固体火箭发动机燃气射流流场和声场数值计算

燃气射流噪声是固体火箭发动机工作过程中的主要噪声源之一,射流流场的参数对其产生的射流噪声有重要影响。通过大涡模拟(LES)对不同尺寸喷管形成的超声速高温射流进行了三维非稳态数值模拟,随后在合适的声源面中,采用FW-H(Ffowcs Williams-Hawkings)声学模型和傅里叶变换得到了燃气射流噪声声压级的空间分布。计算结果表明,随着喷管尺寸增大,超声速射流核心区变大,喷口流场波节数增加,对喷管尾流场的影响域扩大,其产生的射流噪声也增强;燃气射流噪声辐射有较强的指向性,在射流轴向30°角方向噪声声压级最大,与相关文献中的试验结果比较吻合。研究结果可为后续固体火箭发动机降噪设计提供参考。     

一种基于认知无线电的卫星网络信道接入策略

针对可用无线信道资源紧张与固定信道分配方式导致卫星网络信道利用率低下的问题,提出一种基于认知无线电的卫星网络信道接入策略。卫星用户以分时多址（TDMA）方式接入卫星信道,认知用户通过频谱感知发现卫星网络闲置信道资源,并以S-ALOHA方式接入信道。通过建立基于频谱感知与具有捕获效应的认知用户信道接入模型,分析认知用户最佳频谱感知时间,推导干扰信号在相干叠加与非相干叠加条件下的卫星网络吞吐率性能,并对影响网络吞吐率的因素进行仿真分析。结果表明,该信道接入策略能够在不明显降低高负载时卫星网络吞吐率的前提下有效提高低负载条件下的卫星网络吞吐率,且干扰信号相干叠加比非相干叠加对网络吞吐率性能的提升更为显著。     

大力值精密机械力源的研制

运用"平面二次包络弧面蜗杆传动"技术,研制出一种"轴向可调隙蜗轮蜗杆传动付",将它应用到力源动力传动的伺服减速机构中,驱动精密滚珠丝杠上的动横梁来完成对参考力传感器的粗加载。运用物理学中的"逆压电效应"原理,采用压电陶瓷材料和专门的工艺方法制作的力传感器微变形补偿装置——压电陶瓷力调节器,并将它应用到力源的精加载闭环控制中,实现了大载荷下参考力传感器微小力值变化的精确控制,研制出的大力值精密机械力源最大负荷为3 MN。     

软件无线电中的高速设计技术

介绍了高速电路的定义以及在高速电路设计中存在的信号完整性、时序问题,详细分析了产生这些问题的原因.分析了高速电路设计中消除反射常用的端接方式,并给出了串行端接和并行端接的仿真结果.结合实际应用,从工程实现的角度提出合理的连线拓朴结构并给出了实测结果.最后分析了高速电路设计中时序问题,给出了源同步时钟系统中时序设计应该满足的条件.      

基于DSP和FPGA的软件无线电平台研究

从硬件和软件两方面建立了基于DSP和FPGA的软件无线电平台。重点研究了该实验平台多模式数字调制解调的硬件实现结构、软件实现结构和不同模式之间的切换等,充分体现了软件无线电系统的灵活性、开放性和兼容性等特点。     

Investigation of precursory phenomena in the ionosphere,atmosphere and groundwater before large earthquakes of M > 6.5

