利用地月间空间站的载人登月飞行模式分析

为提高空间站利用率，降低载人登月任务成本，有效开发地月空间，研究了基于地月空间不同轨道空间站的载人登月飞行模式。首先对比直接往返登月飞行模式，对基于空间站的载人登月飞行模式进行任务分析，通过空间站将载人登月任务解耦为载人天地往返任务和登月任务两部分；其次通过轨道设计和稳定性分析提出考虑登月任务需求的地月间空间站可运行轨道和停泊点；最后建立一套飞行模式评价模型，从速度增量需求、飞行时间、空间环境、登月任务窗口、测控条件、交会对接技术难度、后续任务支持性和任务可靠性方面对6种不同位置空间站的登月飞行模式进行分析和定量评价。评价结果表明基于L2点Halo轨道空间站的载人登月飞行模式为更优飞行模式。     

对地定向三轴稳定卫星的圆锥扫描地球敏感器的数学模型

本文介绍了对地定向三轴稳定卫星的圆锥扫描式地球敏感器的姿态测量原理、输出几何关系和数学模型，并以实际例子说明大角度姿态控制时必须注意敏感器输出的轴间耦合问题     

Astrophysics in 2006

The fastest pulsar and the slowest nova; the oldest galaxies and the youngest stars; the weirdest life forms and the commonest dwarfs; the highest energy particles and the lowest energy photons. These were some of the extremes of Astrophysics 2006. We attempt also to bring you updates on things of which there is currently only one (habitable planets, the Sun, and the Universe) and others of which there are always many, like meteors and molecules, black holes and binaries.     

Emergence of a Habitable Planet

We address the first several hundred million years of Earth’s history. The Moon-forming impact left Earth enveloped in a hot silicate atmosphere that cooled and condensed over ∼1,000 yrs. As it cooled the Earth degassed its volatiles into the atmosphere. It took another ∼2 Myrs for the magma ocean to freeze at the surface. The cooling rate was determined by atmospheric thermal blanketing. Tidal heating by the new Moon was a major energy source to the magma ocean. After the mantle solidified geothermal heat became climatologically insignificant, which allowed the steam atmosphere to condense, and left behind a ∼100 bar, ∼500 K CO₂ atmosphere. Thereafter cooling was governed by how quickly CO₂ was removed from the atmosphere. If subduction were efficient this could have taken as little as 10 million years. In this case the faint young Sun suggests that a lifeless Earth should have been cold and its oceans white with ice. But if carbonate subduction were inefficient the CO₂ would have mostly stayed in the atmosphere, which would have kept the surface near ∼500 K for many tens of millions of years. Hydrous minerals are harder to subduct than carbonates and there is a good chance that the Hadean mantle was dry. Hadean heat flow was locally high enough to ensure that any ice cover would have been thin (<5 m) in places. Moreover hundreds or thousands of asteroid impacts would have been big enough to melt the ice triggering brief impact summers. We suggest that plate tectonics as it works now was inadequate to handle typical Hadean heat flows of 0.2–0.5 W/m². In its place we hypothesize a convecting mantle capped by a ∼100 km deep basaltic mush that was relatively permeable to heat flow. Recycling and distillation of hydrous basalts produced granitic rocks very early, which is consistent with preserved >4 Ga detrital zircons. If carbonates in oceanic crust subducted as quickly as they formed, Earth could have been habitable as early as 10–20 Myrs after the Moon-forming impact.     

从典型微机遥测站看遥测技术的发展

分析国外典型微机遥测站的技术特点后 ,认为微机遥测站的核心是利用微软公司的商品化软件 ,应全面考虑发展遥测系统软件。我国发展微机遥测技术时 ,应把注意力放在软件上。     

城市供水调度系统的现状与发展

简述国内城市供水调度系统的应用现状，指出在实际应用中存在的问题和解决的途径。并介绍了系统几年来的发展及今后的趋势。     

载人航天的发展

简述了国外主要载人航天器的种类、技术参数和发展过程。介绍了我国载人航天工程的发展概况和主要技术指标,并分析了我国发展载人航天在科学、经济和政治等方面的重要意义。     

摆动扫描地球敏感器数学模型及飞行试验结果

描述了东方红三号卫星(DFH-3)控制系统设计和数学仿真中采用的摆动扫描地球敏感器IRES-01的数学模型，东方红三号卫星近三年飞行试验结果与数学仿真结果基本一致，证明数学模型是正确的。     

国外航天侦察相机和测绘相机发展概况

航天侦察和测绘是战略武装必不可少的组成部分,航天侦察和测绘相机是对地观测卫星的有效载荷。 该文将简要介绍国外航天侦察和测绘相机发展概况、水平和发展趋势。     

国际空间站信息系统方案

为了支持在轨系统和有效载荷的操作 ,由硬件和软件组成的空间站信息系统为处理器、工作站、大容量存储单元以及设备接口提供了一个高速、宽带网络。这种结构的关键点是 :1开放式的并且是非专用的 ,避免传统设计方法的浪费。 2结构化和标准化 ,支持组装、增长性和技术性插入。 3采用标准的与用户隔离的硬件和软件接口组成 ,使用户避免了系统的复杂性 ,并且简化了集成 ,缩短了设计周期 ,压缩了研制和维护费用。文中对国际空间站信息管理系统的结构、初期设计、接口和向用户提供的服务做了概要性叙述