Lord Kelvin: An account of his scientific life and workGray, Andrew
Science
Lord Kelvin: An account of his scientific life and work
Gray, Andrew
Kelvin, William Thomson, Baron, 1824-1907
From the first law Thomson obtained another fundamental equation. For
every substance there is a relation connecting the pressure p (or more
generally the stress of some type), the volume v (or the configuration
according to the specified stress), and the temperature. We may
therefore take arbitrary changes of any two of these quantities: the
relation referred to will give the corresponding change of the third.
Thomson chose v and t as the quantities to be varied, and supposed them
to sustain arbitrary small changes dv and dt in consequence of the
passage of heat to the substance from without. The amount of heat taken
in is Mdv + Ndt, where Mdv and Ndt are heats required for the changes
taken separately. But the substance expanding through dv does external
work pdv. Thus the net amount of energy given to the substance from
without is Mdv + Ndt - pdv or (M - p)dv + Ndt; and if the substance
is made to pass through a cycle of changes so that it returns to the
physical state from which it started, the whole energy received in the
cycle must be zero. From this it follows that the rate of variation of
M - p when the temperature but not the volume varies, is equal to the
rate of variation of N when the volume but not the temperature varies.
To see that this relation holds, the reader unacquainted with the
properties of perfect differentials may proceed thus. Let the substance
be subjected to the infinitesimal closed cycle of changes defined by (1)
a variation consisting of the simultaneous changes dv, dt of volume and
temperature, (2) a variation -dv of volume only, (3) a variation -dt of
temperature only. M - p and N vary so as to have definite values for
the beginning and end of each step, and the proper mean values can
be written down for each step at once, and therefore the value of
(M - p)dv + Ndt obtained. Adding together these values for the three
steps we get the integral for the cycle. The condition that this should
vanish is at once seen to be the relation stated above.
This result combined with the equation A derived from the second law,
gives an important expression for Carnot's function.
We shall not pursue this discussion further: so much is given to make
clear how certain results as to the physical properties of substances
were obtained, and to explain Thomson's scale of absolute thermodynamic
temperature, which is by far the most important discovery within the
range of theoretical thermodynamics.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account