一种新型固体推进剂比冲标准物质

介绍一种新型的比冲标准物质BC-1,同SQ-2标准物质相比,对配方进行了改进,其燃烧性能和燃烧稳定性均优于SQ-2。通过对配方中燃烧催化系统的改进,研制出了一种新型的比冲标准物质BC-1,克服了SQ-2标准物质的燃烧不稳定性,且具有优良的燃烧特性,在6MPa~12 MPa压力范围内的压强指数由0.60降至-0.03。     

岁差章动模型更新等因素对坐标转换的影响

GCRS(Geocentric Celestial Reference System,地心天球参考系)与ITRS(International Terrestrial Reference System,国际地球参考系)之间的坐标转换方法与岁差章动模型密切相关,IERS(International Earth Rotation and reference systems Service,国际地球自转与参考系服务)规范先后推荐了3组不同的岁差章动模型。论文分析了基于春分点的坐标转换过程,在比较3组岁差章动模型间差异的基础上,以太阳系10个天体为例,计算了岁差章动模型更新、极移、世界时与地球时差值等因素对坐标转换影响的具体数值。结果表明,IAU 2006岁差-IAU 2000AR06章动与IAU 2000岁差-IAU 2000A章动间的差异,对坐标转换的影响在0.5mas以内;而IAU1976岁差-IERS 1996章动与前2组岁差章动间的差异,对坐标转换影响的最大值达到37mas;极移对坐标转换影响的最大值达到0.6″,远高于岁差章动模型更新所带来的影响;当忽略世界时与地球时的差异时,结果完全错误。通过此分析,明确了极移、世界时与地球时的差异对坐标转换影响的具体数值,可为工程计算中岁差章动模型的选取提供参考依据。     

失真信号的合成

总结了波叠加的方法，指出了基准坐标系的重要性与有关量的求解方法。     

空间计量与脉冲星导航

以脉冲星导航技术为背景,讨论了空间计量理论中时间测量的关键问题。首先介绍了脉冲星导航的基本原理,和不同坐标系之间的时间尺度转换,比较了不同坐标系时间轴度规对脉冲星的脉冲轮廓测量的影响,说明只有太阳系质心坐标时能够正确测量脉冲轮廓。进而介绍了空间计量提出的两种时间统一的模式:地球卫星导航模式和脉冲星导航模式。以脉冲星导航为例,讨论了基于SI秒绝对定义和太阳系质心坐标时的广域时间统一的方法,给出用航天器原时坐标轴伸缩法修正多普勒效应的公式。最后提出在大尺度广域时空中构建新的守时系统—太阳系质心守时系统的设计思路。     

Comparative study of foF2 measurements with IRI-2007 model predictions during extended solar minimum

The unusually deep and extended solar minimum of cycle 23/24 made it very difficult to predict the solar indices 1 or 2 years into the future. Most of the predictions were proven wrong by the actual observed indices. IRI gets its solar, magnetic, and ionospheric indices from an indices file that is updated twice a year. In recent years, due to the unusual solar minimum, predictions had to be corrected downward with every new indices update. In this paper we analyse how much the uncertainties in the predictability of solar activity indices affect the IRI outcome and how the IRI values calculated with predicted and observed indices compared to the actual measurements. Monthly median values of F2 layer critical frequency (foF2) derived from the ionosonde measurements at the mid-latitude ionospheric station Juliusruh were compared with the International Reference Ionosphere (IRI-2007) model predictions. The analysis found that IRI provides reliable results that compare well with actual measurements, when the definite (observed and adjusted) indices of solar activity are used, while IRI values based on earlier predictions of these indices noticeably overestimated the measurements during the solar minimum. One of the principal objectives of this paper is to direct attention of IRI users to update their solar activity indices files regularly. Use of an older index file can lead to serious IRI overestimations of F-region electron density during the recent extended solar minimum.     

一种新型RLV再入轨迹在线规划方法

针对可重复使用运载器(Reusable Launch Vehicle, RLV)再入轨迹在线规划问题,提出了一种基于割线法的标准轨迹快速生成方法。该方法以驻点热流、法向过载、动压和平衡滑翔限制为再入过程约束,以再入初始点和结束点的高度、速度为再入端点约束;在阻力加速度-速度平面内建立约束模型后,设计了折线形式的标准轨迹;采用割线法迭代计算轨迹转折点以调整轨迹形状,使最终规划轨迹对应的航程和终端点速度同时满足设计需求。最后取3种不同航程的再入情况进行了数值仿真。仿真结果表明,所提出的方法能够在1秒内完成再入轨迹规划,并在一定航程范围内适用,能够满足在线设计标准再入轨迹的实时要求。     

Impact of loading effects on determination of the International Terrestrial Reference Frame

