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Re: CONSERVATION OF ENERGY



Tom ("The Amateur") Wayburn writes:

Now, John, the idea of "internal work" is absolutely out of the
question in my development of thermophysics. Work is the transfer of
energy (unaccompanied by entropy) through a control surface. ...

1. I don't see any reason to impugn the concept of internal work.
If one defines work as force dotted into the displacement of the
associated point of application, then internal forces do perform work
and, unlike net internal force which is always zero due to pairwise
cancellation, no such cancellation occurs for internal work. As I
mentioned in the post to which you responded, when a gas expands, it
does so against weakly attractive intermolecular forces. In the process
these forces do negative net (internal) work and that work is manifest
(internally) in the associated decrease in the total kinetic energy of
the molecules.

2. I don't think you can define work very accurately as "the transfer of
energy (unaccompanied by entropy) through a control surface." There are
lot's of situations (all irreversible) in which work is the only energy
transfer process going on and in which the entropy changes.

I have no problem with internal potential energy. At least I don't
think I do. I suppose a system composed of M kgs of metal sliding
horizontally upon a large metal slab with initial velocity V, relative to
the lab coordinates, should have 0.5MV^2 added to its "regular"
(ordinary?) internal energy, U. Eh? Likewise if the system is a
compressed spring that can be released by wishing it to be released ...
? Or a mass of M kgs 100 meters above the lab floor ... ?

Of the three examples you give above, only the compressed spring
qualifies in my mind as an example of internal potential energy. The
first example is bulk translational energy that I don't even like to
consider "internal," but is, in any event, certainly not internal
*potential* energy. The third example does not involve "internal"
potential energy unless you define the system to be the mass *and* the
earth.

John
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A. John Mallinckrodt http://www.intranet.csupomona.edu/~ajm
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