瞬态平面热源法热物理性能测量准确度和适用范围的标定——常温下标准Pyroceram 9606材料热物理性能测量

瞬态平面热源法作为一种非稳态热物理性能测试技术,其测量范围、测量准确度和试验参数的确定是正确评价和应用这种测试技术的前提条件。详细介绍了瞬态平面热源法的测量原理以及常温下的测量装置,描述了采用Pyroceram 9606热物理性能标准材料研究瞬态平面热源法在实际测试中各种试验参数对测量准确度的影响,并由此考察这种测试方法和测试装置的测量准确度。     

航天材料热物理性能测试技术的发展现状

根据航天材料热物理性能测试技术的特点 ,系统介绍了国内航天材料热物理性能测试技术的发展状况和发展趋势 ,并详细介绍了目前我国航天材料热物理性能测试领域中所具备的测试技术和测试装置、航天热物理性能所涉及的研究领域和内容以及目前正在开展的研究工作。     

高时间分辨力瞬态热反射显微热成像装置

瞬态热反射显微热成像能够测量电子器件表面温度分布,兼具高时间分辨力和高空间分辨力,在GaN HEMT等大功率器件热测试中应用日益广泛。研发了瞬态热反射显微热成像装置,利用窄脉冲照明,捕捉特定短时间内被测器件表面的图像,实现瞬态热反射热成像,时间分辨力达到1 μs。以微带电阻作为被测器件开展了瞬态测温实验,激励脉宽10 μs,测试得到了不同时刻微带电阻上温度分布,可以观察到升温和降温过程的细节,温度上升和下降时间在（2~3） μs,有效验证了装置的时间分辨力性能。     

材料热物理性能非稳态测量方法综述

非稳态法具有快速、准确的特点,一次测量可同时得到热导率、热扩散率和热容等多个热物性参数,测试范围可覆盖多种材料和较宽的热参数区间。阐述了目前国际上主要的六种非稳态测量方法及特点、测量原理及理论模型公式。     

非稳态平面热源法同时测量材料的导热系数和热扩散率

介绍了非稳态平面热源法的测量原理、传热数学模型及温度响应公式,建立了相应的实验装置并进行实际测量。研究结果表明,只需测量试样内某一点的温度变化就可同时得到材料的导热系数和热扩散率以及体积热容等热物性参数。     

卫星热控系统的动态特性建模与仿真

受控对象的动态特性是卫星热控系统设计的基础,为了更加简便地进行卫星热控系统的动态特性计算,根据卫星各部分的温度变化特点及它们之间的热量传输关系,将其划分为外壳、辐射器、舱内环境、关键仪器设备以及相变蓄热装置5个集总参数热控环节,建立起各热控环节温度变化的数学模型.应用这一模型可以十分简便地计算内部热源强度及空间外热流变化时卫星各热控环节的温度变化趋势,其计算过程较常规的卫星瞬态温度场计算简单、方便,满足了对卫星热控系统进行仿真研究和控制策略优化的迫切需要,这对发展各种主动热控制技术来说具有尤其重要的意义.     

用于热控涂层性能原位测试的辐射计设计

针对空间环境中热控涂层性能退化的问题,提出一种模拟空间环境中利用测热法实现热控涂层太阳吸收率原位测试的辐射计设计方案.结合模拟空间环境的测试要求,进行辐射计的原理设计与理论研究;对辐射计进行结构热分析,建立辐射计测试过程中各项换热的计算式,从而得到辐射计的瞬态计算模型.恒温测试环境下利用辐射计对SR107热控涂层进行了测试.实验结果表明:辐射计测试的SR107热控涂层太阳吸收率值与该涂层的标定值之间的相对误差在2%以内,测试的不确定度为6.3%,实验结果验证了该测试方法的有效性.      

