Abstract
The earlier work on the determination of the specific heats of lithium by the use of deLaunay’s model has been extended to sodium and potassium. A new technique has been introduced in which the contributions of the central and the outer parts of the Brillouin zone to
C
v
are calculated separately from different distribution densities of 8000 and 1000 points per zone, respectively. The agreement between the calculated and the experimental values of
C
v
has been found to be very good except at very low temperatures where the deviations can be ascribed to the presence of phase transformation. The effect of using a finer mesh of points on
C
v
has been examined. In order to get accurate values of
C
v
the density of points in the central region has to be increased considerably. In the outer region, however, a low density of eight points per zone as in Raman’s theory is found to be reasonably satisfactory.
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