基于氧气A波段临近空间大气温度反演的贝叶斯与最小二乘法对比

基于氧气A波段的临边辐射模拟数据进行临近空间大气温度廓线的反演，分析比较了贝叶斯和最小二乘两种不同反演算法的特点.80km以下，信噪比为66～337时:基于贝叶斯理论反演的三条谱线761.59，762.2，764.05nm的反演误差平均值分别为5.52，3.94，4.73K；采用最小二乘法的反演误差平均值分别为10.57，7.04，8.80K.信噪比为6～34时:基于贝叶斯理论反演的三条谱线的反演误差平均值分别为18.27，12.18，18.27K；采用最小二乘法的反演误差平均值分别为103.18，68.79，85.98K.研究结果表明，基于贝叶斯理论的反演方法，利用先验信息对反演结果进行约束和修正，在有噪声的情况下获得了更合理的解，从而提高了反演精度和抗干扰能力.这为星载探测临近空间大气温度的算法研究和开发提供了参考，也为提高光谱仪器信噪比并进而提高温度反演精度提供了理论基础.      

基于CO2浓度监测的飞机火警探测方法

目前飞机普遍采用感温、感烟火警探测方法,其存在误报率高的缺陷.分析了发生火灾时气态燃烧产物的生成规律,提出了以CO_2气体为火警探测参量,通过准确监测环境中CO_2气体浓度的变化,进行飞机火警探测的方法;根据飞机飞行所处环境条件的特殊性,研究了基于非色散红外(NDIR)吸收原理的CO_2气体浓度监测的飞机火警探测方法应用于飞机上所面临的温度补偿难题;根据飞机火警探测器测量电压与环境温度、参比电压之间的关系,采用偏最小二乘(PLS)法建立飞机火警探测器温度补偿模型;根据飞机火警探测器测量电压与CO_2气体浓度之间的关系,采用PLS法建立CO_2气体浓度计算模型;研究了基于CO_2气体浓度监测的报警算法,为飞机火警探测提供了一种新的方法.     

以载荷为中心的暗物质探测卫星机电热一体化设计

暗物质粒子探测卫星是中国第一颗空间高能探测卫星,用于实现5GeV~10TeV大动态范围高能宇宙线（电子、正电子、伽马射线等）能谱测量.卫星有效载荷包括BGO量能器、硅阵列探测器、塑闪阵列探测器和中子探测器,是目前中国发射的载荷比最大的卫星.本文介绍了卫星相关技术方案,包括技术指标、轨道方案、工作模式及系统组成等,突出了其以载荷为中心的机电热一体化设计特点.      

（20～400）MeV准单能中子参考辐射场的建立方法CSCD

为了满足对高能中子辐射场测量仪器进行校准的需要,必需建立20MeV以上的准单能中子参考辐射场.对国际上（20～400） MeV准单能中子参考辐射场的建立情况及建立方法进行了调研,可通过7Li（p,n）7Be反应获得该能区准单能中子场,中子束流轮廓可通过转换体和影像板进行测量,辐射场中子能谱可利用液体闪烁探测器或者238U裂变电离室通过飞行时间法进行测量,可建立高效率的反冲质子望远镜作为该能区的中子注量测量初级标准.     

大气臭氧地基遥感反演的退卷积方法

本文提出了一种大气臭氧地基遥感信息处理的新方法,它利用非线性退卷积方法和等效仪器函数提高光谱分辨率,利用非线性最小二乘法进行大气臭氧反演计算,可以显着提高大气臭氧遥感的可探测高度和精度。      

基于同波束干涉的空间三维相对位置测量研究

针对深空探测器相对位置精确测量需求,建立了空间三维相对位置测量模型,研究了基于单基线同波束干涉测量(Same-beam VLBI,SBI)的空间三维位置最小二乘解算方法。利用"嫦娥3号"着陆器的测控天线与定向天线的SBI实测数据,验证了测量模型与解算方法的有效性。结果显示:SBI干涉时延随机误差约0.225 ps(0.07 mm);测控天线与定向天线之间距离误差约0.216 m,方向误差约30.4°。该研究结果有望应用于后续深空探测任务譬如"嫦娥5号"器间高精度相对测量中。     

