某型航空发动机滑油供油系统压力和流量仿真

利用英国商用流体系统仿真软件FLOWMASTER对在中间状态下某型发动机滑油供油系统的压力和流量进行了仿真,总结分析了不同供油温度对该系统流阻特性的影响趋势,根据仿真结果给出了该系统结构的改进建议。     

用于某重型燃气轮机的气体流量试验器研制

阐述了自行研制的某型气体流量试验器的设计思路、系统组成、构件选择以及相关试验.该试验器用于国家863重大项目R0110重型燃机燃烧室喷嘴气体流量测量.该试验器巧妙地将测量系统、操作系统、数据显示、采集与处理系统结合在一起,不仅使设备结构紧凑,占地空间小,实现了单人操作完成试验,并且进气调节系统、冷却器、加温器各成单元便于拆装、运输以及检修、更换.试验器运行稳定,测量精确,成为一种通用高精度气体流量试验系统,可广泛应用于航空发动机、地面燃气轮机和燃用气体燃料的动力装置的喷嘴流量测量.     

超临界压力下航空煤油RP-3焓值的测量及换热研究

基于能量守恒原理提出了一种超临界压力下中国3号喷气燃料RP-3焓值的测量方法,同时对不同超临界压力下RP-3在323～843 K内的焓值进行了测量.结果表明当燃油温度低于其临界温度时,不同超临界压力下燃油的焓值几乎是一样的,当温度高于临界温度后,不同压力下RP-3焓值之间的差异随着压力的升高而缩小.另外,根据焓值曲线计算出的燃油温度及吸热量与先前已做的其他流动与换热实验中的测量数据进行了对比,结果表明该焓值是准确可靠的,满足未来航空发动机内空油换热器的设计要求.最后,研究了热流密度对超临界煤油换热的影响,结果显示当燃油对比温度小于1.179（760 K）时,Nu数随着热流密度的增加而增加.      

商用航空发动机转子部件的电子束焊接

现代商用航空发动机具有长寿命、高可靠性等要求,这对电子束焊接头的设计、制造及检测均提出了更高的要求。介绍了航空发动机转子部件电子束焊接结构及接头设计形式、检测要求,指出了针对商用航空发动机转子电子束焊需开展的研究工作。     

侧载及加热方位对槽道内临界热流密度影响

为了研究侧载以及加热方位对矩形窄缝槽道内临界热流密度特性的影响,在旋转平台上进行了两相流的超重力实验.以蒸馏水为工质,通过改变质量流速、入口温度、侧载大小以及加热方位,获得了发生临界换热现象时的质量流速、实验段压降和壁温的变化趋势,考察了侧载和加热方位对临界热流密度的影响规律,并对侧载下两相流不稳定性进行了简析.实验表明:发生临界换热时,壁温迅速上升,有效加热热流开始减少,关闭加热电源后,实验段压降下降、质量流速回升较明显;侧载以及不同的加热方位对临界热流密度有明显影响;临界热流密度发生前后,蒸汽回流导致进口温度上升,增加了流动的不稳定性.      

火花放电合成射流与超声速来流相互干扰特性数值模拟研究

为了指导火花放电式合成射流激励器在超声速流动控制中的应用,数值模拟研究了火花放电合成射流与超声速来流的相互干扰特性。研究表明火花放电式合成射流在超声速流场中产生强烈扰动,产生较强的激波结构;随着射流的喷出,激励器上游分离区和流场中激波呈先增强后减弱的趋势,激波由弓形激波逐渐弱化为斜激波,并且随着放电能量的增加射流与主流的动量通量比不断增大,射流的干扰和控制能力显著增强。由于超声速流的较大惯性及其对腔内气体的引射作用,激励器的腔体回填速率大幅下降、回填时间明显增长,使得激励器的工作频率受到很大限制。     

Testing the three-dimensional IRI-SIRMUP-P mapping of the ionosphere for disturbed periods

