Ionospheric behavior of the F2 peak parameters foF2 and hmF2 at Hainan and comparisons with IRI model predictions

Monthly median values of foF2, hmF2 and M(3000)F2 parameters, with hourly time interval resolution for the diurnal variation, obtained with DPS-4 digisonde observations at Hainan (19.4°N, 109.0°E) are used to study the low latitude ionospheric variation behavior. The observational results are compared with the International Reference Ionospheric Model (IRI) predictions. The time period coverage of the data used for the present study is from March 2002 to February 2005. Our present study showed that: (1) In general, IRI predictions using CCIR and URSI coefficients follow well the diurnal and seasonal variation patterns of the experimental values of foF2. However, CCIR foF2 and URSI foF2 IRI predictions systematically underestimate the observed results during most time period of the day, with the percentage difference ΔfoF2 (%) values changing between about −5% and −25%, whereas for a few hours around pre-sunrise, the IRI predictions generally overestimate the observational ones with ΔfoF2 (%) sometimes reaching as large as ∼30%. The agreement between the IRI results and the observational ones is better for the year 2002 than for the other years. The best agreement between the IRI results and the observational ones is obtained in summer when using URSI coefficients, with the seasonal average values of ΔfoF2 (%) being within the limits of ±10%. (2) In general, the IRI predicted hmF2 values using CCIR M(3000)F2 option shows a poor agreement with the observational results. However, when using the measured M(3000)F2 as input, the diurnal variation pattern of hmF2 given by IRI2001 has a much better agreement with the observational one with the detailed fine structures including the pre-sunrise and post-sunset peaks reproduced reasonably well. The agreement between the IRI predicted hmF2 values using CCIR M(30,000)F2 option and the observational ones is worst for the afternoon to post-midnight hours for the high solar activity year 2002. During daytime hours the agreement between the hmF2 values obtained with CCIR M(30,000)F2 option and the observational ones is best for summer season. The discrepancy between the observational hmF2 and that obtained with CCIR M(30,000)F2 option stem from the CCIR M(3000)F2 model, which does not produce the small scale structures observed in the measured M(3000)F2.     

滑阀稳态液动力的计算和分析

以液氧/煤油补燃循环火箭发动机中流量调节器中滑阀为例,介绍了滑阀稳态液动力的一种计算方法,分析了不同结构参数下稳态液动力的变化规律,得出了滑阀的稳态液动力与滑阀位移、液流出口处的流道形状以及刃边厚度关系的一些初步结论。     

水洞动态测力和流动显示一体化实验技术

研制能够用于低速水流中的三分量内式测力天平,结合氢气泡(或染色液)方法,在水洞(槽)中实现测力和流动显示实验同步进行的动态实验系统,克服了通常测力和流动显示分别在风洞和水洞中进行,实验条件不同给结果分析带来的困难。天平采用高精度位移传感器,避开传统的应变片技术应用于水中所遇到的技术困难。简易飞行器模型的静态和等速俯仰实验结果表明了测量系统的可靠性。     

空气压强对激光推进器冲量耦合系数影响

设计并加工了激光推进器实验模型,以空气为推进工质,利用脉冲式CO2激光器,研究了空气压强对激光推进器冲量耦合系数影响。实验结果表明,空气压强对激光推进器性能有显著影响。在文中实验条件下,当空气压强大于6 kPa时,激光推进器冲量耦合系数随压强减小而减少较慢;当空气压强小于6 kPa时,激光推进器冲量耦合系数随压强减小而减少很快。     

高亚声速二维位势流动的气动力计算

本文提供了一个精确表达式,通过它可将亚声速位势流动仿射变换成不可压缩流动。同时给出了新的气动力计算公式。在流过Joukovski翼型的气动力计算中,它与用计算机提供的精确数值计算结果相比较,二者很符合。     

功率谱密度(PSD)在评价超精密光学表面中的应用研究

用原子力显微镜对不同工艺下获得的超光滑反射镜基片进行了功率谱密度(PSD)检测,并对结果进行分析,以指导光学元件加工。     

10°尖锥标模高超声速动导数的实验测量

在中科院力学所JP－4B高超声速脉冲风洞中，用模型自由飞方法对1°尖锥开展动态实验测量，并用参数微分法辨识得到了该模型的俯仰阻尼导数。文中还介绍了在模型优化设计，模型工艺以及实验测量记录和数据判读技术方面的一些进展。实验结果表明；脉冲风洞中模型自由飞方法得到的10°尖锥标模高超声速动态气动特性测量值与国外可比数据一致，重复测量精度与弹道把试验相当。     

Fe—10Ni—14Co钢标准状态的组织研究

用透射电子显微镜重点研究了Ｆｅ－１０Ｎｉ－１４Ｃｏ钢的标准处理状态（８３０℃风冷＋—７３℃＋５１０℃Ｓｈ）的微观组织结构。５１０℃回火不同时间，由于Ｍ２Ｃ的析出状态发生变化，钢也由峰时效（５１０℃／１０ｍｉｎ）→过时效（５１０℃／５ｈ）→明显过时效转变。５１０℃５ｈ合会开始发生逆转变。     

深层搅拌法技术及其工程应用

深层搅拌技术是对软土地基进行处理的较常用技术 ,它具有加固效果显著、形式灵活多样、环境无污染、施工机具简单、施工速度快、节省投资等优点 ,目前在地基处理和基坑工程中广泛采用。本文主要阐述该技术特点及在地基处理工程中的应用 ,对同类工程设计具有重要的参考价值。