GNSS-IR双频数据融合的土壤湿度反演方法

目前全球导航卫星系统反射信号干涉测量（GNSS-IR）土壤湿度反演研究仅针对单一频点展开,提出用熵值法将2个频点数据进行融合以改进土壤湿度反演精度。首先,利用频谱分析法分别解析出各频点的信噪比（SNR）序列的振荡频率,计算出对应的等效天线高度,并利用最小二乘法求解各频点信噪比序列相位;然后,通过熵值法进行2个频点的相位观测量融合;最后,利用融合结果与实测土壤湿度建立经验模型,实现土壤湿度反演。利用地基观测实验获得的全球定位系统（GPS）L1和L2信噪比数据对该方法进行了验证,结果表明:L1和L2双频融合反演结果平均标准差为0.6%,比L1单频反演结果提高64.73%,比L2单频反演结果提高32.12%;均方根误差为0.37%,比L1频点降低72.8%,比L2频点降低73.4%。      

近红外绝对光谱响应度传递标准的研制CSCD

在光辐射计量中,陷阱探测技术是一种重要的探测技术,陷阱探测器是光辐射功率基准量值保持和传递的主要媒介。 InGaAs 陷阱探测器常被作为（900～1700）nm 波段光辐射计量的传递标准。本文基于陷阱探测技术,针对近红外波段量值传递的需求,研制了 InGaAs 陷阱探测器,并进行了性能测试。测试结果显示：在1064nm处绝对光谱响应率为0.7098A/ W,测量不确定度达到0.1%,在（0.1～3） mW 内,其非线性指标优于0.99993,1h 测试非稳定性为0.00495%,空间非均匀性达到0.05%,满足作为传递标准的技术要求。     

基于X射线掩星探测反演行星大气密度

X射线掩星是一种常见的天文现象，基于X射线掩星探测的大气密度反演是一种涉及学科交叉的新方法，其通过处理高能X射线天体辐射源的掩星观测数据实现大气密度的反演，基本原理为X射线在大气中传播时，X射线光子被大气中的原子（包括分子中的原子）吸收和散射，从而导致X射线强度发生衰减，根据衰减后X射线信号的强度反演对应的密度廓线。本文根据X射线掩星探测的应用需求，论证了基于X射线掩星实现大气密度反演的新方法，重点介绍了光变曲线拟合和能谱拟合两种地球中高层大气密度反演算法，分析了X射线掩星探测反演大气密度的研究进展和研究方法，对基于X射线掩星反演大气密度的优点进行分析和讨论，进而对X射线掩星探测的应用场景进行展望。结果表明，作为一种新型中高层大气密度测量手段，X射线掩星探测可对中高层大气密度实现有效探测，弥补了目前中高层大气密度实测数据的不足。     

以相对偏差平方和为指标函数的最小二乘法

就测量中最小二乘法用于静态模型估计的问题,分析了传统最小二乘法在某些实验条件下应用的不合理现象,提出以相对偏差平方和为指标函数的最小二乘法。简记LSR法。给出了该方法的实用公式,分析了数学特征并证明在所给实验条件下具有无偏性、一致性,有效性.给出了用该方法拟合电位差计静态特性方程的例子。证明该方法在测量工作中是有实际意义的。     

Spectrometers for fast neutrons from solar flares.

Neutrons with energies exceeding 1 GeV are emitted in the course of solar flares. Suitable dedicated neutron spectrometers with directional characteristics are necessary for a systematic spectroscopy of solar neutrons. We report here a study of instruments based on the detection of proton recoils from hydrogenous media, with double scattering in order to provide directional information, and also a novel scheme based on the detection of radiation from the neutron magnetic dipole moment, permitting also directional detection of neutrons. Specific designs and detection systems are discussed.     

Detection of solar neutrons on a long duration balloon flight

The observation of large solar flares on high altitude balloons requires long duration balloon flights because large flares are infrequent and cannot be predicted with enough reliability and lead time to allow a conventional balloon to be launched and reach altitude before the flare occurs. With the many weeks at float altitude expected for a long duration flight, the probability of “catching” a large flare during solar maximum becomes reasonably high and the study of phenomena which heretofore have required a satellite become accessible to a balloon platform. One example of this type of experiment is the observation of neutrons produced by the interaction of flare accelerated nucleons with the solar atmosphere. Because the neutrons are produced immediately by the flare accelerated particles and are unaffected by their transmission through the upper solar atmosphere and the intervening magnetic fields, their observation at 1 A.U. will provide direct information on the flare acceleration process. Specifically, a measurement of the neutron energy and time spectra will yield the energy spectrum of the charged nucleons in the interval 50 to 500 MeV/amu, the charged particle anisotropy, the height of the acceleration region for limb flares, and information on the two-stage acceleration process. Because the γ-ray spectrum is also sensitive to these factors, a combined neutron and γ-ray measurement will provide a much more stringent test of flare models than either done separately. CWRU and the University of Melbourne have designed the EOSCOR (Extended Observation of Solar and Cosmic Radiation) detector to have the necessary sensitivity to detect neutrons from a flare 0.1 the size of the 4 Aug. 1972 event and to be compatible with the constraints of the long duration balloon system. The detector has been test flown on short duration balloon flights and calibrated at E_n = 38, 58, and 118 MeV. It is planned to launch it on a long duration balloon flight from Australia in December 1982 when simultaneous γ-ray observations will be possible with the SMM and/or HINTORI satellites.     

