基于G2的卫星控制系统故障诊断的半物理仿真

研究一种基于G2的集故障注入、故障模拟和故障诊断为一体的半物理仿真系统,包括基于VxW orks的实时硬件模拟系统、星载姿轨控计算机、数管及遥控遥测模拟器和专用接口箱等.开发了基于G2的以某一类典型卫星控制系统为对象的故障诊断专家系统,并对G2外部接口进行了扩展设计.最后,以典型故障为例,在半物理仿真平台上进行了演示验证.     

哨兵2卫星综合水质指标的河流水质遥感监测方法

上海市河流水污染监测是当前研究的热点问题。针对上海市河流水质监测的需求,提出了一种基于因子分析的河流综合水质遥感反演的方法。以欧洲航空局发射的哨兵-2A(Sentinel-2A)卫星搭载的多光谱成像仪获取的遥感影像,以及准同步获取的河流断面实测水质参数数据为例,研究对象为上海市青浦区和松江区部分河道。选取高锰酸盐指数、氨氮等5项主要水质参数为监测指标,在因子分析的基础上建立水质遥感反演的模型,得到综合水质指标用于确定水质类别。实验结果表明:综合水质指标值越小,内陆河流水质状况越良好,水体更清洁。该方法能够应用于内陆河流水质遥感监测,为水环境管理部门提供参考信息。     

一种基于频移补偿的apFFT相位估计改进方法及应用

全相位快速傅里叶变换（all phase Fast Fourier Transform,apFFT)相位一致性特点使正弦信号相位估计不受频率估计影响,但由于频谱泄露和栅栏效应,apFFT相位估计性能受信号频率位置影响。针对该问题,提出了一种基于高精度频率估计和补偿的apFFT相位估计方法。首先,对信号进行高精度频率估计,并以此对信号进行频移补偿,然后对补偿信号进行apFFT,最后求解信号相位。蒙特卡洛仿真结果表明：所提算法的相位估计性能不受信号频率位置影响,相位估计误差性能与理论值一致,受两参数克拉美罗界（CRLB₂）约束,约为1.158 2倍的CRLB₂;相位估计性能和抗噪声能力明显优于经典apFFT算法和其他对比算法。更进一步,利用我国首次火星探测器TW-1（天问一号）近火捕获段干涉测量数据进行算法验证,结果表明：相位估计精度约4 mrad,干涉测量时延估计精度约50 ps。     

多级嵌套L型阵列及其测向算法

针对基于偶数(2q)阶累积量的测向算法中测向性能提高有限的问题,提出了一种基于多级嵌套 L 型阵列的2维测向算法。首先利用阵列的多级嵌套结构和2q阶累积量,形成具有更多自由度的虚拟均匀面阵;然后使用2维平滑方法,恢复其2q阶累积量矩阵的秩; 采用2维MUSIC算法,进行方位角和俯仰角的估计。与常规的2q MUSIC 算法相比,所提算法不仅具有更好的测向精度,而且由于虚拟均匀阵包含更多的虚拟阵元,因此能够估计更多信源的方位角。另外,针对该L型阵列的最优配置问题,推导了各级子阵阵元数的最优和次优分配表达式。仿真结果表明这些结论的正确性。     

不同碳黑填料含量2D—SiCf／SiC复合材料介电及雷达吸波性能研究

对先驱体浸渍裂解工艺(PIP)制备的含碳黑填料2D-SiCf/SiC复合材料介电以及雷达吸波性能进行研究.研究表明,由于KD-Ⅰ型SiC纤维表面具有连续碳涂层,不能直接用于吸波材料,需通过空气热处理手段将其除去.对纤维表面去碳后制成的不同碳黑填料含量2D-SiCf/SiC复合材料微波介电常数进行测试,结果表明,随碳黑含量增加,复合材料介电常数明显增大,但由于碳黑的高比表面和先驱体溶液粘度的限制,复合材料中碳黑体积分数最大仅能达到7%～8%,介电常数难以继续增大,介电损耗低于0.3,并且介电常数频散效应不理想.对不同碳黑填料含量复合材料反射率进行计算,结果表明,单层复合材料在某一频段内具有较好的吸波性能,但由于复合材料介电常数频散效应较差,宽频吸波性能不理想,采用不同吸收剂含量复合材料层铺工艺可能可以解决吸波性能带宽问题.     

