TY - JOUR
T1 - Revisiting the nature of the acidity in chabazite-related silicoaluminophosphates
T2 - Combined FTIR and29Si MAS NMR study
AU - Martins, G. A.V.
AU - Berlier, G.
AU - Coluccia, S.
AU - Pastore, H. O.
AU - Superti, G. B.
AU - Gatti, G.
AU - Marchese, L.
PY - 2007/1/11
Y1 - 2007/1/11
N2 - The acidity of crystalline silicoaluminophosphates with chabazite-related structure (CHA), was studied by using CO and C2H4 probe molecules. SAPO-34 samples with similar silicon concentrations prepared using different structure-directing agents have been studied, and the results have been compared with a silicoaluminophosphate, CAL-1, having a similar structure and much higher silicon concentration. A detailed analysis of the FTIR spectra in the OH stretching region, and of the downward shift of the OH bands upon CO and C2H4 adsorption, evidenced the presence of three distinct acid sites (named OHA, OHB, and OHC) absorbing at 3631, 3617, and 3600 cm-1, respectively (average values). A multipeak curve-fitting approach, along with hydrogen bond theory, following Makarova et al. (J. Phys. Chem. 1994, 98, 3619), allowed us to compute the fraction of the three sites. While the two main components OHA and OHC were already reported and explained in terms of different crystallographic positions, the existence and nature of the OHB site are here discussed for the first time. Protons at the OHB sites are shown to have an acidity (downward shift upon CO adsorption of ca. 330 cm -1) comparable to that usually measured in zeolites, aluminosilicate crystalline materials, which are known to possess stronger acidity than SAPOs. To our knowledge, this is the first clearcut experimental evidence that such strong acid sites are present in SAPO.materials. A combined FTIR and 29Si MAS NMR study permitted explaining the strong acidity of OHB sites in terms of protons either at the borders of silica patches/islands or inside aluminosilicate domains.
AB - The acidity of crystalline silicoaluminophosphates with chabazite-related structure (CHA), was studied by using CO and C2H4 probe molecules. SAPO-34 samples with similar silicon concentrations prepared using different structure-directing agents have been studied, and the results have been compared with a silicoaluminophosphate, CAL-1, having a similar structure and much higher silicon concentration. A detailed analysis of the FTIR spectra in the OH stretching region, and of the downward shift of the OH bands upon CO and C2H4 adsorption, evidenced the presence of three distinct acid sites (named OHA, OHB, and OHC) absorbing at 3631, 3617, and 3600 cm-1, respectively (average values). A multipeak curve-fitting approach, along with hydrogen bond theory, following Makarova et al. (J. Phys. Chem. 1994, 98, 3619), allowed us to compute the fraction of the three sites. While the two main components OHA and OHC were already reported and explained in terms of different crystallographic positions, the existence and nature of the OHB site are here discussed for the first time. Protons at the OHB sites are shown to have an acidity (downward shift upon CO adsorption of ca. 330 cm -1) comparable to that usually measured in zeolites, aluminosilicate crystalline materials, which are known to possess stronger acidity than SAPOs. To our knowledge, this is the first clearcut experimental evidence that such strong acid sites are present in SAPO.materials. A combined FTIR and 29Si MAS NMR study permitted explaining the strong acidity of OHB sites in terms of protons either at the borders of silica patches/islands or inside aluminosilicate domains.
UR - https://www.scopus.com/pages/publications/33847655632
U2 - 10.1021/jp063921q
DO - 10.1021/jp063921q
M3 - Article
SN - 1932-7447
VL - 111
SP - 330
EP - 339
JO - Journal of Physical Chemistry C
JF - Journal of Physical Chemistry C
IS - 1
ER -