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211.
本文从设计、施工、养护三方面分析了公路水毁的原因 ,提出预防和根治公路水毁的宏观综合处理措施  相似文献   
212.
通过激光流动显示 (LIF)和测量方法 ,就表面水波对垂直平面射流的振翅运动的影响进行了实验和理论研究。研究表明 ,在表面波的影响下 ,振翅运动依然存在。同时 ,波高计和多谱勒激光测速仪的测量结果显示 ,当表面波的频率接近但低于射流振翅运动的自然频率时 ,射流振翅运动的实际振动频率将被锁定在表面波的频率上。而当表面波的频率大于射流振翅摆动的自然频率时 ,频率锁定现象将不存在。  相似文献   
213.
多年来,中小直径薄壁管超声水浸聚焦探伤法中,H=F-√R^2-L^2被称为最佳水声程公式,但探伤实践中发现,实际最佳声程和由此式计算出来的理论最佳水声程出入较大,甚至完全不符。其原因是什么?此式存在的条件是什么?其适应性怎样?最佳水声程的涵义是什么?应如何确定?本文从理论和实践两方面对上述问题进行了分析,并提出了相应的结论。  相似文献   
214.
根据动量原理,提出了反重力充型的数学模型;用高速摄影观察了充型的动态过程,结果表明,反重力充型可用二阶非线性方程描述,具有衰减振荡的动力学特性。  相似文献   
215.
应用氢气泡流动显示技术对圆盘上小半球对边界层转捩的影响进行了观测.实验结果表明当Rer>302时,将会从小半球脱落周期性的发卡涡.发卡涡在自诱导速度的作用下产生倾斜向上的运动,发卡涡头部顶端率先进入高速流区,因而比其根部运动更快,使发卡涡受到流向的拉伸,增加其流向的涡强,增加了流向涡强将使发卡涡的头部有更大的向上速度,由此而形成了不断加强的拉伸、自诱导过程,这就使三维扰动快速增长,导致边界层速度剖面出现局部的暂时变形,从而产生一个强剪切层,强剪切层很不稳定,导致发卡涡破裂而形成湍斑,在下游发展成完全湍流,而在边界层转捩过程中则观察到了水充速度有很强的负脉动.在小半球前缘附近会形成稳定的standing涡,并对standing涡及发卡涡对周围流体的诱导作用进行了细致的分析.小半球对边界层的扰动以锲形向下游传播,锲形的半顶角称为扰动扩散角,一个半球与三个半球的尾迹区没有明显的区别,每个半球扰动的扩散角均为5.7°.  相似文献   
216.
某舰飞行甲板区域流场特性的水洞试验   总被引:1,自引:0,他引:1  
为了满足舰载直升机的需要,南航直升机技术研究所对某舰飞行甲板区域流场进行了水洞试验。本文详述了水洞试验的方法和技术,通过对舰模在各种水速、各种航行偏角状态下的试验,得到了大量照片,并据此对该舰机库后部、飞行甲板上部周围流场进行了分析,得出了在飞行甲板机库门外有一趋于收缩的稳态区,随着流速V的增大,这一区域变短。稳态区之后很快变为乱流区。从侧面上看,稳态区高度有从降低再向上扩散的趋向。在向右偏航时,  相似文献   
217.
