三自由度球形电机位置测量研究

非接触位移测量对实现球电机的闭环运动控制十分重要.对基于微处理器的光学传感器的测量原理作了分析,阐述了利用二自由度光学传感器测量球电机三自由度位移的测量原理,提出了传感器的安装和位移计算方法.这种方法是通过球面的几何关系,由检测到的x和y坐标方向的位置数据计算出z坐标方向的数据,并根据旋量理论建立球电机运动的旋转矩阵和计算出旋转矩阵的旋转角度.通过仿真结果验证了所提方案的实用性.     

地磁测量卫星的矢量磁场在轨标定算法仿真

以SWARM为代表的高精度地磁测量卫星对地球磁场探测精度经过标定之后优于0.5 nT,对于开展地磁科学研究具有重要意义。地磁测量卫星通过安装在伸展杆上的矢量磁通门磁强计、标量磁强计和高精度星敏感器,获取测量方向的惯性空间姿态的地磁信息,其中高精度标量磁强计主要用于对磁通门矢量磁强计进行标定。针对地磁测量卫星,研究了矢量磁强计在轨测量误差的校正方法。考虑到矢量磁强计非正交角、标度因子以及偏差的影响,建立磁场矢量线性输出模型;结合标量磁强计的测量值分别设计基于小量近似的线性校正算法和基于参数辨识更新的非线性校正算法;校验两种算法的标定精度,并通过Tukey权重函数改善算法的鲁棒性。仿真结果表明,两种算法校正结果相似,磁场三轴误差可校正至0.5 nT以内,在标量磁强计存在异常值时仍具有较好的校正效果。      

关于双曲型偏微分方程u_xy=f(X,y,u)的唯一性

本文给出双曲型偏微分方程的特征边值问题 u_xy=f(x,y,u), u(x,O)=σ(x), O≤x≤a, u(O,y)=T(y), O≤y≤b, 在R=[O,a]×[O,b]上的解u=u(x,y)的唯一性定理。     

非晶态Co-T-Zr(T=Cr,Mo,V,W)合金作为磁强计磁芯材料的研究

以快淬法制备了非晶态Co_(90～x)T_xZr_(10)(T=Cr,Mo,V,W;x=0,4,6,8,10,12)合金系列样品,并对其一些热和磁性能进行了测试研究,探讨了它们在磁强计上应用的可能性。结果表明,随着样品中T元素含量的增加,样品的晶化温度和晶化激活能升高,饱和磁化强度和居里温度下降,交流磁导率变化不大。退火处理对交流磁导率和损耗有较大影响。以现有理论对实验结果进行了分析。非晶态Co_(78)Cr_(12)Zr_(10)合金适于用作磁强计探头的磁芯材料,尤其是它良好的高频性能使磁强计测量的交流磁场的截止频率大干20kHz。     

某种新型磁强计在星载部件测试中的应用研究

介绍了一种新型的磁强计，该磁强计用具有零磁滞伸缩系数的非晶态合金薄带作为探头铁心，多谐振荡回路作为磁强计电路。它具有结构简单，操作方便，频率响应范围大（０～５ｋＨｚ）等优点。给出了该磁强计的工作原理，并对其在星载部件测试中的应用进行了探索。     

罐车制动时液体晃动的仿真分析

采用Volume of Fluid (VOF) 模型对罐车制动时液体的晃动进行了数值模拟,对单室受力、受力位置及整车轴荷分配进行了计算,并通过与实验结果的对比验证了计算方法的可靠性.计算结果表明,无防波板时,随减速度增加,单室 x,y方向受力峰值增大,整车轴荷比增大;随充液比增加,单室x方向受力峰值先增大后减小,y 方向受力峰值增大,制动初始与结束时充液比越大轴荷比越大,1s左右充液比越大轴荷比越小;单室带防波板时,随防波板面积增加, x,y 方向受力峰值减小,当防波板面积大于横截面的40%时,增加防波板面积能显著改善罐体受力,且防波板面积越大轴荷比峰值越小.     

激光泵浦铯-氦磁强计的噪声抑制

介绍了一种利用单模激光进行泵浦的铯-氦磁强计。由于单模激光比铯元素放电灯具有更高的泵浦效率，这种铯-氦磁强计得到了比传统的放电灯铯-氦磁强计更强的磁共振信号。通过测量各试验因素中引入的磁噪声，发现激光的光功率涨落是目前磁噪声的主要来源；通过分析信噪比与光强的关系，得到了最优化的光强；通过主动光强降噪技术，在最佳试验条件下，铯-氦磁强计的噪声峰峰值可以优于0.02 nT。结果表明，通过提升激光功率的稳定性，激光泵浦式的铯-氦磁强计非常有潜力得到比质子磁强计更高的准确度，可作为恒定弱磁场计量标准的新一代主标准器。     

考虑支承刚性时转子的临界转速

提出用折合效应系数法计算考虑支点刚性及陀螺力矩影响时转子临界转速的方法,用以计算两支点刚性不同而周向刚性相同转子的临界转速。分析了支点刚性系数对临界转速性质的影响,得出一些结论,可供设计参考。拟制两支点刚性不同,周向刚性不均匀转子的临界转速计算方法及两支点刚性不同,周向刚性不均,且y(z)方向负荷会造成z(y)向变形情况下转子的临界转速计算方法。所有计算方法中考虑了陀螺力矩的影响,这就比目前已有的计算方法更接近实际。由性质分析所导出的一些概念,对实际设计机器时,如何考虑支点刚性对临界转速影响有参考作用。 学生陈宝歧、于香泉,在完成这项科研项目中付出许多劳动,在此表示衷心感谢。     

