阳极氧化TiO2膜对甲基橙溶液的光催化性能研究

本试验利用阳极氧化的方法在纯钛基体上直接获得锐钛相T iO2多孔膜,解决T iO2光催化剂的涂敷固定问题。用场发射扫描电镜(F ie ld em iss ion scann ing e lectron m icroscope,FESEM)和X射线衍射仪(X-ray d iffractionm eter,XRD)对纯钛表面生成的T iO2多孔膜的形貌和晶体结构进行分析。以10m g/L甲基橙溶液为降解物进行光催化试验,分别研究了阳极氧化电压、溶液的初始pH值、T iO2膜的面积、T iO2膜的使用次数对降解率的影响。试验结果表明,当溶液初始pH值为1时,140V阳极氧化所得T iO2膜的光催化性能最好,同时随着T iO2膜使用次数的增加,但其光催化效果有所下降。     

从日地系统L2出发借力月球飞越近地小行星

对于停留在日地系统L2的“嫦娥2号”探测器,其后续飞行方案有多个选项,例如主动撞月或重返月球轨道、返回地球轨道或再入大气、飞往地月系统L1/L2或日地系统L1、进入深空飞越近地小行星(最终,“嫦娥2号”于2012年12月13日成功地实现了对Toutatis小行星的近距离飞越)。探讨上述的飞行方案需要对飞行轨道进行初步设计,总的速度脉冲限制在100 m/s以内并且需要考虑探测器同时受到太阳、地球、月球的引力作用。本研究设计了探测器从日地系统L2出发借力月球实现Toutatis小行星飞越的飞行方案,与直接飞越方案相比,借力月球可以进一步节省探测器的燃料消耗,其等效速度脉冲设计值为58.47 m/s。     

一种基于频移补偿的apFFT相位估计改进方法及应用

全相位快速傅里叶变换（all phase Fast Fourier Transform,apFFT)相位一致性特点使正弦信号相位估计不受频率估计影响,但由于频谱泄露和栅栏效应,apFFT相位估计性能受信号频率位置影响。针对该问题,提出了一种基于高精度频率估计和补偿的apFFT相位估计方法。首先,对信号进行高精度频率估计,并以此对信号进行频移补偿,然后对补偿信号进行apFFT,最后求解信号相位。蒙特卡洛仿真结果表明：所提算法的相位估计性能不受信号频率位置影响,相位估计误差性能与理论值一致,受两参数克拉美罗界（CRLB₂）约束,约为1.158 2倍的CRLB₂;相位估计性能和抗噪声能力明显优于经典apFFT算法和其他对比算法。更进一步,利用我国首次火星探测器TW-1（天问一号）近火捕获段干涉测量数据进行算法验证,结果表明：相位估计精度约4 mrad,干涉测量时延估计精度约50 ps。     

双S弯二元排气系统遮挡偏距比对壁温与红外辐射影响的试验研究

为了探究不同遮挡偏距比双S弯排气系统的红外特性,试验研究了遮挡偏距比为55%和100%的双S弯二元排气系统的壁面温度分布和红外辐射特性,并与相应的基准轴对称排气系统进行了对比分析。结果表明：S弯喷管壁温整体要比基准轴对称喷管高约25%,第一S弯下游的上壁面附近存在局部高温区,提高S弯喷管遮挡偏距比后,温度梯度加剧,热应力集中。与基准轴对称排气系统相比,55%和100%遮挡偏距比双S弯二元排气系统均具有突出的红外抑制效果,正尾向（α=0°）红外辐射强度分别降低77.7%和79.3%。从温度和红外辐射强度综合评价,遮挡偏距比并非全遮挡最好,遮挡偏距比从55%提高到100%后,仅能有效抑制上方探测面α=5°和10°的红外辐射,而基本不会改变尾向其他探测方向的红外辐射,在工程设计时应权衡优化损失。     

Midlatitude ionospheric F2-layer response to eruptive solar events-caused geomagnetic disturbances over Hungary during the maximum of the solar cycle 24: A case study

In our study we analyze and compare the response and behavior of the ionospheric F2 and of the sporadic E-layer during three strong (i.e., Dst?<??100nT) individual geomagnetic storms from years 2012, 2013 and 2015, winter time period. The data was provided by the state-of the art digital ionosonde of the Széchenyi István Geophysical Observatory located at midlatitude, Nagycenk, Hungary (IAGA code: NCK, geomagnetic latitude: 46.17° geomagnetic longitude: 98.85°). The local time of the sudden commencement (SC) was used to characterize the type of the ionospheric storm (after Mendillo and Narvaez, 2010). This way two regular positive phase (RPP) ionospheric storms and one no-positive phase (NPP) storm have been analyzed. In all three cases a significant increase in electron density of the foF2 layer can be observed at dawn/early morning (around 6:00 UT, 07:00 LT). Also we can observe the fade-out of the ionospheric layers at night during the geomagnetically disturbed time periods. Our results suggest that the fade-out effect is not connected to the occurrence of the sporadic E-layers.     

