CBERS-1卫星CCD相机零级图像处理研究

CCD相机是CBERS - 1卫星上的主要有效载荷之一。利用其接收的可见光和近红外谱段的图像 ,可以在国民经济的各个生产部门 ,诸如国土资源调查、农业、林业、地矿、水利、环境、生态等方面得到广泛应用。但是由于探元和光学系统成像的物理机制和各种干扰等因素影响 ,地面接收到的数据必须经过处理才能应用。文章介绍的内容就是将这种图像数据经图像预处理 ,得到零级图像 ;经过相应的辐射校正 ,得到一级图像 ;经过几何校正 ,得到二级图像产品 ,提供给其它部门加以应用     

CBERS-1卫星CCD相机光学系统设计

CBERS -1卫星CCD相机的光学系统采用了折射式光学系统。文章介绍了该系统的设计特点     

基于DS18B20的智能温度控制器

基于DS18B20的智能温度控制器采用单总线数字温度传感器,硬件结构简单,测量精度高,抗干扰能力强,重点介绍DS18B20的特性和编程要点。     

FY-1C/D极轨气象卫星及其在轨运行

简要说明了风云一号(FY-1)极轨气象卫星的总体情况。介绍了FY-1C星运行5年。D星运行2年后的测控、电源、热控、敖传、扫描辐射计和星载数据收集与分发(DCDS)分系统、有效载荷空间粒子成分监测器。以及姿控和星载计算机的在轨运行情况。在轨测试结果表明，两星的在轨运行、功能和性能符合任务书的要求。最后总结了长寿命高可靠稳定优质业务运行的FY-1C，D星的创新点、主要成绩，并给出了部分应用情况。     

GPS定位数据在海洋一号卫星中的应用与比较

简要介绍了海洋一号卫星星载GPS接收机的定位原理、流程和应用，探讨了一种在轨定位结果的确认和互验方法．借助于卫星工具包软件(STK)，利用NASA网站公布的HY-1卫星两行根数(TLE)进行卫星轨道推算，生成星下点位置，并与相应时刻星载GPS接收机实测数据得到的星下点位置进行比较，由此得到两种方法定位结果之间的偏差，用实际在轨数据验证了两者的位置符合程度．     

铝/ZN-1阻尼材料复合结构件的粘接技术研究

探讨了胶黏剂黏度、硬铝表面处理方式及硅烷偶联剂KH-560的使用方式等因素对硬铝板/ZN-1阻尼材料复合结构件的粘接性能的影响。研究表明：如果硬铝板表面采用砂纸打磨处理时，采用黏度较低的TC-1环氧树脂胶或者在黏度较高的J-22环氧树脂胶中添加2％的硅烷偶联剂KH-560可以获得优异的粘接效果；当硬铝板表面采用铬酸阳极化处理时，两种胶黏剂均能获得优异的粘接效果。     

测量机连续扫描控制系统设计

利用UCC1控制器作为核心,构建具有三维空间连续扫描功能的测量机控制系统的方法,并简要介绍了UCC1控制器的功能及控制系统硬件电路的设计。     

应用ART1神经网络仿真车间分组

阐述了ART1神经网络在制造单元设计过程中形成零件族的基本方法,并在基于MATLAB的软件平台上,利用其神经网络工具箱对生产过程中的实际情况进行了仿真和应用。     

Expectations for Infrared Spectroscopy of 9P/Tempel 1 from Deep Impact

The science payload on the Deep Impact mission includes a 1.05–4.8 μm infrared spectrometer with a spectral resolution ranging from R∼200–900. The Deep Impact IR spectrometer was designed to optimize, within engineering and cost constraints, observations of the dust, gas, and nucleus of 9P/Tempel 1. The wavelength range includes absorption and emission features from ices, silicates, organics, and many gases that are known to be, or anticipated to be, present on comets. The expected data will provide measurements at previously unseen spatial resolution before, during, and after our cratering experiment at the comet 9P/Tempel 1. This article explores the unique aspects of the Deep Impact IR spectrometer experiment, presents a range of expectations for spectral data of 9P/Tempel 1, and summarizes the specific science objectives at each phase of the mission.     

Deep Impact: Working Properties for the Target Nucleus – Comet 9P/Tempel 1

In 1998, Comet 9P/Tempel 1 was chosen as the target of the Deep Impact mission (A’Hearn, M. F., Belton, M. J. S., and Delamere, A., Space Sci. Rev., 2005) even though very little was known about its physical properties. Efforts were immediately begun to improve this situation by the Deep Impact Science Team leading to the founding of a worldwide observing campaign (Meech et al., Space Sci. Rev., 2005a). This campaign has already produced a great deal of information on the global properties of the comet’s nucleus (summarized in Table I) that is vital to the planning and the assessment of the chances of success at the impact and encounter. Since the mission was begun the successful encounters of the Deep Space 1 spacecraft at Comet 19P/Borrelly and the Stardust spacecraft at Comet 81P/Wild 2 have occurred yielding new information on the state of the nuclei of these two comets. This information, together with earlier results on the nucleus of comet 1P/Halley from the European Space Agency’s Giotto, the Soviet Vega mission, and various ground-based observational and theoretical studies, is used as a basis for conjectures on the morphological, geological, mechanical, and compositional properties of the surface and subsurface that Deep Impact may find at 9P/Tempel 1. We adopt the following working values (circa December 2004) for the nucleus parameters of prime importance to Deep Impact as follows: mean effective radius = 3.25± 0.2 km, shape – irregular triaxial ellipsoid with a/b = 3.2± 0.4 and overall dimensions of ∼14.4 × 4.4 × 4.4 km, principal axis rotation with period = 41.85± 0.1 hr, pole directions (RA, Dec, J2000) = 46± 10, 73± 10 deg (Pole 1) or 287± 14, 16.5± 10 deg (Pole 2) (the two poles are photometrically, but not geometrically, equivalent), Kron-Cousins (V-R) color = 0.56± 0.02, V-band geometric albedo = 0.04± 0.01, R-band geometric albedo = 0.05± 0.01, R-band H(1,1,0) = 14.441± 0.067, and mass ∼7×10¹³ kg assuming a bulk density of 500 kg m⁻³. As these are working values, {i.e.}, based on preliminary analyses, it is expected that adjustments to their values may be made before encounter as improved estimates become available through further analysis of the large database being made available by the Deep Impact observing campaign. Given the parameters listed above the impact will occur in an environment where the local gravity is estimated at 0.027–0.04 cm s⁻² and the escape velocity between 1.4 and 2 m s⁻¹. For both of the rotation poles found here, the Deep Impact spacecraft on approach to encounter will find the rotation axis close to the plane of the sky (aspect angles 82.2 and 69.7 deg. for pole 1 and 2, respectively). However, until the rotation period estimate is substantially improved, it will remain uncertain whether the impactor will collide with the broadside or the ends of the nucleus.