Because of global warming, global sea levels have risen, the frequency of drought in Taiwan is much more frequent in winter and spring, and rainfall tends to concentrate in summer. The probability of disaster-type weather has also increased significantly. Estimating precipitable water vapor (PWV) through GPS signals, related studies and analyses of weather conditions, and the effective use of meteorological forecasts have been valued by many meteorological research organizations and officials. In this study, PWV data from 2006 to 2017 and rainfall data were used for long-term harmonic analysis. PWV data calculated by ECMWF (ECMWF-PWV) and PWV data calculated by GPS (GPS-PWV) were subjected to regression analysis to verify the reliability of the GPS-PWV data. The research results show that GPS-PWV and ECMWF-PWV have extremely high correlations; however, the climatic characteristics of some regions and the high spatial resolution of GPS-PWV are able to accurately calculate the high topographic relief of small areas. It is judged that the GPS-PWV is more accurate than the ECMWF-PWV. It is worth noting that the PWV trend of the regions during the 6-year-before period has not changed very much, but the rainfall trend has changed obviously. Except for the eastern region, most of the regions show a decreasing trend year by year. More long-term observations are still needed to prove whether this phenomenon relates to global warming. Long-term rainfall analysis showed that the topography blocked water vapor to the western, southern, and mountainous regions, making them distinctly wet or dry. The harmonic curve showed great consistency with the peaks of PWV and rainfall. However, in the northern and eastern parts of the windward side, the time when maximum rainfall occurred each year may be one month later than the time when the maximum PWV value occurred each year. The reason for this difference is likely to be a decrease in the number of autumn typhoons, resulting in a nearly one-month difference in PWV peaks and rainfall peaks. Finally, we analyzed the linear trend of GPS-PWV and temperature for all regions in Taiwan, and found that annual increasing rate of GPS-PWV and temperature of all regions are within 0.4–0.5 mm/year and 0.04–0.11 C°/year, respectively.  相似文献   
218.
杨森  张翔伦 《航空学报》2020,41(z2):724288-724288
基于能量优化的无人机机动能够使无人机在不失去决定性位置优势的情况下获取相对于对手的能量优势,足够的能量优势可转换为有效的位置优势,有利于无人机在空战中随时改出当前机动并投入下一机动动作,对于无人机获取空战胜利至关重要。开展了基于能量优化的无人机机动轨迹生成方法研究,通过在无人机机动飞行包线内设计合适的机动指令,使得无人机能量性能指标最优。以上升转弯机动为例进行了机动轨迹生成的详细设计,并与常规上升转弯机动轨迹生成结果进行对比,仿真结果显示所设计的机动动作完成时间缩短了28.6%~83.8%,总能量变化减少了64.7%~70.1%,实现了无人机机动飞行的能量优化。  相似文献   
219.
使用Haim Nessyahu和Eitan Tadmor给出的求解双曲型守恒律的中心差分交错格式求解浅水波方程,经一维溃坝问题数值实验验证了该格式对于求解浅水波方程的可行性和有效性。  相似文献   
220.
This study aimed to investigate the performance of genetic algorithms coupled with partial least squares (GA-PLS) modeling of spectral reflectance in retrieving equivalent water thickness (EWT) at leaf and canopy level. A genetic algorithm was used to identify a subset of spectral bands sensitive to the variation in EWT, and PLS was then applied to relate the identified bands to EWT values. GA-PLS was applied to leaf level reflectance available from LOPEX dataset, and canopy data includes reflectance simulated by a leaf radiative transfer model PROSPECT and a canopy radiative transfer model SAILH and acquired by airborne visible/infrared imaging spectrometer (AVIRIS). The results indicate that GA-PLS has the capability of retrieving EWT from leaf and canopy reflectance, and achieved good estimation accuracy, i.e. low root mean square errors (RMSE) and high squared correlation coefficients (R2). For the retrieval at leaf level, the estimation accuracy can be as good as RMSE = 0.0019 g/cm2 and R2 = 0.939 or better. For the retrieval at canopy level, the model accuracy is RMSE = 0.0061 g/cm2 and R2 = 0.966 or better when PROSPECT-SAILH simulated reflectance was used; when AVIRIS image spectra were used, the model accuracy is RMSE = 0.0094 g/cm2 and R2 = 0.8734 for the calibration, and RMSE = 0.0132 g/cm2 and R2 = 0.7756 for the validation. These results from GA-PLS modeling support the conclusion that GA-PLS has the potential to be applied to AVIRIS, Hyperion and HyMap imagery for retrieving EWT. The selected bands for the AVIRIS datasets differ from those for the LOPEX and PROSPECT-SAILH simulated datasets, and this inconsistence of the selected bands for different datasets indicates that the GA-PLS method has the advantage of tuning the optimum bands for PLS regression and accommodating the effects of confounding factors.  相似文献   
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