基于非线性混合模型研究太空风化对月壤光谱的影响

月表太空风化会改变月壤光谱特征, 影响月壤元素遥感反演精度. 研究太空风化对月壤光谱的影响有助于开发月壤成熟度光谱解耦算法, 提高月壤成分遥感反演精度. 直接对比月壤风化前后光谱的变化能最真实反映太空风化对光谱的影响, 但无法获取未风化的月壤样品, 利用实验室模拟方法开展研究也存在缺陷. 本文提出了一种简便的方法来研究太空风化对月壤光谱的影响, 并以月海样品为例进行探讨. 利用Hapke模型对月海样品组成矿物光谱按照实测含量进行非线性混合, 并通过对比混合后的光谱与实测的月壤光谱, 研究太空风化过程对月壤光谱的影响. 研究结果表明, 月壤在遭受太空风化后反射率降低, 波长越短降低越显著; 月壤背景吸收斜率增大, 月壤变得更红, 月壤矿物特征吸收峰深度降低, 光谱对比度变弱, 长波吸收峰(2.0μm附近)深度降低程度超过短波吸收峰(1.0μm附近)深度. 未来在利用遥感技术反演月壤元素含量时, 必须考虑这些因素.      

基于衬底偏置的超低耗电流复用混频器

基于SMIC 0. 18μm 1P6M CMOS工艺,设计实现了一种工作在0.6V超低电源电压下的混频器.该混频器跨导级采用自偏置的互补跨导结构,并与开关级构成折叠结构,大大降低了电源电压;电路中所有的MOS管衬底均加有固定偏置电压,减小了MOS管的阈值电压,实现了超低电压超低功耗的设计;并采用电流复用技术,改善了电路的噪声性能,并提高了其转换增益和线性度.该混频器核心电路尺寸为460μm×400μm,当射频信号、本振信号和中频信号分别为1575MHz,1400MHz和175MHz时,仿真表明,该混频器转换增益(G_c)为6.1dB,双边带噪声系数为14dB,输入1dB压缩点为-16.67dBm,在0.6V的电源电压条件下,功耗仅为0.76mW,可用于航空航天领域的电子系统中.     

月表温度和地形对科研站选址的影响

月球极区具有独特的地理特征和潜在的水冰资源,是未来月球科学探测和基地建设的优选区域。但月球极地具有太阳光照条件差异显著、月地直接通信范围有限、月表温度变化幅度大、地势陡峭等特点,对选址研究提出了巨大挑战。定量化地研究月球极地相对宜居区的温度和地形分布,对于深入探索月球极地具有重要意义。利用月球勘测轨道器(LRO)上搭载的激光高度计(LOLA)和辐射计(Diviner)的观测数据产品,建立了一种月球相对宜居区的评估方法;并以月球南极为目标选取了典型的相对宜居区,对相对宜居区内的表面温度的日变化和季节变化特征进行了研究,分析对比了各相对宜居区的地形坡度、表面粗糙度和地形高度分布等情况。其中区域A(Scott M附近)地处月球南极的相对高地(约3～7 km),坡度(中位数为8°)和表面粗糙度(小于2 m)适中;区域B(de Gerlache附近)最靠近南极中心,太阳可见度可高达0.8,坡度较陡(中位数为12.4°),表面粗糙度适中(小于2 m);区域C(Amundsen附近)的地势最低(约-1.8～-0.5 km),太阳可见度(小于0.6)和地球可见度(小于0.5)最小,地形坡度最缓(中位数...     

Image Quality assessment for Chang＇E-1 IIM 2C Data

嫦娥一号干涉成像光谱仪（IIM）获取的多波段图像数据对于月表矿物成分反演具有重要意义.从目视质量、客观参数、几何配准精度、图像质量随时间的变化情况等方面对IIM 2C级的多波段图像数据质量进行了评价.结果显示,其两端波段范围的图像质量较差,不能有效识别月表单元,中间波段图像质量较好;自然色图像显示IIM数据存在明显的横向色调不均一性.利用图像的客观评价指标（辐射精度、清晰度、信息量）将干涉成像光谱仪图像数据与美国Clementine UV-VIS多光谱图像数据进行对比分析,结果表明,IIM数据清晰度好于ClementineUV-VIS,而在方差和信息量上弱于Clementine UV-VIS.将IIM图像数据与Clementine多光谱数据统一到相同的空间分辨率,进行配准精度评价,其最大控制点配准误差为0.63 pixel.此外,还对时间跨度两个月覆盖月表同一区域的IIM图像数据从辐射精度、信息量和清晰度方面进行了评价.     