Accuracy analysis of GNSS-IR snow depth inversion algorithms

In recent years, with the continuous development of Global Navigation Satellite System (GNSS), it has been applied not only to navigation and positioning, but also to Earth surface environment monitoring. At present, when performing GNSS-IR (GNSS Interferometric Reflectometry) snow depth inversion, Lomb-Scargle Periodogram (LSP) spectrum analysis is mainly used to calculate the vertical height from the antenna phase center to the reflection surface. However, it has the problem of low identification of power spectrum analysis, which may lead to frequency leakage. Therefore, Fast Fourier Transform (FFT) spectrum analysis and Nonlinear Least Square Fitting (NLSF) are introduced to calculate the vertical height in this paper. The GNSS-IR snow depth inversion experiment is carried out by using the observation data of P351 station in PBO (Plate Boundary Observatory) network of the United States from 2013 to 2016. Three algorithms are used to invert the snow depth and compared with the actual snow depth provided by the station 490 in the SNOTEL network. The observations data of L1 and L2 bands are respectively used to find the optimal combination between different algorithms further to improve the accuracy of GNSS-IR snow depth inversion. For L1 band, different snow depths correspond to different optimal algorithms. When the snow depth is less than 0.8 m, the inversion accuracy of NLSF algorithm is the highest. When the snow depth is greater than 0.8 m, the inversion accuracy of FFT algorithm is higher. Therefore, according to the different snow depth, a combined algorithm of NLSF + FFT is proposed for GNSS-IR snow depth inversion. Compared with the traditional LSP algorithm, the inversion accuracy of the combined algorithm is improved by 10%. For L2 band data, the results show that the accuracy of snow depth inversion of various algorithms do not change with the variations of snow depth. Among the three single algorithms, the inversion accuracy of FFT algorithm is better than that of LSP and NLSF algorithms.     

基于神经网络的OFDM信道补偿与信号检测

针对非线性失真和多径效应混合的复杂信道条件,提出一种基于神经网络的正交频分复用（OFDM）信道补偿与信号检测的方法。首先接收端信号利用最小二乘（LS）算法和迫零（ZF）算法做预处理,然后再输入到一层全链接层的神经网络进行进一步的信道补偿与信号检测,并恢复数据流。仿真结果表明,在没有进行输入信号功率回退（IBO）时,所提方法的误比特率（BER）性能比LS算法提升2个数量级,比线性最小均方误差（LMMSE）、最小均方误差（MMSE）提升一个数量级;在进行IBO后,所提方法能避免LS信道估计下至少4 dB的功率损失,能避免LMMSE、MMSE信道估计下至少2 dB的功率损失。所提方法在一定程度上验证了机器学习结合通信的先验知识的这种新的网络结构更能提升系统数据传输的准确率。      

Recent results form measurements of the energy spectrum of cosmic-ray induced neutrons aboard an ER-2 airplane and on the ground.

Crews of future high-altitude commercial aircraft may be significantly exposed to atmospheric cosmic radiation from galactic cosmic rays (GCR). To help determine such exposures, the Atmospheric Ionizing Radiation Project, an international collaboration of 15 laboratories, made simultaneous radiation measurements with 14 instruments on a NASA ER-2 high-altitude aircraft. The primary instrument was a sensitive extended-energy multisphere neutron spectrometer, which was also used to make measurements on the ground. Its detector responses were calculated for neutrons and charged hadrons at energies up to 100 GeV using the radiation transport code MCNPX. We have now recalculated the detector responses including the effects of the airplane structure. We are also using new FLUKA calculations of GCR-induced hadron spectra in the atmosphere to correct for spectrometer counts produced by charged hadrons. Neutron spectra are unfolded from the corrected measured count rates using the MAXED code. Results for the measured cosmic-ray neutron spectrum (thermal to >10 GeV), total neutron fluence rate, and neutron dose equivalent and effective dose rates, and their dependence on altitude and geomagnetic cutoff generally agree well with results from recent calculations of GCR-induced neutron spectra.     