吸热碳氢燃料热沉测量实验装置的设计与性能测试

为了测定吸热碳氢燃料在不同温度条件下的总吸热量(热沉),以便于对吸热碳氢燃料进行筛选,研制了一套适合于高温下热沉测量的实验装置。该装置主要由进样计量、载气输送、加热控温、反应量热和产物分析五部分组成。对反应管轴向温度分布进行了测定,实验装置的工作温度范围在500℃-900℃,各温度下恒温区域长达440 mm,恒温区内温度梯度不大于3℃;利用电能标定的方法测定了装置的量热常数,并用纯物质(N2)作为样品对装置的准确度进行了校准,求解仪器量热常数的工作曲线的线性相关系数在0.999 7以上,氮气热沉测定值与理论值基本吻合,表明该装置测定结果可靠、测量准确度高,装置的设计符合T ian’s方程,可用于吸热碳氢燃料热沉的实验测定,为吸热碳氢燃料的研究提供了较可靠的热化学数据。     

铝合金2A12在热冲击条件下的力学性能

测试并确定航空航天材料在复杂高速热冲击条件下的强度极限等关键参数,对于航空航天材料和结构的可靠性评定、寿命预测以及高速飞行器的安全设计具有重要的意义.针对强度设计手册中没有航空航天材料在高速热冲击环境下的强度极限等表征参数的现状,使用自行研制的高速飞行器瞬态气动热试验模拟系统,对铝合金材料2A12在多种不同的瞬态热冲击条件下,进行气动加热模拟与热载联合试验研究,得到在瞬态热、力学环境的共同作用下铝合金2A12材料的强度极限等力学性能变化状况.为研究分析航空航天材料和结构在高速热冲击环境下的承载能力和结构减重提供可靠依据.      

卫星天线在热真空试验中的全场变形测量技术

为真实卫星天线在卫星地面实验站进行了热变形测量的需求,利用卫星天线小模型,进行测试技术研究,用电子散斑干涉技术,在无特殊隔振的条件下,进行全场动态变形测量,获得了全场变形的信息,结果表明,该项技术完全有可能用于真空卫星天线热变形时实时测量。     

Consequences of the application of the streamer fluid model to the study of the sprite inception mechanism

We present the results of a streamer-fluid model used to investigate the electrodynamical coupling between the troposphere and upper atmosphere due to the penetration of lightning electric fields into the mesosphere and the lower ionosphere, generating sprites. The model solves the continuity equation for electrons and ions coupled to Poisson equation. The dominant physical response of the atmosphere is the formation of a screening-ionization wave. The wave shields the atmosphere above it from the action of the lightning field and, together with the conductivity reduction below it due to attachment, the wave amplifies the total field below it, allowing for the penetration of intense electric fields in the mesosphere as it propagates downwards into regions of higher density that compress the wave. This is the key physical mechanism for sprite inception. We evaluated the effects of the thundercloud charge geometry, lightning current waveshape, atmospheric conductivity, via different electron density profiles, and the effect of ionization, attachment and electron mobility coefficients in the electrical breakdown process, related to halo production, and sprite streamer initiation. The results showed that electrons with higher mobility are more efficient in shielding the lightning electric field before breakdown, causing delay, and they contribute to the formation of the streamer seed after breakdown, anticipating the sprite streamer inception. Similarly, a higher effective ionization rate, produced by modifications in the attachment and ionization coefficients, anticipates sprite inception. The simulations with 6 different electron density profiles, and therefore conductivities, spanning 4 orders of magnitude, showed that the altitude of breakdown and sprite initiation, as well as their time delays from the lightning discharge are directly related to atmospheric conductivity: higher conductivities produce halo and sprite inception at lower altitudes with longer delays and may hinder sprite formation. We document that variations of 30 times in the lightning current leads to sprite initiation altitudes in the range 66.0–73.5 km, with delays between 1.550 and 34.500 ms, while variations of 4 orders of magnitude in the conductivity profile lead to initiation altitudes 61.0–70.6 km, with delays in the range 3.825–9.825 ms. Consequently, we suggest that lightning characteristics dominate over atmospheric parameters in determining sprites’ initiation altitude and delay. The simulation of a −CG, with a constant current of 30 kA, did not produce a sprite seed, confirming an asymmetry in the response of the atmosphere to positive and negative lightning. This is due to the free electron drift direction that is away from the screening ionization wave, preventing the formation of the streamer seed for the great majority of −CGs. The same does not apply to halos, which depend on the occurrence of breakdown and can be produced by discharges of both polarities.     

