水工质微波加热推力器的击穿点火与离解损失估算

对水工质微波等离子推力器(MPT),用微波击穿气体放电产生等离子体的条件,数值估算了其点火的可行性;通过化学动力学计算证明了水工质MPT中离解损失的存在,并初步估算了理解损失的大小。结果表明,在1 kW的输入功率下水工质MPT的点火启动并不特别困难,从点火到稳定工作,能量吸收从场致电离、碰撞电离转变为热电离、碰撞电离和场致电离;水在MPT工作过程中会发生离解,离解损失在各类能量损失中所占的比重较大。     

MPT可靠启动与稳定工作影响因素

1引言MPT属于电热型电推进,基本原理是利用微波发生器将来自电源系统的电能转化为电磁能,然后电磁波在谐振腔中产生谐振并与工质(可选用N2,H2,He,Ar,NH3,N2O或水蒸气等)耦合,使工质离解、电离,形成等离子体,最后高温高压等离子体从喷管高速喷出而产生推力。MPT的最大优点是没有     

介质材料复介电常数变温测量技术综述

介绍了在微波及毫米波段介质材料复介电常数在-253—1400℃的变温测试方法，即网络参数法和谐振腔法，并对这些方法进行了优缺点分析，总结出变温测试方法的概况、趋势及技术特点。     

基于Matlab的约瑟夫森结I-V特性数值分析

基于约瑟夫森结的RSJ模型,采用Matlab程序对无微波辐照和微波辐照下约瑟夫森结的特性进行了数值计算求解,并给出了I-V特性曲线,观察到量子化电压台阶。     

星载毫米波反射面天线结构

“神舟4号”飞船的多模态微波辐射计天线的工作频率跨到毫米波段．这在我国过去的航天器天线中尚未遇到．采用了计算机机电热一体化设计手段，从材料的选择入手，把最佳的电性及结构设计、先进有效的制造、检测与装配技术有机地融为一体之后，保证了天线最终的高精度指标．本文从高精度反射面天线的要求出发，从设计、分析、实现以及验证多方面说明星载反射面天线形面高精度的控制与实现．     

用大失配功率座法测量稳幅环路的等效源反射系数

介绍一种测量信号源反射系数的新方法—采用大失配功率座和不同长度空气线连用,用最小二乘法求解的方法。该方法可以在整个同轴传输线频段10 MHz～26.5 GHz扫频测量,与传统的滑动短路器加测量线的方法比较,这种方法十分方便、快捷。由于采用最小二乘法求解出信号源反射系数,克服了功率和空气线损耗测量不准带来的问题,因此测量小量值的信号源反射系数也较准确。     

微放电效应部件设计研究

分析了影响微放电效应阈值电平的几种因素。对微放电效应部件设计的一般步骤和方法进行了论述 ,给出了具体的设计实例 ,并对微放电效应部件设计中需要注意的问题进行了说明     

Technology Progress Report for Microwave Remote Sensing

In this presentation, technological progress for China's microwave remote sensing is introduced. New developments of the microwave remote sensing instruments for China's lunar exploration satellite (Chang'E-1), meteorological satellite FY-3 and ocean dynamic measurement satellite (HY-2) are reported.     

四极－十六极分区式线型阱中汞离子囚禁仿真研究

利用SIMION软件建立了四极-十六极分区式线型离子阱系统模型，在此基础上仿真模拟了汞离子在四极阱和十六极阱中被囚禁时的第一稳定区，并分析了离子在不同阱中的运动特性。研究了汞离子云在分区式阱中的囚禁体积和速度分布，以及在不同囚禁区域之间的穿梭过程。模拟得出了稳态情况下分区式阱中不同囚禁区域的粒子数密度分布，验证了分区式离子阱中离子云被连续囚禁、穿梭时粒子数衰减和补偿。同时，根据以上数据分析讨论了汞离子囚禁时的多普勒效应，估算了基于此分区式离子阱的汞离子微波钟的性能水平。     

Ozone trends in the mid-latitude stratopause region based on microwave measurements at Lindau (51.66° N, 10.13° E), the ozone reference model,and model calculations

We compared 8 years of ozone measurements taken at Lindau (51.66° N, 10.13° E) at altitudes between 40 and 60 km using the microwave technique with the CIRA ozone reference model that was established 20 years ago (Keating et al., 1990). We observed a remarkable decrease in ozone density in the stratopause region (i.e., an altitude of 50 km), but the decrease in ozone density in the middle mesosphere (i.e., up to 60 km in altitude) is slight. Likewise, we observed only a moderate decrease in the atmospheric region below the stratopause. Other studies have found the strongest ozone decrease at 40 km and a more moderate decrease at 50 km, which is somewhat in contradiction to our results. This decrease in ozone density also strongly depends on the season. Similar results showed model calculations using the GCM COMMA-IAP when considering the increase in methane. In the lower mesosphere/stratopause region, the strongest impact on the concentration of odd oxygen (i.e., O₃ and O) was observed due to a catalytic cycle that destroys odd oxygen, including atomic oxygen and hydrogen radicals. The hydrogen radicals mainly result from an increase in water vapor with the growing anthropogenic release of methane. The finding suggesting that the stratopause region is apparently attacked more strongly by the water vapor increase has been interpreted in terms of the action of this catalytic cycle, which is most effective near the stratopause and amplified by a positive feedback between the ozone column density and the ozone dissociation rate, thereby chemically influencing the ozone density. However, the rising carbon dioxide concentration cools the middle atmosphere, thereby damping the ozone decline by hydrogen radicals.