Free access article
Eur. Phys. J. B 7, 19-36
Phase transitions of fluids confined in porous silicon:
A differential calorimetry investigation
C. Faivre - D. Bellet - G. Dolino
Laboratoire de Spectrométrie Physique
,
Université Joseph Fourier (Grenoble-I),
B.P. 87,
38402 Saint Martin d'Hères Cedex, France
Daniel.BELLET@inpg.fr
Received: 11 May 1998 / Revised and Accepted: 29 July 1998
Abstract
The phase transitions of non-polar organic fluids and of water, confined in the pores
of porous silicon samples, were investigated by Differential Scanning Calorimetry
(DSC). Two types of PS samples (p- and p+ type) with different pore size and
morphology were used (with spherical pores with a radius of about 1.5 nm and
cylindrical shape with a radius of about 4 nm respectively). The DSC results clearly
show that the smaller the pores are, the 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 small particles and confined fluids is presented and used to interpret
and discuss our DSC results. The effects of the chemical dissolution as well as the
influence of anodization time are presented, showing that thick p+ type porous
silicon layers are non-homogeneous. The DSC technique which was used for the first
time to investigate fluids confined in porous silicon, enables us to deduce original
information, such as the pore size distribution, the decrease in the freezing
temperature of confined water, and the thickness of non-freezing liquid layer at the
pore wall surface.
PACS
81.65.-b Surface treatments -
64.70.Dv Solid-liquid transitions -
07.20.Fw Calorimetry
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Copyright EDP Sciences, Società Italiana di Fisica, Springer-Verlag



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