Measurements of high-energy neutron and proton fluxes on-board “Mir-Spectr” orbital complex

The measurements of high-energy neutron (with energies 30–300 MeV) and proton (with energies 1–200 MeV) fluxes are being conducted on-board “Mir-Spectr” orbital complex. Neutrons are detected by the undirected (FOV 4π sr) scintillator spectrometer, consisting of 4 identical CsI(Tl) detector units (the effective area for neutrons 30 cm²). The gamma-quanta, which can be also detected by this instrument, are separated from neutrons by the analysis of the scintillator output pulse shape. To exclude registration of charged particles an anticoincidence plastic scintillator shield is realized in each detector unit. The proton fluxes are measured by the telescope based on 3 semiconductor detectors with small geometry factor (1 cm²×sr). As the first result of the experiment the upper limit of the integral flux of local and albedo neutrons in the equatorial region (L<1.1) was estimated. The results of this measurements can be useful for the radiation security. Also, the neutrons of solar flares can be detected in this experiment.     

基于坐标融合的大型壳体壁厚自动测量方法研究

介绍了一种基于光栅投影测量原理的大型壳体壁厚自动化测量方法及其在大型锥形壳体产品自动测量中的应用。采用基于坐标转换统一的数据拼接方法,通过对自动测量系统的多坐标系综合标定,实现了多站位扫描测量数据的精密拼接融合。利用点云检测软件Polyworks完成了产品数模比对分析和壁厚检测,并对测量系统壁厚测量不确定度进行了分析评定。结果表明,基于坐标融合的大型壳体壁厚自动测量方法可有效提高产品的检测质量和检测效率。     

空间中子辐射及其测量技术

空间辐射环境包含大量高能带电粒子,其与航天器的结构材料相互作用会产生次级中子辐射,由于这些中子的平均品质因子是带电粒子的约4~5倍,因而对生物组织的剂量当量相对贡献更大。由于中子与物质的作用机制更为复杂,测量难度大,使得准确测量空间中子注量及其剂量当量贡献成为空间辐射剂量学中最具挑战性的工作之一。主要介绍了空间中子辐射的产生机制以及国外相关测量方法及其相关校准技术的研究状况。     

基于BP神经网络技术的电离层VTEC融合

随着电离层探测技术的不断发展,电离层观测资料也越来越多,只使用单一的观测资料会出现电离层反演精度不高的问题。为了提高电离层的反演精度,使用BP神经网络技术将地基反演和国际参考电离层(international reference ionosphere,IRI)模型的垂直总电子含量（vertical total electron content,VTEC）数据进行有效融合。在温带地区\[35°(N)~45°(N),60°(E)~80°(E)\]进行电离层反演试验,结果表明基于BP神经网络技术的电离层数据融合和地基反演获得的电离层VTEC精度都比较高,但是基于BP神经网络的电离层数据融合反演精度比地基反演更高,所以基于BP神经网络技术的数据融合能够提高电离层的反演精度。     

Comptel measurements of the omnidirectional high-energy neutron flux in near-earth orbit

On four occasions, twice in 1991 (near solar maximum) and twice in 1994 (near solar minimum), one COMPTEL D1 detector module was used as an omnidirectional detector to measure the high-energy (>12.8 MeV) neutron flux near an altitude of 450 km. The Dl modules are cylindrical, with radius 13.8 cm and depth 8 cm, and are filled with liquid scintillator (NE213A). The combined flux measurements can be fit reasonably well by a product of the Mt. Washington neutron monitor rate, a linear function in the spacecraft geocenter zenith angle, and an exponential function of the vertical geomagnetic cutoff rigidity in which the coefficient of the rigidity is a linear function of the neutron monitor rate. When pointed at the nadir, the flux is consistent with that expected from the atmospheric neutron albedo alone. When pointed at the zenith the flux is reduced by a factor of about 0.54. Thus the production of secondary neutrons in the massive (16000 kg) Compton Gamma-Ray Observatory spacecraft is negligible. Rather, the mass of the spacecraft provides shielding from the earth albedo.