电离层电场对磁层活动响应时延的模式研究

本文用极盖边界上电离层驱动电位φ₀随时间变化的不同模式计算了场向电流J_∥2及电离层对流电场E的演化过程。计算表明,当φ₀(t)先升后降有极大值时,J_∥2(t)和E(t)也表现出类似的趋势。但它们的极值滞后于φ_0max出现的时刻,即在一段时间内,φ₀虽已开始下降,J_∥2及高纬E却继续增大。一般说,E先于J_∥2达到极值,但相差甚小。φ₀变化形式不同时,滞后时间亦不同。当φ₀陡升缓降时,E、J_∥2的极值相对于φ_0max的时延可超过一小时。这与持续时间较长的磁暴期间所观测到的电离层场强响应时延量级是一致的。时延大小还受电离层电导率的制约。低纬电离层场强的响应与高纬不同,其升降趋势与φ₀同步。      

Comprehensive investigation of the basic parameters of the upper atmosphere at the time of the flight of the geophysical rocket “vertical-6”

Ion temperature and total ion concentration measured on 25th October 1977 during the flight of the geophysical rocket “Vertical-6” are analyzed. The solar EUV fluxes determined in five wave-length bands with a photoelectron analyzer are also given. The observed anomalous variation of ion temperature between 700 and 900 km and the measured ion concentration can be explained, if the charge exchange reactions H⁺ ? O⁺ and diffusion are taken into account.     

落塔微重力水平激光干涉测量方法中的干扰因素分析

落塔是获得微重力环境的重要设施,落塔微重力水平的测量对微重力科学实验的研究至关重要. 激光干涉是测量落塔微重力水平的一种新方法,这种方法的基本原理是让一个参考落体在落舱中自由下落,落舱由于受到服外空气阻力的作用将与自由落体运动略有差异,1 11. 肫内的参考落体则更接近理想的自由落体运动,这就使得落舱与参考落体之间存在着加速度差,这种加速度差便反映了落服的微重力水平,其所导致的相对运动则可通过激光干涉的方法测量出来. 本文对落塔微重力水平的激光干涉测量方法中将会遇到的一些主要干扰因素进行了分析,计算结果表明,这些干扰网素所造成的总误差约为 1.2 x 10-7g,低于微重力水平的预测值 10-4~lO-6 g,因此该方法是一种比较可行的测量方法.      

热流效应对场向电流确定的影响

给出了任意速度分布函数条件下复频率的介电函数和色散关系的求解方法. 讨论了16矩近似条件下, 场向热流对电子速度分布函数, 介电函数实部与虚部, 以及离子与电子谐振频率和阻尼率的影响, 并与平衡态时麦克斯韦分布等离子体的计算结果进行了比较. 忽略场向热流效应, 正向电子漂移速度条件下, 上行等离子线探测, 会过高估计场向电流; 负向电子漂移速度条件下, 上行等离子线探测会过低估计场向电流. 对上下行等离子线同时探测情况, 忽略热流效应同样会过高估计场向电流.      