嫦娥一号干涉成像光谱仪2C级图像数据质量评价

嫦娥一号干涉成像光谱仪(IIM)获取的多波段图像数据对于月表矿物成分反演具有重要意义. 从目视质量、客观参数、几何配准精度、图像质量随时间的变化情况等方面对IIM 2C级的多波段图像数据质量进行了评价. 结果显示, 其两端波段范围的图像质量较差, 不能有效识别月表单元, 中间波段图像质量较好; 自然色图像显示IIM数据存在明显的横向色调不均一性. 利用图像的客观评价指标(辐射精度、清晰度、信息量)将干涉成像光谱仪图像数据与美国Clementine UV-VIS多光谱图像数据进行对比分析, 结果表明, IIM数据清晰度好于Clementine UV-VIS, 而在方差和信息量上弱于Clementine UV-VIS. 将IIM图像数据与Clementine多光谱数据统一到相同的空间分辨率, 进行配准精度评价, 其最大控制点配准误差为0.63pixel. 此外, 还对时间跨度两个月覆盖月表同一区域的IIM图像数据从辐射精度、信息量和清晰度方面进行了评价.      

海洋水色卫星的用途和特点

1　海洋水色探测原理□□众所周知 ,太阳入射至海洋表面的能量约占入射能的 3 0 % ,其余 70 %被大气吸收或散射后反射入太空。入射至海面的太阳能一部分被海面吸收或直接反射 ,另一部分透射进入水体。进入水体的太阳能光谱只有可见光 (0 .4 0 μm～ 0 .76μm) ,其中蓝光波段(0 .4 9μm)透水性能最好 ,如是清洁海水可透水几十米 ,其他波段透水性能远不如蓝光。透射入水的太阳能中一部分被水分子吸收 ,另一部分经水分子、浮游生物和悬浮颗粒等有机物质或无机物质散射 ,经散射后一部分离开水面反射出来 ,这部分反射能称为离水辐射能 ,对应的功…     

月球表面太空风化作用及其效应

太空风化作用普遍发生在月球、小行星等一些无大气层的天体表面, 主要包括太阳风离子辐射和微陨石撞击等作用. 通过对真实月球样品太空风化作用的研究成果以及低能离子和激光照射等地面模拟实验结果的系统综述和分析, 重点分析了月壤颗粒中非晶质层和纳米铁的成因, 指出太空风化研究中存在的太阳风离子辐射和微陨石撞击贡献难以区分及模拟实验模拟效果尚不充分的问题.进而提出月球太空风化研究不能简单套用其他天体的模型, 并建议未来开展更多月球和陨石样品的精细化学分析.      

臭氧9.6μ带总吸收比的实验测定

在室温(约18℃)下测定了臭氧(O₃)9.6μ带的总吸收比,O₃含量在0.0188-0.5atmcm,压力在17—760mmHg之间。实验中使用了十字型吸收池,其一支通过紫外线,用以测量臭氧含量;另一支通过红外线,用以测量臭氧9.6μ带的总吸收比。对实验数据应用光谱模式理论进行了分析和处理,结果表明本实验资料与统计模式符合。最后给出了适用于统计模式的带参数。      

