Chris, the idea of inducing eddy current into a dime that is 12 inches from the coil and then the dime induces current into the receiver is takes a giant leap of faith to say the least. I think there is a much better way to consider what actually takes place. Here is something I threw together while taking a shower for a person like yourself that understands electronics.
Consider a transformer with a single primary and secondary and the primary being pulsed by a square wave. We can monitor the primary and secondary with an oscilloscope and air as the core and depending of design see a fairly nice square wave in both. I think of an infinite variable core with metal particles embedded. It is pretty easy to visualize that we can see and analyze signal in the secondary of the transformer compared to the signal in the primary. The various electrical parameters of the transformer and of the metal particles are going to paint a pretty clear picture of what the core is doing. What are fairly constant are the soil or base core material and what changes abruptly are the metal particles. We then know to reject the constant parameter and only look at the abrupt changes. What we have done is reject the constant parameter of the core.
The data is in serial form as it enters the input and is amplified and fed to six demodulators. I think we have to keep in mine we are dealing with one signal at a time which is demodulated into 3 frequency ranges for high, mid, and low, filtered and then processed. It would be nice to overlook the 28 frequencies but we really cannot in my opinion since metals respond differently to different frequencies.
Now we sample the secondary so many times, a sequence, to see what the signal looks like. Use precise time measurement we get a very good idea of what the metal is in the core that causes the abnormality in the signal. We can store constant core data as instantaneous and historical in that we look at the constant core data at an instant in time, the core data that just went from instantaneous to historical and predict the future core data. We need some algorithms to tell the processor what to do with the data, store some lookup tables to compare the data to, generate an audio and visual presentation and then I think we have the basics of the detector.
The other function are mostly to help us to get a good look at the core data iron particles and deal with the motion of the coil to feed the data into the receiver. Audio, Fast, Deep, and the like are for that purpose. It is picking those good targets from the core mixed in with trash metals so we need to be able to adjust a few things to do that. As a last thought consider a piece of iron in the core that is fairly large and several particles of other metals that vary the core. That large piece of iron is going to be a problem. It is not that we don
Consider a transformer with a single primary and secondary and the primary being pulsed by a square wave. We can monitor the primary and secondary with an oscilloscope and air as the core and depending of design see a fairly nice square wave in both. I think of an infinite variable core with metal particles embedded. It is pretty easy to visualize that we can see and analyze signal in the secondary of the transformer compared to the signal in the primary. The various electrical parameters of the transformer and of the metal particles are going to paint a pretty clear picture of what the core is doing. What are fairly constant are the soil or base core material and what changes abruptly are the metal particles. We then know to reject the constant parameter and only look at the abrupt changes. What we have done is reject the constant parameter of the core.
The data is in serial form as it enters the input and is amplified and fed to six demodulators. I think we have to keep in mine we are dealing with one signal at a time which is demodulated into 3 frequency ranges for high, mid, and low, filtered and then processed. It would be nice to overlook the 28 frequencies but we really cannot in my opinion since metals respond differently to different frequencies.
Now we sample the secondary so many times, a sequence, to see what the signal looks like. Use precise time measurement we get a very good idea of what the metal is in the core that causes the abnormality in the signal. We can store constant core data as instantaneous and historical in that we look at the constant core data at an instant in time, the core data that just went from instantaneous to historical and predict the future core data. We need some algorithms to tell the processor what to do with the data, store some lookup tables to compare the data to, generate an audio and visual presentation and then I think we have the basics of the detector.
The other function are mostly to help us to get a good look at the core data iron particles and deal with the motion of the coil to feed the data into the receiver. Audio, Fast, Deep, and the like are for that purpose. It is picking those good targets from the core mixed in with trash metals so we need to be able to adjust a few things to do that. As a last thought consider a piece of iron in the core that is fairly large and several particles of other metals that vary the core. That large piece of iron is going to be a problem. It is not that we don