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Infrared spectroscopic evidence for two ways of adsorbed CO coordination. / Tsyganenko, A. A.; Otero Arean, C.; Escalona Platero, E.

In: Studies in Surface Science and Catalysis, Vol. 130 D, 01.01.2000, p. 3143-3148.

Research output: Contribution to journalArticlepeer-review

Harvard

Tsyganenko, AA, Otero Arean, C & Escalona Platero, E 2000, 'Infrared spectroscopic evidence for two ways of adsorbed CO coordination', Studies in Surface Science and Catalysis, vol. 130 D, pp. 3143-3148.

APA

Tsyganenko, A. A., Otero Arean, C., & Escalona Platero, E. (2000). Infrared spectroscopic evidence for two ways of adsorbed CO coordination. Studies in Surface Science and Catalysis, 130 D, 3143-3148.

Vancouver

Tsyganenko AA, Otero Arean C, Escalona Platero E. Infrared spectroscopic evidence for two ways of adsorbed CO coordination. Studies in Surface Science and Catalysis. 2000 Jan 1;130 D:3143-3148.

Author

Tsyganenko, A. A. ; Otero Arean, C. ; Escalona Platero, E. / Infrared spectroscopic evidence for two ways of adsorbed CO coordination. In: Studies in Surface Science and Catalysis. 2000 ; Vol. 130 D. pp. 3143-3148.

BibTeX

@article{c031426a5bb4448ca2d5f7b1b3c15339,
title = "Infrared spectroscopic evidence for two ways of adsorbed CO coordination",
abstract = "By FTIR spectroscopy at variable temperatures it was shown that CO interacts with extraframework alkali or Ca2+ cations in zeolites to form both M⋯CO and M⋯OC species that are in a temperature dependent equilibrium. The C-bonded species have always higher adsorption energy and account for the strong high-frequency vCO band, while the O-bonded structures reveal themselves in a weak band shifted to lower wavenumbers with respect to the free CO molecule. The difference between the energies of C- and O-bonded species depends upon the cation, and to some extent on the zeolite framework. These CO reorientation energy values, as well as the frequency shifts are well reproduced by a simple electrostatic model of dipole-cation interaction. For CaY zeolite, where two CO molecules can be adsorbed on the same cation, the presence of O-bonded molecules accounts for additional frequency increase of the adjacent CO, that could be interpreted as adsorption-induced increase of Lewis acidity.",
author = "Tsyganenko, {A. A.} and {Otero Arean}, C. and {Escalona Platero}, E.",
year = "2000",
month = jan,
day = "1",
language = "English",
volume = "130 D",
pages = "3143--3148",
journal = "Studies in Surface Science and Catalysis",
issn = "0167-2991",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Infrared spectroscopic evidence for two ways of adsorbed CO coordination

AU - Tsyganenko, A. A.

AU - Otero Arean, C.

AU - Escalona Platero, E.

PY - 2000/1/1

Y1 - 2000/1/1

N2 - By FTIR spectroscopy at variable temperatures it was shown that CO interacts with extraframework alkali or Ca2+ cations in zeolites to form both M⋯CO and M⋯OC species that are in a temperature dependent equilibrium. The C-bonded species have always higher adsorption energy and account for the strong high-frequency vCO band, while the O-bonded structures reveal themselves in a weak band shifted to lower wavenumbers with respect to the free CO molecule. The difference between the energies of C- and O-bonded species depends upon the cation, and to some extent on the zeolite framework. These CO reorientation energy values, as well as the frequency shifts are well reproduced by a simple electrostatic model of dipole-cation interaction. For CaY zeolite, where two CO molecules can be adsorbed on the same cation, the presence of O-bonded molecules accounts for additional frequency increase of the adjacent CO, that could be interpreted as adsorption-induced increase of Lewis acidity.

AB - By FTIR spectroscopy at variable temperatures it was shown that CO interacts with extraframework alkali or Ca2+ cations in zeolites to form both M⋯CO and M⋯OC species that are in a temperature dependent equilibrium. The C-bonded species have always higher adsorption energy and account for the strong high-frequency vCO band, while the O-bonded structures reveal themselves in a weak band shifted to lower wavenumbers with respect to the free CO molecule. The difference between the energies of C- and O-bonded species depends upon the cation, and to some extent on the zeolite framework. These CO reorientation energy values, as well as the frequency shifts are well reproduced by a simple electrostatic model of dipole-cation interaction. For CaY zeolite, where two CO molecules can be adsorbed on the same cation, the presence of O-bonded molecules accounts for additional frequency increase of the adjacent CO, that could be interpreted as adsorption-induced increase of Lewis acidity.

UR - http://www.scopus.com/inward/record.url?scp=0034350970&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0034350970

VL - 130 D

SP - 3143

EP - 3148

JO - Studies in Surface Science and Catalysis

JF - Studies in Surface Science and Catalysis

SN - 0167-2991

ER -

ID: 41682824