Precursory phenomena in the ionosphere, atmosphere and groundwater before large earthquakes (M > 6.5) are extensively investigated toward the earthquake prediction. Upward tornado type seismic clouds occurred near the epicenter associated with strong LF-VLF radio noises from lightning discharges in the evening of January 9, 1995 [Yamada, T., Oike, K. On the increase of electromagnetic noises before and after the 1995 Hyogo-Ken Nanbu earthquake. In: Hayakawa M. (Ed.), Atmospheric and Ionospheric Electromagnetic Phenomena Associated with Earthquakes. TERRAPUB, Tokyo, pp. 417–427, 1999] and anomalous foEs increases up to 10 MHz were detected at Shigaraki, 90 km of the epicenter and at Kokubunji, 500 km east of the epicenter [Ondoh, T. Anomalous sporadic-E layers observed before M7.2 Hyogo-ken Nanbu earthquake; Terrestrial gas emanation model. Adv. Polar Upper Atmos. Res. 17, 96–108, 2003; Ondoh, T. Anomalous sporadic-E ionization before a great earthquake, Adv. Space Research 34, 1830–1835, 2004] associated with strong ELF noises from lightning discharges in the daytime on January 15, 1995 [Hata, M., Fujii, T., Takumi, I. EM precursor of large-scale earthquakes in Japan, in: Abstracts of International Workshop on Seismo Electromagnetics (IWSE 2005), Univ. Electro-Communications, Chofu, Tokyo, Japan, March 15–17, pp. 182–186, 2005] before the M7.2 Hyogoken–Nanbu earthquake of January 17, 1995. The anomalous foEs increases occurred at epicentral distances within 500 km that are the same as those of the terrestrial gas emanations along active faults before large earthquakes [King, C.-Y. Gas geochemistry applied to earthquake prediction: An overview. J. Geophys. Res. 91(B12), 12269–12281, 1986]. The anomalous foEs increases seem to be a seismic precursor because geomagnetic and solar conditions were very quiet all day on January 15,1995 and the normal foEs in Japanese winter is below 6 MHz. No significant pre-seismic geomagnetic field variation was detected at epicentral distance of 100 km before this earthquake [Ondoh, T., Hayakawa, M. Anomalous occurrence of sporadic-E layers before the Hyogoken–Nanbu earthquake, M7.2 of January 17, 1995. In: Hayakawa, M. (Ed.), Atmospheric and Ionospheric Electromagnetic Phenomena Associated with Earthquakes, TERRAPUB, Tokyo, pp. 629–639, 1999; Ondoh, T., Hayakawa, M. Seismo discharge model of anomalous sporadic E ionization before great earthquakes. In: Hayakawa, M., O.A. Molchanov, (Eds.), Seismo Electromagnetics: Lithosphere–Atmosphere–Ionosphere Couplings, TERRAPUB, Tokyo, pp. 385–390, 2002; Ondoh. T., Hayakawa, M. Synthetic study of precursory phenomena of the M7.2 Hyogo-ken Nanbu earthquake. Phys. Chem. Earth 31, 378–388, 2006]. The foF2 decrease and h’F increase occurred before the M7.8 Hokkaido Nansei-Oki earthquake of July 12,1993 in a geomagnetic quiet period [Ondoh, T. Ionospheric disturbances associated with great earthquake of Hokkaido southwest coast, Japan of July 12, 1993. Phys. Earth Planet. Interiors. 105, 261–269, 1998; Ondoh, T. Seismo ionospheric phenomena. Adv. Space Res. 26, 8, 1267–1272, 2000]. Characteristic phase changes at terminator times of Omega 10.2 kHz waves passing 70 km of the epicenter extended toward darker local times by 1 h for 3 days before this earthquake due to lowering of the wave reflection height or ion density increases in the D region [Hayakawa, M., Molchanov, O. A., Ondoh, T., Kawai, E. The precursory signature effect of the Kobe earthquake on VLF subionospheric signals. J. Commun. Res. La., 43, 00. 169–180, 1996]. The radon concentration in the atmosphere over Ashiya fault, Kobe [Yasuoka, Y., Shinogi, M. Anomaly in atmospheric radon concentration: a possible precursor of the 1995 Kobe, Japan, earthquake. Health Phys. 72(5), 759–761, 1997] and in the groundwater at 17 m well in Nishinomiya, Japan [Igarashi, G., Saeki, S., Takahata, N., Sumikawa, K., Tasaki, S., Sasaki, Y., Takahashi, M., Sano, Y. Ground-water radon anomaly before the Kobe earthquake in Japan. Science 269, 60–61, 1995] had gradually increased since 2 months before the M7.2 earthquake, increased suddenly in December 1994, and rapidly returned to the normal low level of October, 1994 [Yasuoka, Y., Shinogi, M. 1997. Anomaly in atmospheric radon concentration: a possible precursor of the 1995 Kobe. Japan, earthquake. Health Phys. 72(5), 759–761.]. Radon concentration changes in the groundwater before the M 7.0 Izu-Oshima-kinkai earthquake, Japan on January 14, 1978 [Wakita, H., Nakamura, Y., Notsu, K., Noguchi, M., Asada, T. 1980. Radon anomaly: a possible precursor of the 1978 Izu-Oshima-kinkai earthquake. Science 207, 882–883] and the M6.8 Chengkung earthquake, Taiwan on December 10, 2003 [Kuo, T., Fan, K., Chen, W., Kuochen, H., Han, Y., Wang, C., Chang, T., Lee, Y. Radon anomaly at the Antung Hot Spring before the Taiwan M6.8 Chengkung earthquake. Proceedings, Thirty-First Workshop on Geothermal Reservoir Engineering, Stanford University, Stanford, California, January 30–February 1, 2006, SGP-TR-179, 2006] are also investigated to find common features of the groundwater radon concentration changes before large earthquakes (M > 6.5) in comparison with those before the M7.2 Hyogoken–Nanbu earthquake. Groundwater radon concentrations before the 3 large earthquakes had shown common characteristic changes of gradually initial ones from the normal level since about 2 months before the earthquake onsets, rapid decreases down to the minimum, and quick increases up to the maximum at 7–20 days before the earthquake onsets, respectively. These are very useful characteristics of pre-seismic radon anomaly for the earthquake prediction or warning. Promising observations toward the earthquake prediction are also discussed.     

