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matlab-instructions
matlab的一些常用指令，说明matlab的常见使用方法(some basic Using instructions for matlab)
- 2011-05-20 11:05:43下载
- 积分：1
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Two-Channel-QMF-Bank
The two-channel QMF bank is one of the earliest and most commonly used filter bank structures.
- 2012-05-04 04:09:48下载
- 积分：1
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sorting
关于相控阵雷达分选的一篇比较好的外文文献(paper on sorting of phased array radar signal )
- 2012-05-10 15:18:11下载
- 积分：1
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equaliz
equal file can equalize comm signal.
- 2012-01-11 21:52:30下载
- 积分：1
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基于ASM3模型的一体式MBR出水水质模拟分析
说明： 将活性污泥3号模型（ASM3）与一体式MBR结合，采用Matlab／Simulink自行开发了可视化的仿真模拟程序，构建了活性污泥系统模型(Abstract:Combined the activated sludge model No.3(ASM3)with the submerged MBR,an activated sludge system was constructed based on the self-developed simulation program of Matlab/Simulink)
- 2020-04-08 10:54:41下载
- 积分：1
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chapter02
antenna design-chapter 2
- 2009-11-25 17:36:40下载
- 积分：1
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xmain
说明： 用matlab写的印刷体数字识别程序，对matlab 6.0以上有效(Written with matlab print digital identification procedures, more effective on matlab 6.0)
- 2010-04-25 13:18:38下载
- 积分：1
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leida
将一张图片由直角坐标转换为极坐标，并且分别显示图片(the trans of coordination)
- 2012-03-24 19:12:50下载
- 积分：1
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pan-tomph
this is heart rate detection method
- 2013-07-27 19:15:43下载
- 积分：1
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matlab-raytrace
射线追踪,包含了起点和终点的射线函数，对于地震传播研究具有重要意义！(Raytracing in a v(z) world. The toolbox contains functions forshooting fans of rays and functions for tracing rays with specific start and end points. General multi-bounce rays with any number of mode conversions can be traced. Automatic routines for P-P and P-S primaries in shot-gather geometry are provided for convenience. Any recording geometry can be used but most functions
vectorize (e.g. are most efficient) for shot-gather geometry. Only
traveltimes and rayparameters are detemined, not amplitudes. In these routines, the velocity models should be considered as "background" models. This means that the depths at which flections and mode conversions occur are dependent of the depths given as layer boundaries in the velocity models. Velocity models are specified by a vector of velocities and a same-size vector of depths. The j th velocity is in effect from the j th to the j+1 th depth.
The bottom of the model is assumed at infinite depth. Thus v=5000
and z=0 specifies a cons)
- 2013-09-16 08:15:48下载
- 积分：1
