Isothermal-isobaric ensemble Monte Carlo simulations are used to study the
melting of Mor se solids. At a given pressure, the temperature at which the
solid ceases to be metastable and also the fractional changes in density a
nd potential energy increase with decreasing range of the Morse pair potent
ial. The structural properties of the liquid and solid phases vary signific
antly with the range. The longer range, softer potentials are associated wi
th increased densities and cohesive energies in both the solid and liquid p
hases. The extent of local disorder associated with lattice sites in the so
lid phase, as measured by the Lindemann and bond orientational order parame
ters, increases with increasing range of the pair potential.