空间站大型伸展机构柔性多体动力学数值计算

对用ｋａｎｅ方法建立的空间站大型伸展机构柔性多体动力学数学模型,从数值计算方法和软件实现方面进行了研究。文章采用局部附着浮动坐标系描述各构件的刚体大范围伸展运动;用截断的子结构正则模态描述各构件的柔性变形;用求解刚性方程的ＴＲＥＡＮＯＲ方法进行数值积分;用混合法对系统的微分－代数动力学方程组进行求解。还对空间站伸展机构多体系统的约束方程建立、独立坐标选取和动力学方程的ｓｔｉｆｆ病态问题进行了讨论。并针对空间站伸展机构在驱动展开过程中以及展开完成后的动力学响应进行了算例计算。     

射电爆发显著事件与Ⅱ型爆发

本文分析了北京天文台2840MHz射电望远镜,1989年1月-1993年12月期间观测到的太阳射电爆发的显着事件与米波Ⅱ型、Ⅳ型爆发的对应关系,从相关结果来看,爆发的峰值流量越高△T越短,这说明当太阳流量越大,高达500s.f.u.以上时,Ⅱ型爆发会在爆发的峰值前后很短时间内发生,可能与粒子的加速有关。      

基于多机协作的认知无人机网络能效联合优化

针对无人机（UAV）通信网络中频谱资源紧缺的问题,构建基于认知无线电的多无人机通信网络,通过多机协作频谱感知有效探索授权频谱。提出一种基于Bisection算法的迭代算法,通过联合优化感知时间和判决门限对构建的复杂非凸问题求解,显著提高了无人机次级认知网络的能量效率（EE）。分析了无人机飞行过程中能效的变化情况,仿真结果表明,存在最优感知时间使能效获得最大值,且判决门限的选择会影响该能效最优值;提出的高能效迭代算法具有较好收敛性,有效提高了认知无人机网络的能量利用率。     

飞机座舱缝隙结构行波分析

应用可视化图形电磁计算(GRECO)技术求解高频区复杂目标面元与棱边后向散射场.对低散射截面的座舱而言,行波效应往往贡献较为显著,在某些空域内行波值甚至超过面元与棱边贡献,通过GRECO与行波混合法分析座舱目标的电磁散射特性,并给出其雷达散射截面(RCS)值.