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1.
高压捕获翼(HCW)构型是一种满足高速飞行器高容积、高升力、高升阻比的设计需求的新型气动布局.最近研究表明,HCW构型能够提高飞行器在连续流区的升力和升阻比,缓解飞行器设计中高容积率与高升阻比间的矛盾.为探究该气动布局在过渡流域(70~100 km)的气动特性,以一种楔—平板组合的高压捕获翼原理性构型作为模型,采用直接模拟Monte Carlo(DSMC)方法,详细分析了该模型在典型高超声速条件(马赫数20)下的流场结构和壁面气动力/热分布.结果表明,随着飞行高度增加,稀薄效应增强,机体压缩产生的激波厚度增加,激波边缘逐渐模糊,机体与捕获翼之间的开放通道内出现压力干扰.同时,高压捕获翼表面的摩擦系数迅速上升,气动摩擦成为制约捕获翼构型升阻比的重要因素.针对这一问题,分析了捕获翼材料表面的适应系数对飞行器的气动力/热的影响,结果表明,降低适应系数可以显著减小壁面摩擦和热流量,可通过选用适应系数较小的表面材料进一步提高该类飞行器气动性能. 相似文献
2.
Yongliao Zou Yan Zhu Yunfei Bai Lianguo Wang Yingzhuo Jia Weihua Shen Yu Fan Yang Liu Chi Wang Aibing Zhang Guobin Yu Jihong Dong Rong Shu Zhiping He Tielong Zhang Aimin Du Mingyi Fan Jianfeng Yang Yongqing Peng 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2021,67(2):812-823
This paper describes the scientific objectives and payloads of Tianwen-1, China’s first exploration mission to Mars. An orbiter, carrying a lander and a rover, lifted-off in July 2020 for a journey to Mars where it should arrive in February 2021. A suite of 13 scientific payloads, for in-situ and remote sensing, autonomously commanded by integrated payload controllers and mounted on the orbiter and the rover will study the magnetosphere and ionosphere of Mars and the relation with the solar wind, the atmosphere, surface and subsurface of the planet, looking at the topography, composition and structure and in particular for subsurface ice. The mission will also investigate Mars climate history. It is expected that Tianwen-1 will contribute significantly to advance our scientific knowledge of Mars. 相似文献
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利用薄片金属梁作为非线性刚度元件,构建一种非线性能量阱。为了验证非线性能量阱对飞轮振动特性的抑制效果,搭建地面飞轮测试系统。分别采用力锤敲击和飞轮以恒定转速运行的方法施加不同载荷,对安装非线性能量阱前后测试系统各典型位置的振动响应进行对比研究。利用实测数据,采用傅里叶变换方法将动态响应信息分别在时间域和频率域内展开。研究表明:力锤敲击产生的冲击载荷和飞轮以恒定转速运行产生的稳态载荷均可以激发非线性能量阱定向能量传输;受非线性能量阱的影响,柔性支架设备安装面和飞轮安装面振动响应得到有效抑制。但是,由于非线性能量阱阻尼和吸振子质量较小,不同程度削弱了其振动抑制效果。 相似文献
4.
Xingyuan Yan Guanwen Huang Qin Zhang Chenchen Liu Le Wang Zhiwei Qin 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2019,63(3):1270-1279
Eight new-generation BeiDou satellites (BeiDou-3) have been launched into Medium Earth Orbit (MEO), allowing for global coverage since March 2018, and they are equipped with new hydrogen atomic clocks and updated rubidium clocks. Firstly, we analyzed the signals for the carrier-to-noise-density ratio (C/N0) and pseudorange multipath (MP) by using international GNSS (Global Navigation Satellite System) Monitoring and Assessment System (iGMAS) station data, and found that B1C has a lower C/N0, and B2a has the same level of C/N0 as the B1I and B3I signals. For pseudorange multipath, compared with the BeiDou-2 satellites, the obvious systematic variation of MP scatters related to the elevation angle is greatly improved for the BeiDou-3 and BeiDou-3e satellites signals. For the signals of the BeiDou-3 satellites, the order of the Root Mean Square (RMS) values of multipath and noise is B3I?<?B1I?<?B2a?<?B1C. Then, the comparison of the precise orbit determination and clock offset determination for the BeiDou-2, BeiDou-3, and BeiDou-3 experimental (BeiDou-3e) satellites was done by using 10 stations from iGMAS. The 3D precision of the 24?h orbit overlap is 24.55, 25.61, and 23.35?cm for the BeiDou-3, BeiDou-3e, and BeiDou-2 satellites, respectively. BeiDou-3 satellite has a comparable precision to that of the BeiDou-2 satellite. For the precision of clock offset estimation, the Standard Deviation (STD) of the BeiDou-3 MEO satellite is 0.350?ns, which is an improvement of 0.042?ns over that of the BeiDou-2 MEO satellite. The stabilities of the BeiDou-3 and BeiDou-3e onboard clocks are better than those of BeiDou-2 by factors of 2.84 and 1.61 at an averaging time of 1000 and 10,000?s, respectively. 相似文献
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6.
