基于DSP的雷达车辆检测器的研制

研究一种基于DSP芯片TMS320F240处理器的雷达车辆检测器.该检测器在简单的连续波上加上尖锐的定时标志,克服了连续波雷达不能测距的弱点,采用三角波调制的线性调频连续波雷达实现测距.通过在DSP中预存与各车道相应的FIR系数实现对车辆的检测,便于实时处理.选用带有外围接口如ADC,SCI(串行通信接口)的TMS320F240处理器,增加系统的集成度,减小干扰.实际运行证明,该车辆检测器对运动车辆的速度和流量的检测精度高达95%,适用于智能化的交通系统.     

求广义KdV方程孤立波解的一种迭代法

标准的ADM方法需要显式地求Adomian多项式,已有研究者对标准的ADM方法作了改进,得到了不用显式求Adomian多项式的一种新的ADM方法。利用改进的Adomian分解法,讨论了一类广义KdV方程的孤立波解,并借助于数学软件Maple求得了方程的数值解。通过与对应的精确解的对比,表明我们得到的近似解的精确度比较高。     

关于Einstein-Rosen柱面引力波

在Ｖｉｅｒｂｅｉｎ 表述的局域Ｌｏｒｅｎｔｚ群引力规范理论框架下,给出了Ｅｉｎ－ｓｔｅｉｎ－Ｒｏｓｅｎ 严格柱面引力波的能量动量、功率流密度和辐射总功率的严格表达式．讨论了波的各部分之间的互作用     

带时滞项的高阶Kirchhoff方程的拉回吸引子

研究了带有时滞项的高阶Kirchhoff方程的拉回吸引子的存在性.首先利用解的有界性验证了拉回吸引集的存在性,接着借助sobolev空间的紧嵌入证明了该初边值问题产生的过程是紧的,最后得到了拉回吸引子的存在性.     

铁磁-反铁磁双层系统低温内能

应用线性自旋波的理论导出铁磁－反铁磁双层系统的Ｈｅｉｓｅｎｂｅｒｇ模型哈密顿量,采用矩阵格林函数运动方程技术得到自旋波的色散关系,利用数值计算的方法得到铁磁－反铁磁双层的低温内能。     

强阻尼半线性波动方程的指数吸引子

研究了一类带强阻尼项的半线性波动方程的指数吸引子的存在性,通过算子分解来构造渐近紧的不变吸收集,进而得到了空间Ｅ１中的指数吸引子     

(LiFe)xZn1-2xFe2O4铁氧体的吸波性能研究

采用固相烧结工艺,按不同配方分别制备了(LiFe)xZn1-2xFe2O4(x=0.1、0.2、0.3、0.4、0.45、0.5),用Agilent8510c矢量网络分析仪测试,在0.5～13GHz频段内材料的吸波性能.实验发现(LiFe)0.45Zn0.1Fe2O4有较强的吸波性能,然后再对(LiFe)0.45Zn0.1Fe2O4进行不同搀杂,并在0.5～18GHz频段内测试材料的吸波性能,发现掺入1wt%的Al2O3对增加-10dB带宽非常有效果.     

消除岩石动态实验曲线振荡的有效途径

就岩石动态应力－应变－应变率曲线测定中存在的严重振荡问题进行了讨论，提出了消除这一振荡的有效途径：改传统的矩形波加载为半周期正弦波加载。并就实现半周期正弦波加载的冲头结构进行了研究。     

Fine three-dimensional P-wave velocity structure beneath the capital region and deep environment for the nucleation of strong earthquakes

A detailed 3-D P-wave velocity model of the crust and uppermost mantle under the capitol region is determined with a spatial resolution of 25 km in the horizontal direction and 4-17 km in depth. We used 48750 precise P-wave arrival time data from 2973 events of local crustal earthquakes, controlled seismic explosions and quarry blasts. These events were recorded by 123 seismic stations. The data are analyzed by using a 3-D seismic tomography method. Our tomographic model provides new information on the geological structure and complex seismotectonics of this region. Different patterns of velocity structures show up in the North China Basin, the Taihangshan and the Yanshan Mountainous areas. The velocity images of the upper crust reflect well the surface geological, topographic and lithological features. In the North China Basin, the depression and uplift areas are imaged as slow and fast velocity belts, respectively, which are oriented in NE-SW direction. The trend of velocity anomalies is the same as that of major structure and tectonics. Paleozoic strata and Pre-Cambrian basement rocks outcrop widely in the Taihangshan and Yanshan uplift areas, which exhibit strong and broad high-velocity anomalies in our tomographic images, while the Quaternary intermountain basins show up as small low-velocity anomalies. Most of large earthquakes, such as the 1976 Tangshan earthquake (M 7.8) and the 1679 Sanhe earthquake (M 8.0), generally occurred in high-velocity areas in the upper to middle crust. However, in the lower crust to the uppermost mantle under the source zones of the large earthquakes, low-velocity and high-conductivity anomalies exist, which are considered to be associated with fluids, just like the 1995 Kobe earthquake (M 7.2) and the 2001 Indian Bhuj earthquake (M 7.8). The fluids in the lower crust may cause the weakening of the seismogenic layer in the upper and middle crust and thus contribute to the initiation of the large crustal earthquakes.     

运动物体生成内波的一类非线性谱方程组

本文给出了由运动物体所生成内波的基本方程组和对应的谱方程组。该方程组的线性部分是一具有体积源(其下简称为体源)的Sturm—Liouville本征值问题，而它的非线性部分是由体源与线性波场相互作用的谱表示。在这类强迫方程的源项中包含了10类内波谱，这些谱最终均可利用内波的振幅谱表示。本文给出了线性波场波要素的谱表示和运动物体生成内波的非线性谱方程可解性的讨论。为了检验所得到的谱方程组，文中又进行了该谱方程组线性部分的数值计算。