Meanwhile if we revisit the ferrite pole material specification it looks like it looses quite a bit of initial permeability at fileds as low as 100mT:
https://www.ferroxcube.com/upload/me...le/MDS/3b1.pdf
(it is not very obvious to read from the B-H curve provided as you need to look at the B-H curve slope versus B value)
https://www.ferroxcube.com/upload/me...le/MDS/3b1.pdf
(it is not very obvious to read from the B-H curve provided as you need to look at the B-H curve slope versus B value)
https://www.mag-inc.com/Media/Magnet...7.pdf?ext=.pdf
For this special high permeability ferrite, µ drops from the initial value of around 20000 to below 10 at an H-field of 1000A/m, corresponding to only 13Gauss or 1.3mT. But these measurements are taken in a laboratory situation, where the material is placed in a uniform H-field.
The actual B and H values inside a PU core vary from point to point and are practically impossible to measure. Consequently core sections closer to the magnet may already be in saturation while regions further away don't.
Of course it makes no sense to use such extremely high µ materials in PU cores. A change from µ=20000 to µ=2000 will barely be noticeable. But a change from µ=200 to µ=20 will.
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