基于Web的拦截网页中弹出广告编程技术的研究及实践

本文采用基于Web的拦截技术,通过对服务器传来的数据包进行分析,对其中的弹出广告的数据包进行过滤,最终实现拦截网页中弹出的广告牌,达到快速浏览网页的效果。     

对高校学生欠费问题的思考

本文以独特的视角，分析了高校学生欠费造成的危害及形成的原因，提出了解决该问题的若干对策，对指导高校学生欠费清理工作有一定参考价值。     

非线性失真的准确测量

为满足宽频范围，尤其是低频段非线性失真测量的需求，分析和比较了非线性失真测量中常用的基波抑制法和谐波分析法，并给出了测量仪器选用的一些原则，分析了两种方法的适用范围。结果表明，89441A矢量信号分析仪可以弥补传统频谱分析仪和音频分析仪的缺陷，在非线性失真测量方面有较好的应用效果。     

论中国金融风险问题

文章结合国内金融市场的发展和国际金融市场的大趋势，阐述了中国金融风险突出的种种原因，进一步提出了防范和化解金融风险的有效对策。     

切割法测取螺旋弹簧的残余应力

通常用实验方法测定园柱螺旋弹簧残余应力。本文提出了切割法对比测试技术，为确定高应力、高疲劳强度的弹簧制造工艺提供了依据。     

水面波作用下平面射流振翅运动的频率锁定现象

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。     

管材探伤中最佳水声程问题的探讨

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。     

太阳活动区R9077引起的强烈吸收事件

利用南极中山站的观测数据分析了太阳活动区R9077所引起的强烈吸收事件，其中2000年7月14日的太阳质子事件引起了持续3天多强烈的极盖吸收，同时，激烈的太阳活动使磁层处于极度扰动状态，磁层高能粒子沉降使许多持续时间较短的吸收峰叠加在极盖吸收背景之上，最突出的是7月1日的吸收增强事件，其最大值达26dB。这是自1997年2月中山站安装成像式宇宙噪声接收机以来观测到的最强的吸收，另一个较突出的吸收峰发生在14日1753UT前后，本文还讨论了产生这些吸收的原由。     

Higher order ionospheric error correction in BDS precise orbit determination

The ionospheric error affects the accuracy of the Global Navigation Satellite Systems observation and precise orbit determination. Usually, only the first order ionospheric error is considered, which can be eliminated by the ionospheric-free linear combination observation. But the remaining higher order ionospheric error will affect the accuracy of observations and their applications. In this paper, the influence of the higher order ionospheric error have been studied by using the International Geomagnetic Reference Field 13 and the Global Ionosphere Maps model produced by the Center for Orbit Determination in Europe. Focus on ionospheric error, the experiment of paper at doy 302 in 2019, which show that the second order ionospheric error impacting BeiDou Navigation Satellite System (BDS) B1I and B3I observation is 6.3569 mm and 11.8484 mm, respectively. Whereas, the third order ionospheric error impacting BDS B1I and B3I observation is 0.1734 mm and 0.3977 mm, respectively. Due to the current measurement accuracy of BDS carrier-phase observation can reach 2 mm, the influence of high order ionospheric error on observation should be considered. For BDS precise orbit determination, the orbit overlapping results are indicated that its orbit accuracy can be improved approximately 5 mm with the higher order ionospheric error correction, which is also in agreement with the results of Satellite Laser Ranging in this work.     

Time variations of the total electron content in the Southeast Asian equatorial ionization anomaly for the period 2006–2011

This study presents the time variations of the total electron content in the South East Asian equatorial ionization anomaly. The time variation of the TEC is analyzed through the period 2006–2011 by using a latitudinal chain of GPS stations extending in the northern and southern hemisphere. The data shows that the shape of the diurnal variation of the TEC depends on the latitude: a plateau is observed at the stations near the equator and a Gaussian at the station distant from the equator. We observe a semiannual pattern in all the stations with maxima at equinox. In both hemispheres, the amplitude of the crest is larger in spring than autumn from 2006 to 2008 and smaller in spring than in autumn from 2009 to 2011. We also observe an asymmetry between the amplitude and the position of the two crests of ionization. There is a very high level of correlation between the amplitude of the TEC at the two crests and the sunspot number: ∼0.88. During the deep solar minimum 2008–2009, the amplitude of crests of ionization becomes small during several months in summer and winter. The results show that both crests move significantly equatorward in winter than other seasons and there is a tendency for both crests to appear earlier in winter and later in summer.