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Hi Richard, Please re-read my comment. I understand the self sustaining concept. It is the getting started part that I have trouble with. I know about auto generators too. To support your version, there must exist some residual magnetism in the molten core from day one. OR something has to "twang" the core to get it started - like the experiment using the molten sodium. Steve k.9,d'c\i "Richard Clark" wrote in message ... On Thu, 20 Nov 2003 17:46:55 -0600, "Steve Nosko" wrote: The NOVA the other evening said it is something like 200 to 700 million years, I believe. (May have the multiplier wrong, but the significant digit is what they said) Off by three orders of magnitude. The average (100K-200K) is lower than what has been observed (700K) since the last flip. OK. I knew I had the digits right. The NOVA was not too clear about how a rotating molten conductor creates a field, but once you get one, I can understand how the field and current in the core can cross couple and keep each other going. Hi Steve, This is an example of how generators used to work (when the battery was dead). The "residual" magnetism within the iron bulk presented enough excitation for a formerly motionless coil to cause current to be generated. That current was then used in the excitation coil to build a field that in turn created more current for a larger excitation field - and so on. The term in electronics is called variously as "bootstrapping," "fly-back," "buck-boosting," or "bucking." 73's Richard Clark, KB7QHC |
On Fri, 21 Nov 2003 15:51:29 -0600, "Steve Nosko"
wrote: To support your version, there must exist some residual magnetism in the molten core from day one. Hi Steve, The "first" magnetism could have been "twanged" exactly as you expressed but didn't follow through with. Any number of meteor strikes could have done that, if in fact it wasn't already there from the primordial conditions of plasmas and moving charges during the cosmic soup coagulating into the initial mass. This, after all, was bred from a condition of extreme heat, escaping now to a Mars condition of a frozen core in some several billion years hence. 73's Richard Clark, KB7QHC |
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