The International Terrestrial Reference Frame (ITRF), as a realization of the International Terrestrial Reference System (ITRS), is represented by a set of station positions and linear velocities. They are intended to be used as regularized coordinates to which some corrections should be added to access instantaneous coordinates. The latest ITRS realization is the ITRF2005, which has integrated time series of station positions to form long-term solutions for the four space geodetic techniques. Currently, a purely linear model is used to parameterize station displacements in the estimation process, plus occasional discontinuities in case of earthquakes or equipment changes. However the input data have been derived without applying surface loading models and so surface loading effects are supposed to be embedded in the coordinates as measured quantities. We evaluate the effect of applying a posteriori loading corrections, which include the effect of atmospheric, non-tidal ocean, and continental water loading, to time series of positions estimated from Satellite Laser Ranging (SLR), Very Long Baseline Interferometry (VLBI), and Global Positioning System (GPS) data. We notice that they reduce about 50% or more of the annual signals in the translation and scale parameter time series of the SLR and VLBI techniques, except in SLR Z translation. In general, the estimated secular frame definition is negligibly affected and estimated positions and velocities are not significantly modified for stations that have accumulated a large number of observations. A multi-technique combination of such derived frames allows concluding that, for some cases, loading model corrections might degrade co-located station coordinates almost as much as they benefit them. However, most significant improvement of the estimated secular coordinates is observed for stations with less than 100 estimated positions as demonstrated with a multi-technique combination.     

F-region ionospheric parameters observed in the equatorial and low latitude regions during medium solar activity in the Brazilian sector and comparison with the IRI-2007 model results

The ionospheric sounding observations using the Canadian Advanced Digital Ionosondes (CADIs) operational at Palmas (PAL; 10.2°S, 48.2°W; dip latitude 6.6°S; a near-equatorial station), and São José dos Campos (SJC, 23.2°S, 45.9°W; dip latitude 17.6°S; a low-latitude station located under the southern crest of the equatorial ionospheric anomaly), Brazil, are analyzed during the different seasons viz., winter (June and July 2003), spring (September and October 2003), summer (December 2003 and January 2004), and fall (March and April 2004). The period used has medium solar activity (sunspot number between 77.4 and 39.3). The seasonal mean variations (using only geomagnetically quiet days) of the ionospheric parameters foF2 (critical frequency of the F-region), hpF2 (virtual height at 0.834 foF2; considered to be close to hmF2 (peak height of the F-region)), and h’F (minimum virtual height of the F-region) are calculated and compared between PAL and SJC. The prominent differences between PAL and SJC are as follows: h’F variations show strong post-sunset enhancement at PAL during the seasons of spring, summer, and fall; hpF2 variations show pre-sunrise uplifting of the F-layer at both stations during all the seasons and the hpF2 values during the daytime are lower at SJC compared with PAL during all the seasons; the foF2 variations show mid-day bite-out at PAL during all the seasons and SJC shows strong equatorial ionospheric anomaly during summer and fall seasons. Also, the seasonal variations of the ionospheric parameters foF2 and hpF2 (with ±1 standard deviation) observed at PAL and SJC are compared with the IRI-2007 model results of foF2 and hmF2. In addition, variations of the foF2 and hpF2 observed at SJC are compared with the IRI-2001 model results of foF2 and hmF2. It should be pointed out that the ionospheric parameter hpF2 is much easier to obtain using computer program developed at UNIVAP compared with hmF2 (using POLAN program). During the daytime due to underlying ionization hpF2 estimated is higher (approximately 50 km) than the true peak height hmF2. During the nighttime hpF2 is fairly close to hmF2. The comparison between the foF2 variations observed at PAL and SJC with the IRI-2007 model results shows a fairly good agreement during all the seasons. However, the comparison between the hpF2 variations observed at PAL and SJC with the hmF2 variations with the IRI-2007 model results shows: (1) a fairly good agreement during the nighttime in all the seasons; (2) the model results do not show the pre-sunrise uplifting of the F-layer at PAL and SJC in any season; (3) the model results do not show the post-sunset uplifting of the F-layer at PAL; (4) considering that, in general, hpF2 is higher than hmF2 during the daytime by about 50 km, the model results are in good agreement at PAL and SJC during all the seasons except summer at SJC, when large discrepancies in the observed hpF2 and modeled hmF2 are observed. Also, it has been observed that, in general, hmF2 values for SJC calculated using IRI-2001 are higher than IRI-2007 during the daytime in winter, summer, and fall. However, hmF2 values for SJC calculated using IRI-2001, are lower than IRI-2007 during the nighttime in spring.     

便携式γ射线照射装置散射辐射特性研究

便携式γ射线照射装置对于提高固定式X、γ辐射剂量仪检定率、解决现场校准难题具有重要意义,利用蒙特卡罗模拟与实验测量协同开展便携式γ射线照射装置散射辐射特性研究。结果表明：蒙特卡罗方法可以模拟得到装置自身的散射辐射,实验测量只能获得照射装置以外辐射场中的散射辐射。利用MCNP程序F4卡和CF卡得到距放射源1 m处照射装置自身的散射贡献分别为13.07 %和4.55 %;反平方律实验和移出实验得到辐射场散射辐射贡献分别为0.2 %和3.94 %,满足ISO 4037-1:2019和GB/T 12162.1-2000的要求。该装置可用于固定式X、γ辐射剂量仪的现场校准。     

地心非旋转坐标系中的卫星双向时间比对计算模型

根据卫星双向时间频率传递 (TWSTFT)的基本原理 ,详细推导了地心非旋转坐标系中TWSTFT的计算模型 ,并与地固系中的计算模型进行了分析比较 ,证明了两种计算模型在亚纳秒量级上的等价性。