Jia Luo Fangfang Sun Xiaohua Xu Han Wang 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2019,63(1):327-336
In this paper, we compared the F2-Layer critical frequency (foF2) derived from FORMOSAT-3/COSMIC radio occultation (RO) and ionosondes at Chiang Mai, Chumphon and Kototabang during the years 2008–2015 to evaluate the performance of COSMIC RO over Southeast Asia region. The results show that the time development of foF2 values derived from COSMIC RO generally agrees well with those from ionosonde measurements. However, the differences between the foF2 derived from COSMIC RO and that derived from ionosonde observations display latitudinal dependence. COSMIC RO tends to underestimate foF2 at Chiang Mai and Kototabang, which is near to the north EIA crest and the south one, respectively, while a little overestimate foF2 at Chumphon, which is close to the geomagnetic equator. COSMIC RO agrees best with ionosonde at Chumphon and worst at Chiang Mai. At each ionosonde station, the quality of COSMIC RO data degrades with the increase of solar activity. In addition, at the station Chiang Mai and Kototabang, COSMIC RO performs better in summer than in equinox and winter. Furthermore, the differences in foF2 derived from COSMIC RO and that from ionosonde measurements vary with local time, i.e., the differences in foF2 are generally smaller at night and larger in noontime when equatorial ionization anomaly (EIA) is well developed. 相似文献
7.
Mukul Kumar Wang Chi 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2019,63(1):640-652
We study the Propagation and damping properties of Alfvén gravity waves in the presence of the vertical magnetic field in the viscous solar plasma under influence of the background flow by deriving a fourth order dispersion relation in terms of the Doppler shifted frequency. We derive the dispersion relation under WKB and Boussinesq approximation. We study the damping of Alfvén gravity waves for the wave frequencies less than and greater than the Brunt-Väisälä frequency. We find that the Brunt-Väisälä frequency divides the frequency ranges where the weakly or strongly damped oscillations occur. The background flow exhibits a strong effect on weakly damped oscillations and a weak effect on the strongly damped oscillations. We also notice that the damping of both the strong and weakly damped oscillations depend on the Brunt-Väisälä frequency and wave number. The effect of the background flow is also being governed by the Brunt-Väisälä frequency and wave number. We also study the properties of gravity wave mode after filtering the Alfvén wave mode by minimizing the magnetic field and noticed that the background flow shows a very strong effect on the gravity wave mode. 相似文献
8.
针对连续推力的合作航天器,采用双重无迹卡尔曼滤波(DUKF)算法估计其状态和加速度。通过状态滤波器和参数滤波器的配合,提升滤波精度,完成运动状态和参数的估计,从而实现合作目标的运动轨迹跟踪。与合作航天器相比,非合作航天器存在大小未知、发生时刻未知的机动,无法获得加速度,且信息获取和运动状态的估计难度大。针对非合作航天器,基于简化的相对运动方程,结合天基平台获得目标的观测信息,采用两个扩展卡尔曼滤波(EKF)及基于半正焦弦的机动检测策略实现多未知脉冲机动的运动状态的估计。仿真结果表明:相比于无迹卡尔曼滤波(UKF),DUKF在对合作航天器的状态和加速度估计方面具有更快的收敛速度和更高的滤波精度;对于存在未知机动的非合作航天器,通过对比验证机动检测策略与滤波器切换策略相结合的方法的有效性,该方法能够检测到多次机动并且减少误判。 相似文献
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