Skippy's post:
Off-topic, I know, sorry:
The "iron see-through" label was one that usually got applied to VLF's with high operating frequency, such as the 100 kHz Compass range, like the Yukon. The idea was the high frequency only penetrated iron items to a tiny depth ( ferromagnetic materials have very small skin depths, and at 100K it's really small ) so the iron targets didn't in turn create a strong magnetic field of their own, and they didn't distort the detectors field in the ground so much, thus allowing the possibility of finding non-ferrous items nearby - items that would be hidden/masked by using a more conventional lower freq VLF.
This is an interesting post, that could be the beginning of a useful discussion.
We know that PI detectors "have an affinity" for magnetic targets.
I believe that magnetic targets have 2 distinct Tau's. An initial short decay and then a long decay.
How does this happen?
Lets look at it a bit closer.
Off-topic, I know, sorry:
The "iron see-through" label was one that usually got applied to VLF's with high operating frequency, such as the 100 kHz Compass range, like the Yukon. The idea was the high frequency only penetrated iron items to a tiny depth ( ferromagnetic materials have very small skin depths, and at 100K it's really small ) so the iron targets didn't in turn create a strong magnetic field of their own, and they didn't distort the detectors field in the ground so much, thus allowing the possibility of finding non-ferrous items nearby - items that would be hidden/masked by using a more conventional lower freq VLF.
This is an interesting post, that could be the beginning of a useful discussion.
We know that PI detectors "have an affinity" for magnetic targets.
I believe that magnetic targets have 2 distinct Tau's. An initial short decay and then a long decay.
How does this happen?
Lets look at it a bit closer.
Comment