“…The shift, now known as the Gibbs-Thomson effect, has been studied with a variety of substances dispersed on inert substrates or confined in porous media. A sampling is given in the references in four groups: weakly interacting molecular species such as rare gas atoms in porous media ͑Brewer et Tell and Maris, 1983;Liezhao et al, 1986;Shimoda et al, 1986;Kondo et al, 1987;Brown et al, 1988;Bruschi et al, 1988;Hiroi et al, 1989;Jackson and McKenna, 1990;Rall et al, 1991;Duffy et al, 1995;Beaudoin et al, 1996͒, ice in porous media ͑Blachere andYoung, 1972;Gay et al, 1992;Maruyama et al, 1992;Ishizaki et al, 1996;Mori et al, 1996͒, dispersed metal particles ͑Takagi, 1954Gladkich et al, 1966;Wronski, 1967;Coombes, 1972;Peppiatt and Sambles, 1975;Buffat andBorel, 1976͒, andice in soils ͑Hoekstra andDelaney, 1974;Konrad and Morgenstern, 1981;Smith and Tice, 1988͒. The typical behavior of the first group is that melting begins appreciably below the bulk transition when the pores are filled. Although the first one or two adsorbed layers prefreeze, due to substrate attractive forces stronger than the interactions within the material.…”