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matlabshiyongchengxubaili
常用的MATLAB变换代码,1-32是:图形应用篇
33-66是:界面设计篇
67-84是:图形处理篇
85-100是:数值分析篇适合初学者(MATLAB transform code commonly used 1-32 is: graphics articles 33-66 is: interface design articles 67-84 is: is the graphics chapter 85-100: Numerical Analysis Section for beginners)
- 2010-11-09 21:14:05下载
- 积分:1
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split1
利用分步傅立叶积分法,计算了光纤中色散与SPM效应(Step-by-step use of Fourier integral method, the calculation of the fiber dispersion and SPM.)
- 2011-01-04 10:00:13下载
- 积分:1
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New-folder-(3)
musc this program calculates arrival
- 2013-10-01 23:53:23下载
- 积分:1
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Untitled
uwb A Framework for UWB-Based Communication and Location Tracking Systems for Wireless Sensor
- 2011-11-30 19:37:05下载
- 积分:1
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DDC_prj1
公司最近项目做的一个DDC(数字下变频)simulink建模模型 真情奉献给大家(this is a project about digital down-converter,it is bulit with Simulink.)
- 2010-08-18 11:26:00下载
- 积分:1
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mna_compute_source_vector
计算电路矢量值,本代码主要计算电路的电流傅里叶矢量,稍加修改就可以用于求电路的电源傅里叶矢量(compute circuit vector)
- 2013-10-12 06:21:36下载
- 积分:1
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linedatas
line data for ieee 5,14,30 and 57 bus systems
- 2015-02-04 23:55:23下载
- 积分:1
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grav_plot
地球物理勘探中重力资料解释的主要目的是由地表观测值推断地下可能存在的密度分布。众所周知,任何一组重力数据都可能由无数个密度分布所引起。即使假设了重力异常是由具有均匀密度差的单一地质体产生的,也得不出唯一的解。画图(Gravity geophysical exploration data interpretation main purpose is inferred from surface observations may exist underground density distribution. Is known, any set of data may be provided by gravity density caused numerous. Even assuming that the gravity anomaly is determined by having a uniform density difference arising from a single geological body, they have no unique solution. Paint)
- 2013-11-21 23:46:56下载
- 积分:1
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123dadas123
these are two audio features , LPC whith cepstral coefficients this a feature for speech recognition and speaker recognition , and other feature named zcr for calculate the change of the sing ( + or - ) of the signal.
- 2013-05-07 09:06:54下载
- 积分:1
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GSM
program to interface nwith gsm modem
- 2014-02-02 20:41:20下载
- 积分:1