This paper describes the three-dimensional (3-D) electron density mapping of the ionosphere given as output by the assimilative IRI-SIRMUP-P (ISP) model for three different geomagnetic storms. Results of the 3-D model are shown by comparing the electron density profiles given by the model with the ones measured at two testing ionospheric stations: Roquetes (40.8°N, 0.5°E), Spain, and San Vito (40.6°N, 17.8°E), Italy. The reference ionospheric stations from which the autoscaled foF2 and M(3000)F2 data as well as the real-time vertical electron density profiles are assimilated by the ISP model are those of El Arenosillo (37.1°N, 353.3°E), Spain, Rome (41.8°N, 12.5°E), and Gibilmanna (37.9°N, 14.0°E), Italy. Overall, the representation of the ionosphere made by the ISP model is better than the climatological representation made by only the IRI-URSI and the IRI-CCIR models. However, there are few cases for which the assimilation of the autoscaled data from the reference stations causes either a strong underestimation or a strong overestimation of the real conditions of the ionosphere, which is in these cases better represented by only the IRI-URSI model. This ISP misrepresentation is mainly due to the fact that the reference ionospheric stations covering the region mapped by the model turn out to be few, especially for disturbed periods when the ionosphere is very variable both in time and in space and hence a larger number of stations would be required. The inclusion of new additional reference ionospheric stations could surely smooth out this concern.     

Analysis of the ionosphere/plasmasphere electron content variability during strong geomagnetic storm

The ionosphere/plasmasphere electron content (PEC) variations during strong geomagnetic storms in November 2004 were estimated by combining of mid-latitude Kharkov incoherent scatter radar observations and GPS TEC data derived from global TEC maps. The comparison between two independent measurements was performed by analysis of the height-temporal distribution for specific location corresponding to the mid-latitudes of Europe. The percentage contribution of PEC to GPS TEC indicated the clear dependence from the time with maximal values (more than 70%) during night-time. During day-time the lesser values (30–45%) were observed for quiet geomagnetic conditions and rather high values of the PEC contribution to GPS TEC (up to 90%) were observed during strong negative storm. These changes can be explained by the competing effects of electric fields and winds, which tend to raise the layer to the region with lower loss rate and movement of the ionospheric plasma to the plasmasphere.     

一种修正的Osher通量在高阶WCNS中的特性

将一种基于多维修正的Osher通量运用于高阶加权紧致非线性格式(WCNS)中,该修正通量主要在垂直于激波面的界面上增加耗散,能够改善Osher通量的激波捕捉稳定性,同时对边界层和接触间断的分辨率影响非常小。对修正的Osher通量在高阶WCNS中的特性进行研究,通过数值模拟测试了基于Osher通量的WCNS的激波稳定性、热流预测精度、边界层模拟能力、激波边界层干扰模拟能力,并与Steger-Warming通量和Roe通量进行了对比。结果表明修正后的Osher通量比Harten修正的Roe通量具有更好的激波捕捉鲁棒性,而边界层、驻点热流值和激波边界层干扰的模拟则明显优于Steger-Warming通量。上述结果说明了基于修正的Osher通量的高阶WCNS具有较好的激波捕捉特性、热流预测精度和边界层计算能力。     

Latitudinal variation of the topside electron temperature at different levels of solar activity

A database of electron temperature (T_e) measurements comprising of most of the available satellite measurements in the topside ionosphere is used for studying the solar activity variations of the electron temperature T_e at different latitudes, altitudes, local times and seasons. The T_e data are grouped into three levels of solar activity (low, medium, high) at four altitude ranges, for day and night, and for equinox and solstices. We find that in general T_e changes with solar activity are small and comparable in magnitude with seasonal changes but much smaller than the changes with altitude, latitude, and from day to night. In all cases, except at low altitude during daytime, T_e increases with increasing solar activity. But this increase is not linear as assumed in most empirical T_e models but requires at least a parabolic approximation. At 550 km during daytime negative as well as positive correlation is found with solar activity. Our global data base allows to quantify the latitude range and seasonal conditions for which these correlations occur. A negative correlation with solar activity is found in the invdip latitude range from 20 to 55 degrees during equinox and from 20 degrees onward during winter. In the low latitude (20 to −20 degrees invdip) F-region there is almost no change with solar activity during solstice and a positive correlation during equinox. A positive correlation is also observed during summer from 30 degrees onward.