火星再入飞行器风洞试验与真实飞行之间相关性的探讨

由于风洞试验条件限制,难以完全模拟火星再入飞行器真实飞行环境,因此需要建立火星再入飞行器风洞条件与真实飞行之间的关联关系。基于国外文献公开数据,采用数值方法和对比分析方法探讨了类"探路者号"外形的火星再入飞行器的风洞试验与真实飞行之间的外推方法。结果表明,在高焓空气风洞和常规空气风洞试验条件下,可以将模型驻点附近的无量纲压力和压力系数作为相关性参数,将风洞条件与飞行条件相关联起来,但是不能直接利用风洞试验的热流、无量纲热流和Stanton数作为关联参数;在高焓CO₂风洞试验条件下,可以利用模型驻点附近的无量纲压力、压力系数和Stanton数作为外推参数,但是不能直接将风洞试验的热流、无量纲热流作为相关性参数,将风洞条件下的风洞数据通过外推获取飞行条件下飞行器的性能参数。      

实践十号上的19项实验

正在实践十号返回式卫星上,进行了19项新奇又有趣的实验,这颗卫星的首席科学家、中科院院士胡文瑞说:"这些科学实验具有创新性和很强的科学研究价值,将孕育学术上重大问题的突破。"1.微重力条件下哺乳动物早期胚胎发育研究这一研究将展示哺乳动物早期胚胎在太空环境下的发育情况,揭示太空环境下哺乳动物早期生命活动规律,为保障人类太空活动中生殖发育健康提供科学依据。在国内外,迄今尚未见到在空间     

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.     

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.      

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.     

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.     

Method for the prediction of the effective dose equivalent to the crew of the International Space Station

This paper describes a methodology for assessing the pre-mission exposure of space crew aboard the International Space Station (ISS) in terms of an effective dose equivalent. In this approach, the PHITS Monte Carlo code was used to assess the particle transport of galactic cosmic radiation (GCR) and trapped radiation for solar maximum and minimum conditions through an aluminum shield thickness. From these predicted spectra, and using fluence-to-dose conversion factors, a scaling ratio of the effective dose equivalent rate to the ICRU ambient dose equivalent rate at a 10 mm depth was determined. Only contributions from secondary neutrons, protons, and alpha particles were considered in this analysis.     

Influence of the Ionosphere on the Observation of the Mid-Latitude Pi2 Pulsations at the Global Scale

Results of our investigation showed that occurrence frequency of Pi2 over a 24 hour period undergoes seasonal variations in time coincidence with foF2. In the winter months, at sunrise and sunset (when foF2gradients are the largest) the observation probability of these oscillations is minimal. At periods of summer solstice when the F2-layer persists almost round the clock, no effect of Pi2 pulsation attenuation is observed at sunrise and sunset. The pulsation amplitudes behave in a similar manner. Results of this study suggest the conclusion that the propagation of signal from the Pi2 sourse into the mid-latitudes, and also the parameters of these pulsations are essentially affected by electron density in the ionospheric F2-layer.      

Effects of the position of the solar wind termination shock and the heliopause on the heliospheric modulation of cosmic rays

The effects of changing the position of the solar wind termination shock and the position of the heliopause, and therefore the extent of the heliosheath, on the modulation of cosmic ray protons are illustrated. An improved numerical model with diffusive termination shock acceleration, a heliosheath and drifts is used. The modulation is computed in the equatorial plane and at 35 heliolatitude using recently derived diffusion coefficients applicable to a number of cosmic ray species during both magnetic polarity cycles of the Sun. It was found that qualitatively the modulation results for the different heliopause positions are similar although they differ quantitatively, e.g., clearly different radial gradients are predicted for the regions beyond the termination shock compared to inside the shock. The difference between the modulation for the two solar polarity cycles are less significant at a heliolatitude of 35° than in the equatorial plane. We found that moving the termination shock from 90 to 100 AU, with the heliopause fixed at 120 AU, caused only quantitative differences so that the exact position of the TS in the outer heliosphere seems not crucially important to global modulation. Moving the heliopause outwards, to represent the modulation in the tail region of the heliosphere, causes overall decreases in the cosmic ray intensities but not linearly as a function of energy, e.g., at 1 GeV the effect is insignificant. We conclude from this modelling that the modulation of protons in the heliospheric nose and tail regions are qualitatively similar although, clear quantitative and interesting differences occur.     

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。      

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.