Heats of adsorption of N-hexane by thermal gravimetry with differential scanning calorimetry (TG-DSC): A tool for textural characterization of pillared clays
J. Pires et al., Heats of adsorption of N-hexane by thermal gravimetry with differential scanning calorimetry (TG-DSC): A tool for textural characterization of pillared clays, CLAY CLAY M, 48(3), 2000, pp. 385-391
Microporous materials, (materials with pore sizes with widths <2 nm) were p
repared by pillaring of smectites obtained from different soil deposits. Th
e materials were prepared by intercalation with oligomeric cations of alumi
num, which were transformed to aluminum-oxide pillars by calcination. The a
dsorption of n-hexane in the pillared clays was studied by the determinatio
n of heats of adsorption. Heats of adsorption were measured using either a
static microcalorimeter or differential scanning calorimetry coupled with t
hermogravimetry (TG-DSC). In this latter case, two different procedures wer
e used that differ on the introduction of the (n-hexane) molecules that are
to be adsorbed. The results obtained by the (standard) static microcalorim
eter method and the TG-DSC method were compared. This comparison showed the
heats of adsorption obtained by TG-DSC are differential heats of adsorptio
n, and it showed the range of adsorption. Characterizing the texture of pil
lared clays, especially microporosity, is important for monitoring the inte
rcalation process and for determining potential applications of these mater
ials. Correlations between the obtained heats of adsorption and the dimensi
ons of micropores suggest that TG-DSC is a semi-quantitative method for cha
racterizing micropores in aluminum-pillared clays.