
5.4 Defining the Kelvin Temperature Scale 191
If a reversible power cycle were operated in the opposite direction as a refrigeration or
heat pump cycle, the magnitudes of the energy transfers Q
C
and Q
H
would remain the same,
but the energy transfers would be oppositely directed. Accordingly, Eq. 5.6 applies to each
type of cycle considered thus far, provided the system undergoing the cycle operates between
two thermal reservoirs and the cycle is reversible.
Equation 5.6 gives only a ratio of temperatures. To complete the definition of the Kelvin scale,
it is necessary to proceed as in Sec. 1.6 by assigning the value 273.16 K to the temperature at
the triple point of water. Then, if a reversible cycle is operated between a reservoir at 273.16 K
and another reservoir at temperature T, the two temperatures are related according to
(5.7)
where Q
tp
and Q are the heat transfers between the cycle and reservoirs at 273.16 K and tem-
perature T, respectively. In the present case, the heat transfer Q plays the role of the ther-
mometric property. However, since the performance of a reversible cycle is independent of
the makeup of the system executing the cycle, the definition of temperature given by Eq. 5.7
depends in no way on the properties of any substance or class of substances.
In Sec. 1.6 we noted that the Kelvin scale has a zero of 0 K, and lower temperatures than
this are not defined. Let us take up these points by considering a reversible power cycle op-
erating between reservoirs at 273.16 K and a lower temperature T. Referring to Eq. 5.7, we
know that the energy rejected from the cycle by heat transfer Q would not be negative, so T
must be nonnegative. Equation 5.7 also shows that the smaller the value of Q, the lower the
value of T, and conversely. Accordingly, as Q approaches zero the temperature T approaches
zero. It can be concluded that a temperature of zero on the Kelvin scale is the lowest con-
ceivable temperature. This temperature is called the absolute zero, and the Kelvin scale is
called an absolute temperature scale.
INTERNATIONAL TEMPERATURE SCALE
When numerical values of the thermodynamic temperature are to be determined, it is not
possible to use reversible cycles, for these exist only in our imaginations. However, temper-
atures evaluated using the constant-volume gas thermometer introduced in Sec. 1.6 are iden-
tical to those of the Kelvin scale in the range of temperatures where the gas thermometer can
be used. Other empirical approaches can be employed for temperatures above and below the
range accessible to gas thermometry. The Kelvin scale provides a continuous definition of
temperature valid over all ranges and provides an essential connection between the several
empirical measures of temperature.
To provide a standard for temperature measurement taking into account both theoretical
and practical considerations, the International Temperature Scale (ITS) was adopted in 1927.
This scale has been refined and extended in several revisions, most recently in 1990. The
International Temperature Scale of 1990 (ITS-90) is defined in such a way that the temper-
ature measured on it conforms with the thermodynamic temperature, the unit of which is the
kelvin, to within the limits of accuracy of measurement obtainable in 1990. The ITS-90 is
based on the assigned values of temperature of a number of reproducible fixed points
(Table 5.1). Interpolation between the fixed-point temperatures is accomplished by formulas
that give the relation between readings of standard instruments and values of the ITS. In the
range from 0.65 to 5.0 K, ITS-90 is defined by equations giving the temperature as functions
of the vapor pressures of particular helium isotopes. The range from 3.0 to 24.5561 K is
based on measurements using a helium constant-volume gas thermometer. In the range from
13.8033 to 1234.93 K, ITS-90 is defined by means of certain platinum resistance ther-
mometers. Above 1234.9 K the temperature is defined using Planck’s equation for blackbody
radiation and measurements of the intensity of visible-spectrum radiation.
T 273.16 a
Q
Q
tp
b
rev
cycle