The heat capacities of diamond, graphite, and the fullerenes C-60 and
C-70, are compared and linked to their approximate vibrational spectra
. Because all the allotropes have the chemical composition C, their ul
timate heat capacity is the Dunlog-Petit value 3R = 24.9 J K-1 mol(-1)
. At low temperatures (0-50 K), the fullerenes have a much higher heat
capacity than the other two allotropes. As the temperature is increas
ed, graphite and the fullerenes approach approximately equal heat capa
cities. Up to 1000 K, diamond has a lower heat capacity, but then, bec
ause of its weaker C-C bonds compared to the conjugated double bonds i
n graphite and the fullerenes, it exceeds the heat capacities of the l
atter. Fullerenes have crystal to plastic-crystal transitions in the r
egion 250-350 K with entropies in agreement with the orientational ent
ropy increase derivable from Walden's rule. Their sublimation pressure
s reach atmospheric pressure at about 1500 K, and the entropies of tra
nsition, when corrected for the entropy of fusion (Richards' rule), ob
ey Trouton's rule. Carbon is thus a textbook example for the differenc
es in thermal behavior possible as a function of chemical bonding and
structure.