

设计了一种基于1 bit Sigma-Delta环路调制技术的高精度数字磁通门磁强计,建立了数字磁强计信号处理仿真模型,并利用Matlab的Simulink仿真工具开展了数字磁通门磁强计模型的仿真分析,对数字磁强计系统的噪声、线性度、响应速度和频率响应进行了仿真计算。利用本文1 bit Sigma-Delta环路调制技术的数字磁强计在量程超过±10⁵ nT的情况下,系统在1 Hz处的噪声仅为4.66 pT·Hz^–1/2,最大线性偏差为0.16 nT,动态响应速度达到2×10⁶ nT·s^–1,频率响应带宽超过10 Hz。仿真结果表明,基于1 bit Sigma-Delta环路调制技术的数字磁通门磁强计可以有效降低对A/D转换器精度的要求,在保证性能的前提下大幅度降低了电路复杂程度,提高了系统的可靠性,在深空探测、空间磁场测量等领域具有广泛的应用前景。     

Science objectives of the magnetic field experiment onboard Aditya-L1 spacecraft

The Aditya-L1 is first Indian solar mission scheduled to be placed in a halo orbit around the first Lagrangian point (L1) of Sun-Earth system in the year 2018–19. The approved scientific payloads onboard Aditya-L1 spacecraft includes a Fluxgate Digital Magnetometer (FGM) to measure the local magnetic field which is necessary to supplement the outcome of other scientific experiments onboard. The in-situ vector magnetic field data at L1 is essential for better understanding of the data provided by the particle and plasma analysis experiments, onboard Aditya-L1 mission. Also, the dynamics of Coronal Mass Ejections (CMEs) can be better understood with the help of in-situ magnetic field data at the L1 point region. This data will also serve as crucial input for the short lead-time space weather forecasting models.The proposed FGM is a dual range magnetic sensor on a 6?m long boom mounted on the Sun viewing panel deck and configured to deploy along the negative roll direction of the spacecraft. Two sets of sensors (tri-axial each) are proposed to be mounted, one at the tip of boom (6?m from the spacecraft) and other, midway (3?m from the spacecraft). The main science objective of this experiment is to measure the magnitude and nature of the interplanetary magnetic field (IMF) locally and to study the disturbed magnetic conditions and extreme solar events by detecting the CME from Sun as a transient event. The proposed secondary science objectives are to study the impact of interplanetary structures and shock solar wind interaction on geo-space environment and to detect low frequency plasma waves emanating from the solar corona at L1 point. This will provide a better understanding on how the Sun affects interplanetary space.In this paper, we shall give the main scientific objectives of the magnetic field experiment and brief technical details of the FGM onboard Aditya-1 spacecraft.     

Evaluation of the improvement of IRI-2016 over IRI-2012 at the India low-latitude region during the ascending phase of cycle 24

This paper investigated the performance of the latest International Reference Ionosphere model (IRI-2016) over that of IRI-2012 in predicting total electron content (TEC) at three different stations in the Indian region. The data used were Global Positioning System (GPS) data collected during the ascending phase of solar cycle 24 over three low-latitude stations in India namely; Bangalore (13.02°N Geographic latitude, 77.57°E Geographic longitude), Hyderabad (17.25°N Geographic latitude, 78.30°E Geographic longitude) and Surat (21.16°N Geographic latitude, 72.78°E Geographic longitude). Monthly, the seasonal and annual variability of GPS-TEC have been compared with those derived from International Reference Ionosphere IRI-2016 and IRI-2012 with two different options of topside electron density: NeQuick and IRI01-corr. It is observed that both versions of IRI (i.e., IRI-2012 and IRI-2016) predict the GPS-TEC with some deviations, the latest version of IRI (IRI-2016) predicted the TEC similar to those predicted by IRI-2012 for all the seasons at all stations except for morning hours (0500 LT to 1000?LT). This shows that the effect of the updated version is seen only during morning hours and also that there is no change in TEC values by IRI-2016 from those predicted by IRI-2012 for the rest of the time of the day in the Indian low latitude region. The semiannual variations in the daytime maximum values of TEC are clearly observed from both GPS and model-derived TEC values with two peaks around March-April and September-October months of each year. Further, the Correlation of TEC derived by IRI-2016 and IRI-2012 with EUV and F10.7 shows similar results. This shows that the solar input to the IRI-2016 is similar to IRI 2012. There is no significant difference observed in TEC, bottom-side thickness (B0) and shape (B1) parameter predictions by both the versions of the IRI model. However, a clear improvement is visible in hmF2 and NmF2 predictions by IRI-2016 to that by IRI-2012. The SHU-2015 option of the IRI-2016 gives a better prediction of NmF2 for all the months at low latitude station Ahmedabad compare to AMTB 2013.