De. Petrakis et al., CONTROLLED MODULATION OF MESOPOROSITIES IN METAL (M=AL, FE) PHOSPHATESOLIDS, Colloids and surfaces. A, Physicochemical and engineering aspects, 90(2-3), 1994, pp. 191-202
Mesoporous solids which posses average pore diameters between 7 and 20
nm, depending on the composition, have been prepared. The solids have
the general formula Al100P(x)M20 where M = Al or Fe, and x = 0, 4.5,
9, 18, 36, 72 or 144. The initial addition of phosphorus as phosphate
transforms the originally crystalline oxide/oxides into amorphous soli
ds. These amorphous materials posses a narrow pore size distribution:
80-90% of the pores lie within 1-2 nm of the average pore diameter. Su
bsequent incremental amounts of phosphorus transform the material into
a crystalline solid whilst the pore size distribution becomes much wi
der and the maximum moves towards larger pore diameters. Substitution
of 20% of the aluminium by iron results, at a low phosphorus content,
in pores with smaller pore volumes and smaller surface areas. The data
in the dV(p)/dD(p) = f(D(p)) graphs, where V(p) is the incremental po
re volume and D(p) is the average pore diameter, can be approximated u
sing an admixture of Gaussian and Lorentzian curves. For low phosphoru
s contents the dV(p)/dD(p) = f(D(p)) curves have a mainly Gaussian pro
file but the gradual addition of phosphorus transforms them to Lorentz
ian-type curves. An attempt to approximate the histograms dV(p) = f(D(
p)) with the minimum number of distribution curves made up of the corr
esponding Gaussian and Lorentzian components indicates that each succe
ssive addition of phosphorus creates a dominant new pore component at
a larger pore diameter. At the same time, the components at smaller po
re diameters are diminished and eventually disappear as more phosphoru
s is added.