电流积分器对I/F转换性能的影响分析

本文介绍了带分流结构的电流/频率转换电路和电流积分器的工作原理,推导了电流积分器的误差,并分析了运放的几个关键参数对l/F电路性能的影响.通过理论推导和实验对比,得出了I/F电路设计时电流积分器电路选择运算放大器的参考依据,并对带分流结构的I/F电路作出了改进.     

力值加载装置控制系统设计

针对力标准机不适用于力值现场校准测试的问题,设计了一种便携式的力值加载装置。该装置采用STM32F103为主控单片机,采用高准确度AD转换器测量力值,优化了力值加载控制算法,避免了力值加载过程中可能出现的各种问题。该装置控制速度快,准确度高,适用于力值现场校准测试。     

基于C8051F020单片机的无人机加速度采集系统

为了满足无人机三轴加速度测量与控制的需要,设计了一种简易、方便的加速度采集系统.本系统采用高集成度单片机C8051F020进行多通道数据的采集和A/D 转换,在单片机内部完成数据存储、数据处理,再利用串行通信接口将数据传送至上位机,然后由无线发射模块发送至地面接收设备.在试验条件下,可以将采集到的数据传送至PC机进行分析或者由液晶显示仪显示.     

一种非周期调制直扩信号扩频码估计方法

对卫星测控中一类扩频码周期与信息码周期之比为非整数的直扩信号进行了研究,得出这类信号可建模成非周期调制直扩信号,提出并讨论了一种基于差分主元分析（D PCA）的非周期调制直扩信号扩频码估计方法,该方法通过计算与差分序列协方差矩阵的最大特征值对应的特征向量完成信息码个数、子序列、信息码同步点等参数的估计,解决了传统矩阵分解方法在估计码序列时码序列相位模糊问题,理论分析和仿真结果表明该方法可以在低信噪比下进行有效估计。     

单音干扰下扩频测控信号伪码跟踪性能研究

扩频测控信号的伪码跟踪性能直接关系到测控系统的测距精度。以伪码跟踪环中鉴相曲线平衡点的过零偏移为研究对象,推导了音频干扰条件下扩频测控信号伪码跟踪的干扰最大误差;并针对干扰最大误差需考虑具体鉴相算法的特点,提出基于相关曲线主瓣的二阶中心矩扩展因子的性能评价方法。该方法利用伪码相关曲线主瓣在干扰前后的畸变情况,反映干扰对伪码跟踪性能的影响。仿真分析表明,干扰最大误差的理论及仿真结果和二阶中心矩扩展因子所得结论一致,从而验证了干扰最大误差理论的正确性以及所提性能指标的有效性。     

S形蒙皮零件成形工艺

通过运用S3F软件对S形蒙皮拉形过程进行模拟仿真分析,评估S蒙皮拉形工艺性;预测拉形过程中将产生的缺陷;制定合理工艺方案;优化零件设计和模具结构;实现了该蒙皮零件在数控蒙皮拉伸机上的拉形。     

数字化机载环控地面检测系统的研究

通过采用两片PIC18F448及其外围器件实现了机载环控地面检测系统的数字化设计。通过I^2C总线实现两片单片机之间的数据传输与协调，并利用其CAN接口模块实现多套检测系统的网络化和远程控制操作。     

PIC16F877实现CAN总线分布式数据采集系统

叙述了一种采用CAN总线通信来实现分布式数据采集的设计方法;介绍了用PIC16F877通过SPI方式直接对MCP2510进行操作,与带智能适配卡的PC机实现CAN通信,并对CAN控制器MCP2510作了分析;给出了系统结构框图与部分硬件图,以及给出了软件设计思路。该基于CAN总线的分布式数据采集系统是一种高可靠性、实时性的系统。     

Upgrading CCIR's foF2 maps using available ionosondes and genetic algorithms

We have developed a new approach towards a new database of the ionospheric parameter $f_{o}F2$. This parameter, being the frequency of the maximum of the ionospheric electronic density profile and its main modeller, is of great interest not only in atmospheric studies but also in the realm of radio propagation. The current databases, generated by CCIR (Committee Consultative for Ionospheric Radiowave propagation) and URSI (International Union of Radio Science), and used by the IRI (International Reference Ionosphere) model, are based on Fourier expansions and have been built in the 60s from the available ionosondes at that time. The main goal of this work is to upgrade the databases by using new available ionosonde data. To this end we used the IRI diurnal/spherical expansions to represent the $f_{o}F2$ variability, and computed its coefficients by means of a genetic algorithm (GA). In order to test the performance of the proposed methodology, we applied it to the South American region with data obtained by RAPEAS (Red Argentina para el Estudio de la Atmósfera Superior, i.e. Argentine Network for the Study of the Upper Atmosphere) during the years 1958–2009. The new GA coefficients provide a global better fit of the IRI model to the observed $f_{o}F2$ than the CCIR coefficients. Since the same formulae and the same number of coefficients were used, the overall integrity of IRI’s typical ionospheric feature representation was preserved. The best improvements with respect to CCIR are obtained at low solar activities, at large (in absolute value) modip latitudes, and at night-time. The new method is flexible in the sense that can be applied either globally or regionally. It is also very easy to recompute the coefficients when new data is available. The computation of a third set of coefficients corresponding to days of medium solar activity in order to avoid the interpolation between low and high activities is suggested. The same procedure as for $f_{o}F2$ can be perfomed to obtain the ionospheric parameter M(3000)F2.     

Midlatitude ionospheric F2-layer response to eruptive solar events-caused geomagnetic disturbances over Hungary during the maximum of the solar cycle 24: A case study

In our study we analyze and compare the response and behavior of the ionospheric F2 and of the sporadic E-layer during three strong (i.e., Dst?<??100nT) individual geomagnetic storms from years 2012, 2013 and 2015, winter time period. The data was provided by the state-of the art digital ionosonde of the Széchenyi István Geophysical Observatory located at midlatitude, Nagycenk, Hungary (IAGA code: NCK, geomagnetic latitude: 46.17° geomagnetic longitude: 98.85°). The local time of the sudden commencement (SC) was used to characterize the type of the ionospheric storm (after Mendillo and Narvaez, 2010). This way two regular positive phase (RPP) ionospheric storms and one no-positive phase (NPP) storm have been analyzed. In all three cases a significant increase in electron density of the foF2 layer can be observed at dawn/early morning (around 6:00 UT, 07:00 LT). Also we can observe the fade-out of the ionospheric layers at night during the geomagnetically disturbed time periods. Our results suggest that the fade-out effect is not connected to the occurrence of the sporadic E-layers.