玉树地震前的电离层异常现象分析

分析了玉树地震前地基电离层探测临界频率、GPS TEC和卫星探测原位等离子体参量等多个参数的扰动变化信息, 研究了不同高度异常变化的时空关联性. 分析发现, 在地震前一天的4月13日, 多个电离层参量出现同步扰动异常, 电离层临界频率f₀F₂异常相对滑动中值增大40%, 异常空间上存在从震中东南向西南漂移的特性; GPS TEC异常增强15TECU (1TECU=1016m-2)左右, 分布于震中南部经度15°范围内, 且有明显的磁共轭效应; DEMETER观测的原位氧离子密度N_i(O+) 4月13日为1-4月中最强的一天, 异常分布偏向赤道区, 但仅局限在30°-50°左右的经度范围内. 综合三个参量的异常特征发现, 无论是空间的局地性还是时间上的密切关联均反映这次电离层扰动可能与玉树地震孕育有关. 结合其他观测信息, 进一步探讨了这次地震孕育过程的地震电离层耦合机理.      

美国一体化导弹防御系统研究

从美国一体化导弹防御系统的内涵入手,系统地研究了美国导弹防御系统的结构、作战指挥、试验,以及国际合作的情况,最后总结其未来发展趋势。     

Study on O2 generation and CO2 absorption capability of four co-cultured salad plants in an enclosed system

The ability to generate O₂ and absorb CO₂ of several co-cultured vegetable plants in an enclosed system was studied to provide theoretical reference for the future man-plant integrated tests. Four kinds of salad plants (Lactuca sativa L. var. Dasusheng, Lactuca sativa L. var. Youmaicai, Gynura bicolor and Cichorium endivia L.) were grown in the CELSS Integration Test Platform (CITP). The environmental factors including O₂ and CO₂ concentration were continuously monitored on-line and the plant biomass was measured at the end of the test. The changing rules of O₂ and CO₂ concentration in the system were basically understood and it was found that the O₂ generated by the plants could satisfy the respiratory needs of 1.75 persons by calculation. It was also found that the plants could absorb the CO₂ breathed out by 2 persons when the light intensity was raised to 550 mmol m⁻² s⁻¹ PPF. The results showed that the co-cultured plants hold good compatibility and excellent O₂-generating and CO₂-absorbing capability. They could also supply some fresh edible vegetable for a 2-person crew.     

Stability of the seasonal variations in diurnal and semidiurnal components of mid-latitude F2 layer parameters

We report work utilizing 15-min resolution ionospheric data obtained with DPS-4 digisonde in 2003–2011 to study the seasonal variations in amplitudes and phases of the most powerful spectral components of the F2 layer critical frequency (foF2) and peak height (hmF2) fluctuations over Irkutsk (52.5°N, 104.0°E). We show that fluctuations of both parameters contain quasi-harmonic components with periods of T_n = 24/n h (n = 1–7). The number of distinct spectral peaks varies from 3 in summer to 7 in winter. Amplitude and phase characteristics of the diurnal (n = 1) and semidiurnal (n = 2) components is studied using the data sets extracted from the original data sets with band-pass filter. It has been found that the amplitudes of diurnal/semidiurnal foF2 and diurnal hmF2 components are maximum in winter and minimum in summer. Amplitudes of the diurnal components vary gradually; those of the foF2 semidiurnal one, abruptly, thus forming a narrow winter maximum in November–January. The phase (local time of maximum) of the diurnal foF2 component increases gradually by 4–6 h from winter to summer. The phase of the semidiurnal foF2 component is nearly stable in winter/summer and sharply decreases (increases) by 2–3 h near the spring (autumn) equinox. The phase of the diurnal component of hmF2 (local time of minimum) varies slightly between 1130 and 1300 LT; that of the semidiurnal one decreases (increases) by 4–6 h from January to March (from September to November). The results obtained show that the main features of seasonal variations in the diurnal and semidiurnal components of the mid-latitude F2 layer parameters recur consistently during the solar activity growth and decline phases.