[计] 解卷积
解卷积(Deconvolution)就是利用数学算法将色谱未分离的组分重新解析开,还原它们最真实的质谱信息。
[地质] 反褶积
...反褶积(deconvolution)就是反滤波(inverse filter),是最常用的地震资料数字处理方法之一,可用于叠前资料处理,也可用于叠后资料处理.
[计] 去卷积
去卷积(Deconvolution)是卷积计算的逆过程,是根据输出信号和系统响应来确定输入信号。
反卷积
...糖及非葡萄糖胰岛素刺激机体胰岛素释放,根据刺激后外周血胰岛素浓度及个体胰岛素分布清除动力学参数,采用反卷积(Deconvolution)的数学模型,计算经肝门脉系统向外周传输胰岛素的速率和量。。
In mathematics, deconvolution is an algorithm-based process used to reverse the effects of convolution on recorded data. The concept of deconvolution is widely used in the techniques of signal processing and image processing. Because these techniques are in turn widely used in many scientific and engineering disciplines, deconvolution finds many applications.In general, the object of deconvolution is to find the solution of a convolution equation of the form:Usually, h is some recorded signal, and ƒ is some signal that we wish to recover, but has been convolved with some other signal g before we recorded it. The function g might represent the transfer function of an instrument or a driving force that was applied to a physical system. If we know g, or at least know the form of g, then we can perform deterministic deconvolution. However, if we do not know g in advance, then we need to estimate it. This is most often done using methods of statistical estimation.In physical measurements, the situation is usually closer toIn this case ε is noise that has entered our recorded signal. If we assume that a noisy signal or image is noiseless when we try to make a statistical estimate of g, our estimate will be incorrect. In turn, our estimate of ƒ will also be incorrect. The lower the signal-to-noise ratio, the worse our estimate of the deconvolved signal will be. That is the reason why inverse filtering the signal is usually not a good solution. However, if we have at least some knowledge of the type of noise in the data (for example, white noise), we may be able to improve the estimate of ƒ through techniques such as Wiener deconvolution.The foundations for deconvolution and time-series analysis were largely laid by Norbert Wiener of the Massachusetts Institute of Technology in his book Extrapolation, Interpolation, and Smoothing of Stationary Time Series (1949). The book was based on work Wiener had done during World War II but that had been classified at the time. Some of the early attempts to apply these theories were in the fields of weather forecasting and economics.