推力架测试系统误差的研究

针对卫星推进系统小推力测量的特点,主要是分析推力架系统所带来的推力误差,对引起推力误差的因素进行了分析研究,并提出了误差相应的解决方法和试验数据处理方法     

Possible physical properties of the flow in the vicinity of the heliopause

An interface between the fully ionized hydrogen plasma of the solar wind (SW) and the partially ionized hydrogen gas flow of the local interstellar medium (LISM) is formed as a region where there is a strong interaction between these two flows. The interface is bounded by the solar wind termination shock (TS) and the LISM bow shock (BS) and is separated on two regions by the heliopause (HP) separating the solar wind and charged component of the LISM (plasma component below). The BS is formed due to the deceleration of the supersonic LISM flow relative to the solar system. Regions of the interface between the TS and HP and between the HP and BS were in literature named as the inner and outer heliosheaths, respectively. An investigation of the structure and physical properties of the heliosheath is at present especially interested due to the fact that Voyager-1 and Voyager-2 have crossed the TS in December 2004 (Burlaga, L.F., Ness, N.F., Acuna, M.Y., et al. Crossing the termination shock into the the heliosheath. Magnetic fields. Science 309, 2027–2029, 2005; Fisk, L.A. Journey into the unknown beyond. Science 309, 2016–2017, 2005; Decker, R.B., Krimigis, S.M., Roelof, E.C., et al. Voyager 1 in the foreshock, termination shock and heliosheath. Science 309, 2020–2024, 2005; Stone, E.C., Cummings, A.C., McDonald, F.B., et al. Voyager 1 explores the termination shock region and the heliosheath beyond. Science 309, 2017–2020, 2005) and in September 2007 (Jokipii, J.R. A shock for Voyager 2. Nature 454, 38–39, 2008; Gurnett, D.A., Kurth, W.S. Intense plasma waves at and near the solar wind termination shock. Nature 454, 78–80, 2008. doi: 10.1038/nature07023; Wang, L., Lin, R.P., Larson, D.E., Luhmann, J.G. Domination of heliosheath pressure by shock-accelerated pickup ions from observations of neutral atoms. Nature 454, 81–83, 2008. doi: 10.1038/nature07068.14; Burlaga, L.F., Ness, N.F., Acuna, M.H., et al. Magnetic fields at the solar wind termination shock. Nature 454, 75–77, 2008. doi: 10.1038/nature07029; Richardson, J.D., Kasper, J.C., Wang, C., et al. Cool heliosheath plasma and deceleration of the upstream solar wind at the termination shock. Nature 454, 63–66, 2008. doi: 10.1038/nature07024; Stone, E.C., Cummings, A.C., McDonald, F.B., et al. An asymmetric solar wind termination shock. Nature 454, 71–74, 2008. doi: 10.1038/nature07022; Decker, R.B., Krimigis, S.M., Roelof, E.C., et al. Mediation of the solar wind termination shock by non-thermal ions. Nature 454, 67–70, 2008. doi: 10.1038/nature 07030), respectively, and entered to the inner heliosheath.     

火星地形对火星大气运动的影响及火星尘暴发生的可能机制

本文在准地转模式的假定下,讨论了火星地形对火星大气的影响,并根据文章所提供的信息对火星尘暴发生的物理机制作了粗略的解释。      

Testing the improvement of performance of the IRI model in the estimation of TEC over the mid-latitude American regions

This paper mainly discusses the improvement of performance of the International Reference Ionosphere (IRI) model in estimating the variation of the Vertical Total Electron Content (VTEC) over the mid latitude American regions during the relatively low (2008–2010) and relatively high (2012) solar activity years. This has been conducted employing the VTEC values obtained from the dual frequency ground based Global Positioning System (GPS) receivers located at Mineral Area Community College, MACC (37.85°N, 269.52°W) and Mississippi County Airport, MAIR (36.85°N, 270.64°W), and the latest versions of the IRI online model (IRI 2007, IRI 2012 and IRI 2016). The study mainly focuses to compare the trend of variability of the monthly and seasonal modeled VTEC values (IRI 2007 VTEC, IRI 2012 VTEC and IRI 2016 VTEC) with the corresponding measured VTEC values (GPS VTEC). The overall results show that the IRI VTEC values (almost in all versions of the model) are generally smaller than the GPS VTEC except after about 15:00 UT (09:00 LT) in the December solstice when the Sun shifts to the high solar activity. On the contrary, overestimations of the VTEC values by the model are observed in traversing from the low solar activity (2008) to high solar activity (2012) phase, especially after about 15:00 UT (09::00 LT) with the IRI 2016 version showing the highest. In general, the IRI 2007 and IRI 2012 versions show similar monthly and seasonal underestimations or overestimations showing that the two versions have almost similar performance. The IRI 2016 version is generally better in capturing both the diurnal and arithmetic mean GPS VTEC values with some exceptional months and seasons as compared to those of the IRI 2007 and IRI 2012 versions.     

Features of the occurrence of the additional stratification on the bottom-side F region over the equatorial location of Trivandrum

The general features of occurrence of an additional layer on the bottom side of F region, referred to as F0.5 layer in the pre noon period, over the magnetic equatorial location of Trivandrum (8.5° N; 77° E; dip lat of 0.5° N) in India during the period from 2004 to 2007 are presented using ionosonde observations. The F0.5 layer has a June (northern summer) solsticial maximum probability of occurrence with secondary maxima during December (northern winter) solstice. The seasonal as well as the day-to-day variability in the occurrence of F0.5 layer as mentioned in this paper seems to be a result of the variations in the amplitude and phases of the tides and gravity waves, and inventory of the metallic ions of meteoric origin. This study brings out an important manifestation of morning time F layer base region dynamics.