Adsorbed states of acetonitrile and chloroform on amorphous and crystalline ice studied with X-ray photoelectron spectroscopy

Citation
Je. Schaff et Jt. Roberts, Adsorbed states of acetonitrile and chloroform on amorphous and crystalline ice studied with X-ray photoelectron spectroscopy, SURF SCI, 426(3), 1999, pp. 384-394
Citations number
30
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
SURFACE SCIENCE
ISSN journal
00396028 → ACNP
Volume
426
Issue
3
Year of publication
1999
Pages
384 - 394
Database
ISI
SICI code
0039-6028(19990520)426:3<384:ASOAAC>2.0.ZU;2-A
Abstract
The adsorbed states of acetonitrile (CH3CN) and chloroform (CHCl3) on ultra thin films of amorphous and crystalline ice were studied with X-ray photoel ectron spectroscopy (XPS). Results were in agreement with previously publis hed temperature programmed desorption (TPD) and Fourier transform infrared reflection absorption spectroscopy (FTIRAS) studies. The N(ls) spectrum of acetonitrile on amorphous ice exhibits two states of binding energies, 402. 2 and 401.4 eV, which are assigned to hydrogen bonded and physisorbed/multi layer acetonitrile, respectively. The Cl(2p) spectrum of chloroform on amor phous ice exhibits a single set of peaks, associated with the 2p(1/2) and 2 p(3/2) spin states of the physisorbed molecules. There is no hydrogen bonde d state, as expected for a weak hydrogen bond acceptor like CHCl3. The N(1s ) spectra of acetonitrile on crystalline ice show that very little hydrogen bonded CH3CN is present. Instead, there are two states, one at 401.4 eV (t he multilayer) and the other at 400.4 eV. The latter state saturates at a c overage of similar to 1 monolayer. The C(1s) spectra of acetonitrile on cry stalline ice and the Cl(2p) spectra of chloroform on crystalline ice also r eveal the: presence of states shifted by roughly -1 eV with respect to the multilayer. These states are attributed to the first layer of physisorbed C H3CN or CHCl3, their binding energies are shifted relative to the multilaye r because of final state interactions between the adsorbed molecules and th e dipolar crystalline ice surface. The crystalline surface is suggested to be dipolar because of a reconstruction that results in a decrease in the co verage of free surface OH groups. (C) 1999 Elsevier Science B.V. All rights reserved.