分布式航天器相对位置测量平台设计

分布式航天器间相对位置的实时高精度测量是分布式航天器实现空间队形保持的关键技术之一。为了对相对位置测量方法进行研究、分析和论证,建立了分布式航天器相对位置测量地面实验平台。介绍了分布式航天器相对位置测量和解算的基本原理;论述了仿真平台的组成和功能;基于仿真平台对相对位置测量精度进行了仿真试验,试验结果显示该平台具有良好的性能指标;最后介绍了相对位置解算仿真评估软件的设计方法。     

Eliminating negative VTEC in global ionosphere maps using inequality-constrained least squares

Currently, ground-based Global Navigation Satellite System (GNSS) stations of the International GNSS Service (IGS) are distributed unevenly around the world. Most of them are located on the mainland, while only a small part of them are scattered on some islands in the oceans. As a consequence, many unreasonable zero values (in fact negative values) appear in Vertical Total Electron Content (VTEC) of European Space Agency (ESA) and Center for Orbit Determination in Europe (CODE) IONEX products, especially in 2008 and 2009 when the solar activities were rather quiet. To improve this situation, we directly implement non-negative physical constraints of ionosphere for global ionosphere maps (GIM) with spherical harmonic functions. Mathematically, we propose an inequality-constrained least squares method by imposing non-negative inequality constraints in the areas where negative VTEC values may occur to reconstruct GIM models. We then apply the new method to process the IGS data in 2008. The results have shown that the new algorithm efficiently eliminates the unwanted behavior of negative VTEC values, which could otherwise often be seen in the current CODE and ESA GIM products in both middle and high latitude areas of the Southern Hemisphere (45°S∼90°S) and the Northern Hemisphere (50°N∼90°N). About 64% of GPS receivers’ DCBs have been significantly improved. Finally, we compare the GIM results between with and without the inequality constraints, which has clearly shown that the GIM result with inequality constraints is significantly better than that without the inequality constraints. The inequality-constrained GIM result is also highly consistent with the final IGS products in terms of root mean squared (RMS) and mean VTEC.     

GRACE gravity field modeling with an investigation on correlation between nuisance parameters and gravity field coefficients

The GRACE (Gravity Recovery And Climate Experiment) monthly gravity models have been independently produced and published by several research institutions, such as Center for Space Research (CSR), GeoForschungsZentrum (GFZ), Jet Propulsion Laboratory (JPL), Centre National d’Etudes Spatiales (CNES) and Delft Institute of Earth Observation and Space Systems (DEOS). According to their processing standards, above institutions use the traditional variational approach except that the DEOS exploits the acceleration approach. The background force models employed are rather similar. The produced gravity field models generally agree with one another in the spatial pattern. However, there are some discrepancies in the gravity signal amplitude between solutions produced by different institutions. In particular, 10%–30% signal amplitude differences in some river basins can be observed. In this paper, we implemented a variant of the traditional variational approach and computed two sets of monthly gravity field solutions using the data from January 2005 to December 2006. The input data are K-band range-rates (KBRR) and kinematic orbits of GRACE satellites. The main difference in the production of our two types of models is how to deal with nuisance parameters. This type of parameters is necessary to absorb low-frequency errors in the data, which are mainly the aliasing and instrument errors. One way is to remove the nuisance parameters before estimating the geopotential coefficients, called NPARB approach in the paper. The other way is to estimate the nuisance parameters and geopotential coefficients simultaneously, called NPESS approach. These two types of solutions mainly differ in geopotential coefficients from degree 2 to 5. This can be explained by the fact that the nuisance parameters and the gravity field coefficients are highly correlated, particularly at low degrees. We compare these solutions with the official and published ones by means of spectral analysis. It is found that our solutions are, in general, consistent with others in the spatial pattern. The water storage variations of the Amazon, Chari and Ganges river basins have also been computed. The variations computed with the NPARB approach are closer to those produced by JPL and DEOS solutions, while the variations produced with the NPESS approach are in good agreement with those produced by the CSR and GFZ solutions. A simulation study is implemented with considering realistic noise and low-frequency error. The two approaches are used to recover the true model. The NPESS solution appears closer to the true one. Therefore we are inclined to estimate the nuisance parameters simultaneously with the geopential coefficients.     

干涉配合构件的应力腐蚀开裂特性

采用恒载荷拉伸实验技术,研究了镀锌３０ＧｒＭｎＳｉＡ锡螺栓干涉配合连接ＬＹ１２－ＣＺ铝合金构件在３．５％ＮａＣａｌ＋０．５％Ｈ２Ｏ２溶液中的应力腐蚀开裂特性。结果表明,随干涉量的增加,应力腐蚀敏感性有所下降,基材与紧固件的电偶效应对应力腐蚀繁感性有重大影响。     

Parylene真空涂覆新工艺研究

简述了Parylene真空沉积的机理,并对采用Parylene真空涂覆的涂层样件进行了全面的性能摸底试验。     

规范疲劳寿命及其标准差

从理论上严格证明了服从对数正态分布的试验寿命的样本标准差服从S分布,给出了母体标准差的无偏估计公式及纠偏系数表。给出了一定置信度下试验寿命安全标准差的计算公式及计算所必须的表格。提出了规范疲劳寿命的概念,它的标准差是试验寿命标准差的加权平均值。     

平板湍流摩阻系数的显式表达式

 湍流摩阻系数的计算是工程技术中经常遇到的问题。计算时所依据的公式多为半经验半理论的结果,如Karman公式,Van Driest公式和Prandtl公式等。这些公式是以隐函数给出的,给计算带来不便。但是不难发现,这类公式经过适当的变换,可以化为统一形式的超越代数方程,这种方程没有有限形式的解析解,本文给出了一种近似解析解。根据这种方法除了导出上述公式的显式表达式外,还对White公式作了修正。当然解超越代数方程最根本的方法是迭代法,本文对此也作了简单讨论。     

K_(Imax)<K_(Iscc)时30CrMnSiNi2A钢的腐蚀疲劳与失效机理

 应用电化学-断裂力学方法研究了30CrMnSiNi2A钢在室温模拟潮湿大气（H₂O）及海洋大气（3.5％NaCl）环境中低K范围内不同电位下的疲劳裂纹扩展特性。通过动力学及断口分析,提出在K_ImaxIscc范围内高强度钢可发生循环应力腐蚀开裂,其湿腐蚀疲劳失效机理应是裂尖局部阳极溶解与氢脆共同作用,且两者对△K_th及da/dN的意义不同,从而对以往高强度钢湿腐蚀疲劳的纯氢脆模型作出修正。     

用慢拉伸法研究GC-4超高强度钢的应力腐蚀开裂敏感性

 本文采用慢拉伸试验法研究了GC-4超高强度钢（40CrMnSiMoVA）的应力腐蚀开裂敏感性。结果表明,三种热处理的GC-4钢在典型模拟环境3％NaCl溶液和蒸馏水中都对应力腐蚀开裂敏感。环境介质的存在使该钢的抗拉强度、总应变和断裂能大大降低,而且,阴极极化和阳极极化都使其应力腐蚀开裂敏感性显著提高。分析表明,氢脆和阳极溶解都是导致GC-4钢应力腐蚀开裂的重要原因。