Special Technologies Related to Electron Beam Welding

In order to improve the manufacturing quality of electron beam welding,some technologies are developed by using the special features of electron beam.Comparing with the conventional electron beam welding,the usage of multi-beam technology and micro-beam technology are introduced.In addition.the development of beam diagnostic system is also presented.     

Differential code bias estimation based on uncombined PPP with LEO onboard GPS observations

Differential Code Bias (DCB) is an essential correction that must be provided to the Global Navigation Satellite System (GNSS) users for precise position determination. With the continuous deployment of Low Earth Orbit (LEO) satellites, DCB estimation using observations from GNSS receivers onboard the LEO satellites is drawing increasing interests in order to meet the growing demands on high-quality DCB products from LEO-based applications, such as LEO-based GNSS signal augmentation and space weather research. Previous studies on LEO-based DCB estimation are usually using the geometry-free combination of GNSS observations, and it may suffer from significant leveling errors due to non-zero mean of multipath errors and short-term variations of receiver code and phase biases. In this study, we utilize the uncombined Precise Point Positioning (PPP) model for LEO DCB estimation. The models for uncombined PPP-based LEO DCB estimation are presented and GPS observations acquired from receivers onboard three identical Swarm satellites from February 1 to 28, 2019 are used for the validation. The results show that the average Root Mean Square errors (RMS) of the GPS satellite DCBs estimated with onboard data from each of the three Swarm satellites using the uncombined PPP model are less than 0.18 ns when compared to the GPS satellite DCBs obtained from IGS final daily Global Ionospheric Map (GIM) products. Meanwhile, the corresponding average RMS of GPS satellite DCBs estimated with the conventional geometry-free model are 0.290, 0.210, 0.281 ns, respectively, which are significantly larger than those obtained with the uncombined PPP model. It is also noted that the estimated GPS satellite DCBs by Swarm A and C satellites are highly correlated, likely attributed to their similar orbit type and space environment. On the other hand, the Swarm receiver DCBs estimated with uncombined PPP model, with Standard Deviation (STD) of 0.065, 0.037 and 0.071 ns, are more stable than those obtained from the official Swarm Level 2 products with corresponding STD values of 0.115, 0.101, and 0.109 ns, respectively. The above indicates that high-quality DCB products can be estimated based on uncombined PPP with LEO onboard observations.     

First results of operational ionospheric dynamics prediction for the Brazilian Space Weather program

It is shown the development and preliminary results of operational ionosphere dynamics prediction system for the Brazilian Space Weather program. The system is based on the Sheffield University Plasmasphere–Ionosphere Model (SUPIM), a physics-based model computer code describing the distribution of ionization within the Earth mid to equatorial latitude ionosphere and plasmasphere, during geomagnetically quiet periods. The model outputs are given in a 2-dimensional plane aligned with Earth magnetic field lines, with fixed magnetic longitude coordinate. The code was adapted to provide the output in geographical coordinates. It was made referring to the Earth’s magnetic field as an eccentric dipole, using the approximation based on International Geomagnetic Reference Field (IGRF-11). During the system operation, several simulation runs are performed at different longitudes. The original code would not be able to run all simulations serially in reasonable time. So, a parallel version for the code was developed for enhancing the performance. After preliminary tests, it was frequently observed code instability, when negative ion temperatures or concentrations prevented the code from continuing its processing. After a detailed analysis, it was verified that most of these problems occurred due to concentration estimation of simulation points located at high altitudes, typically over 4000 km of altitude. In order to force convergence, an artificial exponential decay for ion–neutral collisional frequency was used above mentioned altitudes. This approach shown no significant difference from original code output, but improved substantially the code stability. In order to make operational system even more stable, the initial altitude and initial ion concentration values used on exponential decay equation are changed when convergence is not achieved, within pre-defined values. When all code runs end, the longitude of every point is then compared with its original reference station longitude, and differences are compensated by changing the simulation point time slot, in a temporal adjustment optimization. Then, an approximate neighbor searching technique was developed to obtain the ion concentration values in a regularly spaced grid, using inverse distance weighting (IDW) interpolation. A 3D grid containing ion and electron concentrations is generated for every hour of simulated day. Its spatial resolution is 1° of latitude per 1° of longitude per 10 km of altitude. The vertical total electron content (VTEC) is calculated from the grid, and plotted in a geographic map. An important feature that was implemented in the system is the capacity of combining observational data and simulation outputs to obtain more appropriate initial conditions to the ionosphere prediction. Newtonian relaxation method was used for this data assimilation process, where ionosonde data from four different locations in South America was used to improve the system accuracy. The whole process runs every day and predicts the VTEC values for South America region with almost 24 h ahead.     