BERNOULLI方程的推广

本文讨论了微分方程 dy/dx+P_1(x)P_2(y)=Q_1(x)Q_2(y)在P_1(x),P_2(y),Q_1(x),Q_2(y)满足什么条件下可化为可积类型;并得出了Bernoulli方程仅仅是此种方程的一个特例;从而使一类一阶微分方程能较方便的用初等解法化为求积分问题。     

“阿里安”运载火箭准备采用激光陀螺

为了进一步提高制导精度和弹道修正精度,欧洲准备在“阿里安”运载火箭最后变型部件上采用激光陀螺。这种激光陀螺将首次安装在阿里安-4系列上,能将角度与速度信息传给火箭上的计     

Research on the Relation Between the Seeker's Handover and the Geometrical Position of the Missile and the Target

 研究了雷达导引头的交班误差以及截获概率与交班时刻弹目几何位置的关系,提出了单个误差角的导引头天线指向角误差模型,它与两个误差角的导引头指向角误差模型相比可以更好地分析天线指向角误差,并得到使指向角误差最小的弹目几何位置;然后进一步得到使多普勒频率误差最小的弹目几何位置;给出了最终的截获概率的表达式,截获概率由目标处于导引头天线主波束的概率、目标回波多普勒频率落入接收机频带内的概率和目标的检测概率组成的;最后分析了一种典型的中末交班情况.     

Comparison of the magnetic field before the subsolar magnetopause with the magnetic field in the solar wind before the bow shock

Crossings of the magnetopause near the subsolar point are analyzed using data of THEMIS mission. Variations of the magnetic field near magnetopause measured by one of THEMIS satellites are studied and compared with simultaneous measurements in the solar wind by another THEMIS satellite. The time delay of the solar wind arrival at the subsolar point of the magnetopause is taken into account. 30 and 90 s averaging of the magnetic field in the magnetosheath is produced. The results of averaging are compared with the results of measurements in the solar wind before the bow shock and foreshock. It is shown, that _Bx$B_x$ component of the magnetic field near magnetopause is near to zero, which supports the possibility to consider the magnetopause as the tangential discontinuity. Comparatively good correlation of _By$B_y$ component in the solar wind and near the magnetopause is observed. The correlation of _Bz$B_z$ component near the magnetopause and IMF is practically absent, the sign of the _Bz$B_z$ near the subsolar point does not coincide with the sign of IMF _Bz$B_z$ in ∼$\sim$30% cases.     

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.     

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.     

On the correlation of the solar wind observed at the L5 point and at the Earth

The L5 point is a promising location for forecasting co-rotating high-speed streams in the solar wind arriving at the Earth. We correlated the solar wind data obtained by the Nozomi spacecraft in interplanetary space and by the Advanced Composition Explorer (ACE) at the L1 point, and found that the correlation is significantly improved from that of the 27-day recurrence of ACE data. Based on the correlation between the two spacecraft observations, we estimated the correlation of the solar wind velocity between the L5 point and at the Earth, and found that the correlation coefficient was about 0.78 in late 1999, while that of the 27-day recurrence was 0.51. Eighty-eight percent of the velocity difference falls within 100 km/s between the L5 point and the Earth. This demonstrates the potential capability of solar wind monitoring at the L5 point to forecast the geomagnetic disturbances 4.5 days in advance.     

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.     

太阳风——磁层相互作用的磁流体力学数值模拟研究

磁层位于地球空间的最外层, 太阳风与磁层的相互作用是空间天气变化因果链中承上启下的关键环节, 是揭示地球空间天气基本规律的关键科学课题. 地球空间由于时变、多成分、多自由度的关联相互作用,使得传统的理论分析变得非常困难. 数值模拟作为近几十年发展起来的一个新的研究手段,对地球空间的理论和应用研究产生了深刻的影响. 国际上磁层的全球MHD数值模拟工作开始于20世纪70年代末, 最初的研究局限于二维空间. 由于磁层内在的三维特性, 20世纪80年代三维MHD数值模拟工作兴起. 本文简要说明了三维全球磁层MHD (磁流体力学)研究的特点及现状, 给出了三维全球磁层模型的基本框架, 综述了行星际激波与磁层相互作用、大尺度电流体系、重联电压和越极电位、磁层顶K-H不稳定性等方面的太阳风--磁层相互作用的MHD数值模拟的研究进展.      

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.      

辐射变色薄膜剂量计性能测试及加速器应用

本课题的目的是建立用于辐射加工高剂量水平吸收剂量测量的辐射变色薄膜剂量计。通过系统研究,批量制备了以尼龙为基材,副品红氰化物为染料的辐射变色薄膜剂量计。为了验证批制辐射变色薄膜剂量测量的可靠性,选择了国际上应用较广的FWT-60膜及丙氨酸薄膜剂量计与本实验室批制的辐射变色薄膜开展实验室内剂量比对,比对结果均在±4%内符合,归一化偏差En绝对值均小于1。通过在加速器上进一步应用实验表明批制辐射变色薄膜可用于电子束辐照参数测量。     

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.