CFM56系列发动机部件技术综述

综述了CFM56系列大涵道比发动机在风扇叶片、防冰、吞水、燃烧室、尾喷管方面所采用的结构技术。     

一种基于FPGA的海杂波产生器设计

海杂波是反舰导弹末制导雷达回波的主要背景噪声,在末制导雷达模拟器的设计中,海杂波产生器是一个重要组成部分。在研究海杂波噪声概率分布密度的基础上,给出了一种基于FPGA技术的海杂波产生器的设计方案,并利用Altera公司的cyclone II系列芯片和QuartusII开发软件对设计进行了仿真验证。采用FPGA技术可以方便地对设计方案、海杂波的分布形式、数据量大小进行修改。仿真结果表明,该设计能够产生符合要求的海杂波信号,并且具有结构简单、集成度高、易于修改等特点。     

掠海飞行导弹基于滤波的滑模高度控制

超低空掠海飞行反舰导弹或巡航导弹的高度表测量信号受到海浪噪声严重影响,其传统控制方法在海面风等干扰因素影响下,导弹难以保持定高飞行,容易失稳落水。采用基于滤波的滑模高度控制方法,利用组合高度测量Kalman滤波估计,有效消除海浪和测量噪声,提出一种基于趋近律的滑模控制方案,该方案具有控制参数少、抖振不明显、便于应用的优点。仿真表明,通过组合滤波,比较准确获取导弹飞行高度信息。与PID控制方法和常规滑模控制方法相比,基于趋近律滑模控制方法抗干扰性强,响应速度快,动态品质良好。应用该方法,导弹能够在较恶劣海情和海面风干扰下实现稳定掠海飞行,有效降低击水概率。     

飞机结冰探测器安装位置研究

基于飞机结冰探测器安装要求,通过三维数值仿真,模拟了机头表面流场和水滴撞击特性.通过标定水滴遮蔽区和浓度增加区引入危险位置点的概念,对结冰探测器的安装位置进行了分析,模拟了安装位置处结冰探测器探头表面和飞机主要迎风部件表面的水滴收集特性和结冰特性,并进行对比分析.分析结果表明探头表面的最大收集系数、结冰强度和结冰程度等...     

内融冰盘管动态蓄冰特性数值模拟与实验研究

采用焓法建立了管外结冰过程的二维动态数学模型,数值模拟了冰层沿换热管径向及长度方向的动态生长规律,并在此基础上分析了载冷剂进口温度、流量变化和不同结冰时间等对冰层动态生长及蓄冷特性的影响,并进行了实验验证。实验结果表明:在结冰初期的2 h内冰层厚度及动态蓄冷量数值模拟结果与实验数据误差较大,而在蓄冰过程结束时二者吻合较好,误差在10%以内;沿载冷剂流动方向冰层厚度逐渐减小,数值模拟与实验结果基本吻合。数值模拟结果与实验数据基本相符,验证了建立的数学模型的合理性。     

基于改进A*算法的UUV冰下避障航迹规划算法

针对冰下避障航迹规划问题,提出了一种基于改进A*算法的三维冰下避障航迹规划算法.不同于传统的A*航迹规划算法,该算法结合了人工势场航迹规划算法的思想,将水下地形碰撞约束、海冰碰撞约束以及UUV巡航高度约束重新编排.算法分析表明,该避障航迹规划算法能够有效增强UUV冰下避障能力与定深巡航高度控制能力.基于改进的A*冰下避障航迹规划算法,给出了上述约束的设计方法并进行了仿真验证.仿真结果表明,基于上述约束的航迹规划算法具有良好的避障能力、巡航高度控制能力以及航行距离控制能力.     