Ni18%和0Cr15Ni5Cu2Ti异种钢材电子束焊接工艺试验研究

对Ni18%和0Cr15Ni5Cu2Ti超高强度马氏体沉淀硬化不锈钢异种钢材之间进行了电子束焊接工艺试验,就其工艺可焊性及接头性能、金相组织、焊缝质量、力学性能等开展研究,采用X-探伤、静载强度、金相观察、电镜扫描和能谱分析等检测手段对试件进行了分析并得出了相应结论。     

The role of volcanic aerosols and relativistic electrons in modulating winter storm vorticity

Small changes in the vorticity of winter storms, responding to solar wind variations, are found in winters from 1957 to 2011, and are greater for winters with higher levels of stratospheric volcanic aerosols. Using 1993–2011 data, the response of the vorticity area index (VAI) is shown to be of larger amplitude when the days of minima in the relativistic electron flux (REF) precipitating from the radiation belts are used, instead of heliospheric current sheet (HCS) crossings, as key days in superposed epoch analyses. The HCS crossings mostly occur within a few days of the REF minima. The VAI is an objective measure of the area of high cyclonic vorticity, and for the present work is derived from ERA-40 and ERA-Interim reanalyses of global meteorological data. The VAI dependencies on the stratospheric aerosol content (SAC) and the REF are consistent with a model in which the ionosphere-earth current density (J_z) affects cloud microphysics. One of the ways in which J_z is modulated is by changes in stratospheric column resistance (S), which is increased by stratospheric aerosols. Because S is in series with the tropospheric column resistance (T), J_z modulation by REF requires that S be not negligible with respect to T. So the J_z modulation and the VAI response appear when the SAC is very high, or the REF reductions (which also increase S) are very deep, and when the product of the SAC and the reciprocal of the REF exceeds a threshold value dependent on T.     

双栅极空气计数器系统参数优化设计方法

 基于金属材料微裂纹检测传感器系统放电脉冲的形成过程, 建立了离散化放电的数学模型, 提出了传感器系统参数优化设计的一种新方法。实验结果表明, 采用该理论设计的传感器系统参数, 避免了经验公式设计的片面性, 保证了传感器系统无损检测的可靠性和精确性。     

不同磁暴条件下GEO卫星表面充电电位分布

文章利用1989-2004年间"Los Alamos"7 颗地球同步轨道卫星的数据对不同磁暴条件下处于地球同步轨道高度等离子体片区域的卫星表面充电电位和热电子(0.03~45 keV)温度随地方时的分布及随磁暴发生时间的变化规律进行统计分析.根据对磁层顶电流修正后的Dst指数(Dst*)将磁暴分成弱磁暴、强磁暴以及超大磁暴.在随地方时的分布上,弱磁暴时卫星最可能在午夜后侧负向强充电(＞800 V);随着磁暴强度的增加,在超大磁暴情况下该区域会沿东西方向扩展到夜晚21时到凌晨4时的区域.在随磁暴发生时间的分布上,弱磁暴下卫星表面充电到高负电位主要发生在Dst*最低点前3 h和后2 h的时刻,强磁暴下主要发生在Dst*最低点时刻,而超大磁暴下主要发生在恢复相,持续时间达十几个小时.表面电位的分布规律和热电子温度的分布规律表现一致:卫星表面负电位超过100 V的区域主要集中在热电子温度大于2 keV的区域,而表面负电位最可能超过800 V的区域主要集中在热电子温度大于2.5 keV的区域.通过统计分析看出,对于那些极可能发生高负电位充电(＞8 kV)情况下的卫星表面电位分布与磁暴的强弱并无明显的相关性,但发现在弱磁暴情况下明显集中在正午前侧区域.     

高超声速钝体尾流的积分电子密度与尺寸度律

本文提出了一个高超声速非烧蚀钝体化学非平衡尾流流场的简化模型和简化的空气化学模型。应用该模型计算尾流的积分电子密度。计算结果与实验数据符合得很好。在此基础上,以P_∞D_N=375mmHg·mm为例,初步论证了尾流双尺度律的适用程度与范围,为弹道靶模型实验提供正确的导向。     

太阳同步轨道电子探测器的多方向设计研究

为实现观测电子投掷角分布的目标,本文讨论了太阳同步轨道三轴稳定卫星电子观测的多方向设计。分析了磁层电子投掷角分布特征,并根据太阳同步轨道卫星的轨道参数,计算得到卫星运行轨迹上,三个探测器常用安装面正入射粒子的投掷角。在此基础上,进行电子探测器的探测方向设计,结果表明探测器要在任何安装面都满足投掷角观测要求,至少需要在0°、10°、20°、25°、35°、45°、70°、80°和90°共9个方向上设计探测窗口。     

空间次生环境研究及探测方法概述

文章基于空间次生环境及其效应定义,分别结合不同次生环境阐述了国内外在磁场作用下带电粒子对航天器的影响、航天器非金属材料出气的影响、航天器与空间等离子体相互作用影响、航天器发动机羽流效应和航天器舱内电子环境及效应等的研究状况,并有针对性地开展了典型的发动机羽流效应、放电监测系统和航天器自身磁场分布探测研究。