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QuoteThere are dozens of different measurements that can be used to characterize a componet and when the meaning of these is not fully understood it gives people the impression that maybe there are new types of measurement yet to be discovered that show things that all of the current ones don't show.The truth is that there will be new types of measurements but they will show the same thing the already existing types of measurement show.Translation - We already know everything - the earth is flat.My point was not that there might be new types of measurements - but new things TO measure. What if at some point we find something that dismisses the need to assume systems are linear (IMO a bad assumption since NO system is perfectly linear - much less when having to interact with other dynamic, non-linear systems)? What if the proof turns out to be different than the assumption? Yes, what we know and assume now gets us pretty close, but not exact - and there is no 'e' to define that error as there is in calculus. Is it even a constant 'e'?Bryan
There are dozens of different measurements that can be used to characterize a componet and when the meaning of these is not fully understood it gives people the impression that maybe there are new types of measurement yet to be discovered that show things that all of the current ones don't show.The truth is that there will be new types of measurements but they will show the same thing the already existing types of measurement show.
It is very common to hear someone commenting yeah the frequency response is flat but what about the time domain, you need to look at it's square wave resonse to see how it handles transients.
Quote from: Daryl on 16 Apr 2007, 02:57 pmIt is very common to hear someone commenting yeah the frequency response is flat but what about the time domain, you need to look at it's square wave resonse to see how it handles transients.For any element with a nonlinear characteristic, this is true. Remember that a function has to be linear for one to transfer something from the frequency domain to the time domain (or vice versa). For instance, what's the Fourier transform of x^2 or log(x)? There isn't one, because these are nonlinear functions and the rule of supposition does not work for nonlinear functions (in other words, no matter how many sine/cosine functions you use, you cannot replicate a nonlinear function through the use a sine/cosine functions).
Then you're wrong. The system HAS TO BE linear and time invariant for a Fourier transform to apply.
For any element with a nonlinear characteristic, this is true. Remember that a function has to be linear for one to transfer something from the frequency domain to the time domain (or vice versa). For instance, what's the Fourier transform of x^2 or log(x)? There isn't one, because these are nonlinear functions and the rule of supposition does not work for nonlinear functions (in other words, no matter how many sine/cosine functions you use, you cannot replicate a nonlinear function through the use a sine/cosine functions).
This is so tedious. ctviggen is talking about the relationship between the value of the output and the input of a system at a given time. Not a function from time to a value.
You take the FT of the output and compare it to FT of the input; it's as simple as that.
Again - there is nothing wrong with or inapplicable about Fourier analysis no matter how non-linear the system is. As has been emphasized repeatedly the FT is completely equivalent to the time domain, period.
Well, more specifically, you divide the FT of the output by the FT of the input. So suppose I input a 1V sinewave at 1 khz, and the output is 1v at 1 kHz, and 0.00001V at 2kHz, what is the result of this operation at 2 kHz?
Yes. For signals. But you are attempting to apply this fact to the frequency RESPONSE of a SYSTEM which is something different. (Hopefully the above example might give you pause to think about why.)
I'm sorry but I don't have much more to say on this. Not understanding is one thing but insulting other people as a result is completely another.