Originally posted by waltr
View Post
The way EFE works is that you take an initial (main) sample after (for example) 15us. Then you take a second (EFE) sample much later (for example) 200us. If there is a signal due to the Earth's magnetic filed, it will have substantially the same amplitude in both samples. However, any target signal will be much stronger in the main sample than it is in the second sample. Therefore, subtracting the second sample from the main sample will leave only the target signal. i.e. the effect of moving the coil in the Earth's magnetic filed will have been eliminated. This method requires both the main and second samples to have the samesample width.
Comment