红外反射材料In(Sn)2O3(ITO)的微波吸收性能

测试7.7vol%和15.8vol%In(Sn)2O3(ITO)/石蜡在2~18GHz的介电谱。测定10vol%和20vol%In(Sn)2O3(ITO)/环氧树脂在2~8GHz的反射率。结果显示,ITO材料具有很好的介电损耗。当涂层厚度d=3mm时,两种涂层分别在4.51GHz和6.27GHz有-10.5dB和-14dB的反射率。理论值显示,15.8vol%ITO/石蜡复合材料在4.56~11GHz的反射率低于-10dB,有好的吸波性能。同时分析ITO的介电损耗机理。     

Modeling of ionospheric parameter variations in East Asia during the moderate geomagnetic disturbances

The results of modeling of ionospheric disturbances observed in the East Asian region during moderate storms are presented. The numerical model for ionosphere–plasmasphere coupling developed at the ISTP SB RAS is used to interpret the data of observations at ionospheric stations located in the longitudinal sector of 90–130°E at latitudes from auroral zone to equator. There is obtained a reasonable agreement between measurements and modeling results for winter and equinox. In the summer ionosphere, at the background of high ionization by the solar EUV radiation in the quiet geomagnetic period the meridional thermospheric wind strongly impacts the electron concentration in the middle and auroral ionosphere. The consistent calculations of the thermospheric wind permit to obtain the model results which are closer to summer observations. The actual information about the space-time variations of thermosphere and magnetosphere parameters should be taken into account during storms.     

SCIAMACHY limb measurements of NO2, BrO and OClO. Retrieval of vertical profiles: Algorithm,first results,sensitivity and comparison studies

The Scanning Imaging Absorption Spectrometer for Atmospheric Chartography (SCIAMACHY) measures scattered sun light also in limb viewing mode (i.e. tangential to Earth’s surface and its atmosphere), which allows determining vertical profiles of atmospheric trace gases. First results on the retrieval of NO₂, BrO and OClO profiles from the SCIAMACHY Limb measurements are presented and compared to independent satellite and balloon borne observations.     

Implication of multiple dipolarization event near 9 RE for the physics of substorms

In 2001, 2002 and 2003, the Polar spacecraft probed the near equatorial plasma sheet at 9 R_E near local midnight. Using the magnetic field observations, the signatures at substorm onsets are studied. Close to the flux pile-up region, the Polar spacecraft readily detects the dipolarization front, especially for pseudo onsets. An event with two distinct onsets has been examined. The signatures are found to be consistent with the multiple-onset model suggested by Russell [Russell, C.T. How northward turnings of the IMF can lead to substorm expansion onsets. Geophys. Res. Lett. 27, 3257–3259, 2000] which is a modified Near-Earth Neutral Line (NENL) model. Another similar event is also examined showing the effects of different Interplanetary Magnetic Field (IMF) conditions upon substorms. Moreover, ground effects can be very weak compared to in situ observations, especially for pseudo onsets, because these signatures appear to be localized and not global.     

Responses of ionospheric foF2 to geomagnetic activities in Hainan

Responses of low-latitude ionospheric critical frequency of F2 layer to geomagnetic activities in different seasons and under different levels of solar activity are investigated by analyzing the ionospheric foF2 data from DPS-4 Digisonde in Hainan Observatory during 2002–2005. The results are as follows: (1) the response of foF2 to geomagnetic activity in Hainan shows obvious diurnal variation except for the summer in low solar activity period. Generally, geomagnetic activity will cause foF2 to increase at daytime and decrease at nighttime. The intensity of response of foF2 is stronger at nighttime than that at daytime; (2) seasonal dependence of the response of foF2 to geomagnetic activity is very obvious. The negative ionospheric storm effect is the strongest in summer and the positive ionospheric storm effect is the strongest in winter; (3) the solar cycle has important effect on the response of foF2 to geomagnetic activity in Hainan. In high solar activity period, the diurnal variation of the response of foF2 is very pronounced in each season, and the strong ionospheric response can last several days. In low solar activity period, ionospheric response has very pronounced diurnal variation in winter only; (4) the local time of geomagnetic activities occurring also has important effect on the responses of foF2 in Hainan. Generally, geomagnetic activities occurred at nighttime can cause stronger and longer responses of foF2 in Hainan.