Improving aircraft aerodynamic performance with bionic wing obtained by ice shape modulation

For Unmanned Aerial Vehicles (UAVs) with limited electrical power to achieve effectively anti-/de-icing at the leading edge of the wing, a strategy of ice shape modulation was proposed. Isolated simulated ice shape pieces printed by 3D printing technology are mounted on a NACA0012 finite wing model, and its lift/drag coefficients and suction-side velocity fields are measured by the six-component force balance and the Particle Imaging Velocimetry (PIV), respectively. The ratio of the spanwise length of a single ice shape piece to chord length and the spanwise length of the non-icing area between the two adjacent single ice shape pieces are defined as dimensionless ice shape length (w/c) and dimensionless modulation ratio (w/λ), respectively. The results indicate that for a fixed w/λ, the wing lift coefficient first increases and then drops with increasing w/c, and a peak value exists when w/c is between 0.1 and 0.2. The lower the w/λ is, the higher the wing lift coefficient will be. The periodical variation of the flow separation area along the spanwise direction is attributed on the one hand to the acceleration effect of the flow field in the non-icing area which reduces the separation area, and on the other hand to the cross-flow caused by the streamwise vortices from the non-icing area to the icing area which promotes the mixing of the flow field (similar to vortex generators). The obtained modulation law is verified through flight tests and provides guidance for the use of ice shape modulation scheme for UAVs that cannot be completely anti-/de-icing under severe weather conditions.     

基于极化神经网络的雷达舰船检测识别方法

相参雷达捕获的全极化海面目标距离-多普勒(RD)回波数据中，目标区域占比小、信噪比低，且海况环境与干扰种类多变，使得经典的深度神经网络在此种条件下检测识别精度较低。为此，本文提出了一种基于极化深度神经网络的全极化相参雷达海面目标检测识别算法。首先，引入极化特征提取模块挖掘目标与干扰的差异化特征;其次，通过特征金字塔网络解决小目标检测识别的问题;最后，使用级联结构进一步提升算法性能。在全极化相参雷达回波数据集上的测试结果表明:基于特征值与特征矢量的极化特征对于数据集中两类舰船目标的平均精度分别达到0.907 9与1.0，相比不采用极化特征有着显著提高。     

天基海表精细探测微波载荷性能分析与展望

海表精细探测是海洋卫星未来发展的重要方向。介绍卫星海表参数探测的特点与优势，总结海表温度、海表高度、海表盐度等要素，分析天基探测载荷的发展现状。根据海表参数时空变化特性，分析高时空分辨率微波探测载荷性能需求。在此基础上，针对美国和欧洲相关卫星系统发展计划，分析了高时空分辨率、高精度天基微波探测载荷可实现性与未来发展趋势，针对海表精细探测天基微波载荷的发展提出了建议。     

An improved altimeter-derived gravity anomaly from shipborne gravity based on the mean sea surface height constraint factors method

Coastal marine gravity modeling faces challenges due to the degradation of the quality and poor coverage of altimeter data in coastal regions. The effective fusion of shipborne gravity data and altimeter-derived marine gravity data can make shipborne gravity data more useful for the accurate estimation of altimeter-derived coastal marine gravity. A mean sea surface height constraint factor (MSSHCF) method based on the ordinary kriging method and the remove-restore technique is proposed to fuse altimeter-derived gravity model with shipborne gravity data. In this method, all data are standardized during the interpolation process to reduce the error and mean sea surface as a vertical variable is added to the semi-variance function in ordinary kriging to obtain the residual shipborne gravity as corrected data source. The coastal marine gravity models V2.1 and V3.1 which fused altimeter-derived gravity data with shipborne gravity data and V1.1 without shipborne gravity data at a spatial resolution of 1′×1′ can be obtained. Validation experiments show that the accuracy of the gravity model V3.1 obtained by the MSSHCF method more closely agrees with the validated gravity model DTU17 and SS V31 than the model V2.1 obtained by the ordinary kriging interpolation method and the V1.1 model. Our results were validated against shipborne gravity data; the accuracy of model V3.1 was 4.95 % higher than the model V1.1 in South China Sea area A and 2.48 % higher in South China Sea area B. Meanwhile, the accuracy of model V3.1 was 2.07 % higher than model V2.1 in South China Sea area A and 2.42 % higher in South China Sea area B. The effects of distance from the coast and sea depth on the marine gravity model were also evaluated. The results show that the gravity model V3.1 has higher accuracy with the change in ocean distance and depth than the V2.1 and V1.1 gravity models. Thus, our study shows that the MSSHCF method effectively refines coastal altimeter-derived gravity using shipborne gravity data.