PSN-L Email List Message
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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