The phase transitions of non-polar organic fluids and of water, confined in
the pores of porous silicon samples, were investigated by Differential Sca
nning Calorimetry (DSC). Two types of PS samples (p(-) and p(+) type) with
different pore size and morphology were used (with spherical pores with a r
adius of about 1.5 nm and cylindrical shape with a radius of about 4 nm res
pectively). The DSC results clearly show that the smaller the pores are, th
e larger is the decrease in the transition temperature. Moreover, a larger
hysteresis between melting and freezing is observed for p(+) type than for
p(-) type samples. A critical review of the thermodynamical properties of s
mall particles and confined fluids is presented and used to interpret and d
iscuss our DSC results. The effects of the chemical dissolution as well as
the influence of anodization time are presented, showing that thick p(+) ty
pe porous silicon layers are non-homogeneous. The DSC technique which was u
sed for the first time to investigate fluids confined in porous silicon, en
ables us to deduce original information, such as the pore size distribution
, the decrease in the freezing temperature of confined water, and the thick
ness of non-freezing liquid layer at the pore wall surface.