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Subject: Re: diamagnetic levitation seismometer possibility
From: Charles R Patton charles.r.patton@........
Date: Mon, 09 Jul 2012 10:49:45 -0700


Interesting observations about the possibility of diamagnetic 
roughness.  This brings up two observations:
1) By the current theories of magnetic flux lines as I understand them, 
there is no possibility for them to exhibit "kinks or roughness" at the 
scales and method of field generation we're discussing.  (The non-smooth 
examples I'm thinking of are of solar magnetic flux that also include 
ion current flow,  tokamaks, etc.)

2) So that leaves two possibilities in my mind:
     a) The magnetic field is undergoing slight changes in field 
strength with the actual counterpressure of the carbon being levitated.  
Hard to imagine with the relative strengths of the permanent magnets -- 
but still a possibility.  I've never heard of such a thing myself, but 
what do I know?  Maybe a PhD thesis here?
     b) The carbon diamagnetic properties exhibit a domain phenomenon in 
a similar vein to the ferromagnetic properties of iron.  Again, " I've 
never heard of such a thing, but what do I know?  Maybe a PhD thesis here?"

In a more blue sky way of reasoning, project the following thoughts:
1) Dr. Randall Peters has brought to this list the interesting concepts 
of mesoscale damping.  Part of what I take away from that concept is 
that as we burrow down in dimension, the concept of an amorphous solid 
with smooth mathematically described properties breaks down.  Just as 
ferrous magnetics were thought to be smooth, the discovery of Barkhausen 
noise was discovered early on to be the individual magnetic domains 
switching.  Diamagnetic properties come from electron properties of 
masses of atoms just as the ferrous magnetic properties do.  So, atoms 
can move within a "solid".  The most stable solids are crystalline in 
nature, where the atoms are locked in both space and orientation.    The 
big question, "Would a crystalline diamagnetic solid exhibit this 
magnetIc "roughness", perhaps equivalent to the Barkhausen noise?   The 
experiment to perform here is to use a Barkhausen test setup, but 
substitute carbon for iron.

Just a few idle thoughts for the morning.
Charles R. Patton


On 7/9/2012 9:34 AM, chrisatupw@....... wrote:
> From: Bob McClure bobmcclure90@......... 
> Sent: Mon, 9 Jul 2012 15:02
> Subject: Re: diamagnetic levitation seismometer possibility
> Hi Randall,
> I, too, have carried out diamagnetic levitation experiments similar to 
> those by Meredith Lamb. Although the large amplitude motion looks 
> smooth and frictionless, what I concluded for very small amplitudes, 
> such is not the case. The supporting magnetic field has small-scale 
> roughness, and the levitated graphite tends to hung up in the hills 
> and valleys of the resulting force.
>
> Hi Bob,
>     Did you ever try putting a transformer lamination on top of the 
> magnets to smooth out any field irregularities ?
>     Regards,
>     Chris Chapman



  
    
  
  
    
Interesting observations about the possibility of diamagnetic roughness.  This brings up two observations:
1) By the current theories of magnetic flux lines as I understand them, there is no possibility for them to exhibit "kinks or roughness" at the scales and method of field generation we're discussing.  (The non-smooth examples I'm thinking of are of solar magnetic flux that also include ion current flow,  tokamaks, etc.)

2) So that leaves two possibilities in my mind:
    a) The magnetic field is undergoing slight changes in field strength with the actual counterpressure of the carbon being levitated.  Hard to imagine with the relative strengths of the permanent magnets -- but still a possibility.  I've never heard of such a thing myself, but what do I know?  Maybe a PhD thesis here?
    b) The carbon diamagnetic properties exhibit a domain phenomenon in a similar vein to the ferromagnetic properties of iron.  Again, " I've never heard of such a thing, but what do I know?  Maybe a PhD thesis here?" 

In a more blue sky way of reasoning, project the following thoughts:
1) Dr. Randall Peters has brought to this list the interesting concepts of mesoscale damping.  Part of what I take away from that concept is that as we burrow down in dimension, the concept of an amorphous solid with smooth mathematically described properties breaks down.  Just as ferrous magnetics were thought to be smooth, the discovery of Barkhausen noise was discovered early on to be the individual magnetic domains switching.  Diamagnetic  properties come from electron properties of masses of atoms just as the ferrous magnetic properties do.  So, atoms can move within a "solid".  The most stable solids are crystalline in nature, where the atoms are locked in both space and orientation.    The big question, "Would a crystalline diamagnetic solid exhibit this magnetIc "roughness", perhaps equivalent to the Barkhausen noise?    The experiment to perform here is to use a Barkhausen test setup, but substitute carbon for iron.     

Just a few idle thoughts for the morning.
Charles R. Patton
 

On 7/9/2012 9:34 AM, chrisatupw@....... wrote:
From: Bob McClure bobmcclure90@.........
Sent: Mon, 9 Jul 2012 15:02
Subject: Re: diamagnetic levitation seismometer possibility
Hi Randall,
 
I, too, have carried out diamagnetic levitation experiments similar to those by Meredith Lamb. Although the large amplitude motion looks smooth and frictionless, what I concluded for very small amplitudes, such is not the case. The supporting magnetic field has small-scale roughness, and the levitated graphite tends to hung up in the hills and valleys of the resulting force.

Hi Bob,
 
    Did you ever try putting a transformer lamination on top of the magnets to smooth out any field irregularities ?
    Regards,
    Chris Chapman
 
 



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