空乘专业大学生的人格特征与职业素质分析

采用16PF和UPI量表对176名空乘专业大学生进行测评,发现有中度以上心理障碍的人数占8．40％;焦虑值偏高的人数占20．45％;适应性和成长性偏低的人数占33．50％。该群体的职业素质不能适应现代民航空服职业发展的要求。其主要问题是：缺乏认真负责的精神、意志水平不高、对社会信任不足、感情用事、自律不足、依赖性强、缺乏独立工作和应变能力。对该专业大学生加强责任意识、培养合作精神、树立人生目标的职业素质教育显得尤为重要。     

铝粉颗粒燃烧产物的平均弥散度计算研究

采用金属颗粒的扩散燃烧模型和燃烧产物的均匀多相成核理论，对铝粉燃烧所形成的Al2O3平均弥散度进行了计算研究。根据计算结果，对铝粉燃烧区域中的温度、燃烧产物的过饱和度及其凝聚成核速率的变化规律进行了分析讨论。并研究了环境因素对上述多数和铝粉燃烧产物平均弥散度的影响。     

21世纪中国的农业专用飞机

从中国的国情入笔，论速了农业航空在发展国民经济中的重要作用；农业航空采用农业专用飞机是必然趋势；指出农业航空滑坡问题亟待解决。     

产品开发机制初探

国营大中型企业缺乏内在活力,发展后劲不足,除了一些客观因素之外,企业产品开发过程中存在的问题是其重要原因之一。对此本文作了一定分析,并提出了建立企业产品开发机制的思路,旨在使企业不断地推出适销对路的新产品,以充分发挥国有大中型企业在国民经济发展中的主导地位。     

求解大型对称特征值问题的迭代Chebyshev-Lanczos方法

本文研究计算大型对称矩阵极端(几个最大或最小)特征值及相应特征向量的问题,讨论了Chebyshev迭代法对Lanczos方法的应用,提出了Chebyshev-Lanczos方法。计算实践表明迭代Chebyshev-Lanczos方法比迭代Lanczos方法优越。     

综合环境试验中所遇到的一些具体问题的探讨

指出电子产品的可靠性增长、验证试验应采用与实际使用现场相仿的综合环境条件下进行,并结合工程实际介绍了综合环境试验的应用情况、经验和典型结果,并提出了存在的问题。     

一类变结构控制系统滑动模态的特征值条件

在单输入双线性常值变结构控制和比例变结构控制及一般双线性常值变结构控制系统的基础上，将系统推广到一般多输入双线性系统的比例变结构控制，引入排序截尾算子取变结构控制律与状态变量中ｍ个绝对值较大的分量成比例实现对ｎ个被控变量的控制，采用李亚普诺夫方法研究这类系统的滑动模态，得出此类系统产生稳定滑模运动的条件，并对该条件进行讨论和简化，将其表述成系统矩阵与双线性矩阵特征值之间的关系式。同时给出了一个三阶     

飞机液压能源管路系统的振动特性分析

论述了液压能源管路网络系统的建模，着重建立了液体输管路及有关元件的传递矩阵，并给出了如何用特性阻抗法对系统进行求解，最后对飞机液压能源管路系统的动态特性进行了仿真，并指出了一些重要的影响因素。     

A comprehensive study of the 2016 Mw 6.0 Italy earthquake based on high-rate (10 Hz) GPS data

The 2016 M_w 6.0 Italy earthquake is successfully recorded by the near-field 10?Hz GPS and 200?Hz Strong Motion (SM) stations, providing valuable data for this study. A comprehensive study of this earthquake is carried out based on GPS data, which contains coseismic deformations analysis, noise analysis, seismic wave picking, and magnitude determination. The noise of most GPS-derived displacement waveforms can be described as a combination of white noise, flicker noise, and random walk noise after the earthquake occurrence, and the spectral indices vary significantly for most stations, implying that the seismic signals have affected the noise characteristic of GPS-derived displacement waveforms. S-transform is employed to assess the GPS capability to detect the seismic arrival time. The SM station AMT and the GPS station AMAT are in good agreement in seismic wave picking, and the difference is only 1.2?s in the north component, suggesting that the outcome of seismic wave picking using GPS data is reliable. Then, a classic empirical formula is employed to determine the moment magnitude. A robust moment magnitude (Mw 5.90) can be estimated by the nine GPS stations with about 23.9?s. If four GPS stations near the epicenter is chosen to determine the magnitude, it only take 13.0?s to retrieve a reliable preliminary (Mw 5.82) magnitude, which is 5.4?s ahead of nine stations. In addition, Cross Wavelet Transform (XWT) is adopted to measuring the correlation and phase relationship between GPS and SM records. The result of XWT analysis indicates 10?Hz GPS is capable of capturing reliable and accurate coseismic dynamic deformations, as evidenced by the XWT-based semblance being close to 1 between GPS and SM records. The above results confirm the capability of 10?Hz GPS to capture coseismic dynamic deformations, detect seismic arrival time, and determine earthquake magnitude. Moreover, rapid magnitude determination based on 10?Hz GPS data can be regarded as an important supplement to Earthquake Early Warning (EEW).     

Ionospheric F2-Layer critical frequency retrieved from COSMIC radio occultation: A statistical comparison with measurements from a meridional ionosonde chain over Southeast Asia

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.