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V1Features

于 2013-04-05 发布 文件大小:14KB
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  This is an archive for feature extraction.

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    2009-01-03 09:03:07下载
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    说明:  修改视图图标及标题,能够让程序员使用自己设定的标题及图标(Edit View icon and title, allowing programmers to use their own title and icon set)
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  • deng2
    绘制等值线Matlab程序,可以实现绘制功能,比较初级,但是觉得很重要所以上传(Contour drawing)
    2011-04-22 14:55:03下载
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    比例积分型的GPC,由新的目标函数解出的控制率与常规PI控制有着一样的形式,这样就获得了一种具有PI结构的广义预测控制,而且其参数 、 有着明显的工程意义,整定原则基本类似于PID。(Proportional-integral-type GPC, the new objective function solution of the control rate with conventional PI control has the same form, so to obtain a PI structure with generalized predictive control, and its parameters, there is a clear sense of the project, setting basic principle is similar to PID.)
    2011-06-22 21:18:52下载
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  • rk
    说明:  4阶龙格库塔解解微分方程,源程序的编写资料的详细功能(Runge kutta)
    2013-11-14 18:40:44下载
    积分:1
  • chap3_06_Narendra_MRAC_n1
    在自动控制系统的过程中,narendra稳定方程 持续时间 稳定时间 动态响应(In the process of automatic control system, narendra stability equation dynamic response settling time duration)
    2013-09-04 14:53:29下载
    积分:1
  • FSK
    FSK调制方式的SIMULINK仿真和完整的参数设置(FSK modulation of the SIMULINK simulation and a complete set of parameters)
    2009-04-27 20:52:05下载
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    Descriptor DAISY for Matlab in Windows
    2013-02-07 21:56:58下载
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    硕士论文:粘弹性介质地震波数值模拟。 震波在实际地层介质中传播与在理想的完全弹性介质中传播有许多不同之处,地层的粘滞性会损耗地震波能量,使其振幅衰减并且视频率逐渐降低。地震波的这种能量 衰减和频散,使得不能直接从地震数据上得到准确的地下信息和分辨率更高的图像。实 际的地层更接近于粘弹性介质,本论文主要探讨和研究了粘弹性介质中地震波传播的数 值模拟方法及其衰减规律。 (Thesis: viscoelastic medium seismic wave numerical simulation. The shock wave propagation in the formation medium and ideal perfectly elastic medium spread there are many differences, the viscosity of the strata will loss seismic energy, so that the amplitude attenuation and video rate gradually reduce. This energy of the seismic wave attenuation and dispersion makes accurate subsurface information and higher resolution images can not be obtained directly from the seismic data. Actual formation closer viscoelastic medium, this thesis is to explore and study the numerical simulation of seismic wave propagation in viscoelastic media and its decay law.)
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