SPACE LIFE SCIENCE IN 2000-2001

Chinese scientists studied some of the problems in the field of space life science and achieved success in the area during 2000-2001. Space biological experi ments were carried out in the orbit and the results of ground studies on protein crystallization, space radiation, space motion sickness were introduced in this paper. The influences of simulated weightlessness on the brain-function, the car diovascular, endocrine hormones, immunity, skeletal and muscle systems were presented. In addition, gravity medicine and space environment medicine, as well as countermeasures to space deconditioning, such as the traditional Chinese medicine, were also reported.     

KuaFu Mission

The KuaFu mission-Space Storms, Aurora and Space Weather Explorer-is an "L1+Polar" triple satellite project composed of three spacecraft: KuaFu-A will be located at L1 and have instruments to observe solar EUV and FUV emissions, and white-light Coronal Mass Ejections (CMEs), and to measure radio waves, the local plasma and magnetic field,and high-energy particles. KuaFuB1 and KuaFu- B2 will bein polar orbits chosen to facilitate continuous 24 hours a day observation of the north polar Aurora Oval. The KuaFu mission is designed to observe the complete chain of disturbances from the solar atmosphere to geospace, including solar flares, CMEs, interplanetary clouds, shock waves, and their geo-effects, such as magnetospheric sub-storms and magnetic storms, and auroral activities. The mission may start at the next solar maximum (launch in about 2012), and with an initial mission lifetime of two to three years. KuaFu data will be used for the scientific study of space weather phenomena, and will be used for space weather monitoring and forecast purposes. The overall mission design, instrument complement, and incorporation of recent technologies will target new fundamental science, advance our understanding of the physical processes underlying space weather, and raise the standard of end-to-end monitoring of the Sun-Earth system.     

空间飞行体与等离子体在压缩区内的非稳态相互作用研究

研究了空间飞行体在运动过程中，其前端压缩区内飞行体与等离子体的、非稳态相互作用问题，得到了在强天线辐射源高频场作用下的控制方程．通过计算表明，飞行体上的天线可作为调制不稳定性的激发源，在等离子体中激发起很强的电磁孤波．     

2000年4月6-8日磁暴期间电离层TEC观测研究

利用北京、乌鲁木齐、武汉GPS观测数据计算的垂直总电子含量，分析了发生于2000年4月6-8日磁暴期间观测区域的电离层状态。结果表明，在4月7日北京时间0200-0700之间，在中、低纬地区出现了较弱的电离层负相暴，与前一日相比，最大TEC之差在-8TECU左右；在北京时间0700之后，在较高纬度地区开始出现强列的电离层负相暴，并且该负相暴随着时间逐渐增强；但在北京时间0700-0900之间，在低纬地区出现了电离层正相暴。在定时间内较高纬度地区的负相暴逐渐增强并向南移动而低纬地区的正相暴经历了增强到减弱的过程。     

直升机飞行动力学仿射非线性系统建模

建立一种单旋翼带尾浆直升机飞行动力学仿射非线性系统数学模型，为进一步开展直升机非线性系统特性和控制律设计研究做准备，建模过程中，保证了控制量能在方程中线性表示，又保证了模型的精度，以ＵＨ－６０Ａ直升机为对象，进行定直飞行配平计算以及直升机对不同操纵输入的动态响应计算，计算结果与试飞结果吻合，与国外较成熟的非线性工程实时仿真模型相比有相当的精度，证明建模理论和方法的合理和有效。     

1958年7月8日磁暴的电离层响应

本文用遍布全球的52个电离层垂测台站资料,研究1958年7月8日磁暴期间全球电离层扰动的发展变化;各扇区的响应特性;扰动的传播轨迹及速度等。获得以下结果:1.几大扇区的电离层扰动始于南北两极,美洲扇区除具这一特征外,其赤道地区在磁暴急始后不久,出现一个扰动中心,邻近区域的扰动受其控制。2.扰动由高纬向低纬发展,由扰动中心向外传播。3.扰动峰面几乎与地磁力线垂直,即扰动沿磁力线方向发展,其传播速度大约在150—600m/s范围。     

冲击响应谱（SRS）分析数字化方法探讨

本文介绍了求单自由度二阶系统冲击响应谱（ＳＲＳ）的几种常用的数字化分析方法：直接积分法；快速富氏变换（ＦＦＴ）法；递推法；数字滤波器方法；改进的数字滤波器方法。并比较了它们的优缺点。     

PRACTICAL G~2 CONTINUITY ALGORITHMS BETWEEN ADJACENT NURBS PATCHES

Geometriccontinuityiswidelyrecognizedastheappropriatewaytofittogethertwoadja-centsurfacepatchesinCAD/CAM.ItavoidsdePendenceofparametrizatinnandprovidesaddi-tionalparametersformodelingtheshapes.Apatchworktechniqueconstructsanycompositesurfacestraightforwardly,patchbypatch.ThetangentplanecontinuityG1andcurvaturecon-tinuityG2ofparametricsurfacepatcheshavebeenstudied[1~6J-AlltheseresearchersworkwithsurfacepatchesinBezierformandrationalBezierform.IncontrasttoNURBSsurface,BezierandrationalBe…     

在高燃速推进剂中粗颗粒铝粉的作用

本文用50μm铝粉作复合固体推进剂金属燃料,与大量超细氧化剂(AP)组成合理级配,改善了药浆流变特性,有利于提高燃速。50μm铝粉的推进剂药条的燃速及φ118发动机推进剂的燃速比相应的填加30μm铝粉的高2～3mm/s。讨论了50μm铝粉对推进剂工艺和燃速所起的作用。     

含硼富燃料推进剂燃烧机理研究

分析了AP包覆硼对含硼富燃料推进剂低压燃烧的影响。通过微热电偶测温和火焰单幅照相技术分别测试含硼富燃料推进剂燃烧波温度分布及燃烧火焰结构；根据气相温度变化的趋势，把该推进剂的气相区燃烧又分为三个子区，并给出了三个子区的厚度，分析了各区温度变化趋势不同的原因。用扫描电镜对熄火表面形貌进行观察，并通过能谱仪进行局部元素分析；该推进剂中断燃烧熄火纵向剖面的实验表明，该推进剂的燃烧表面存在“沉积层”；分析认为该“沉积层”由硼、积炭和少量的三氧化二硼组成，且基本惰性。燃面上“沉积层”的厚度与温度分布曲线中燃面上气相区的厚度基本一致，认为该推进剂的气相反应在燃面上的惰性“沉积层”中进行。