INFRARED-SPECTROSCOPY OF MODEL ELECTROCHEMICAL INTERFACES IN ULTRAHIGH-VACUUM - EVIDENCE FOR COUPLED CATION-ANION HYDRATION IN THE PT(111) K+,CL- SYSTEM/
I. Villegas et Mj. Weaver, INFRARED-SPECTROSCOPY OF MODEL ELECTROCHEMICAL INTERFACES IN ULTRAHIGH-VACUUM - EVIDENCE FOR COUPLED CATION-ANION HYDRATION IN THE PT(111) K+,CL- SYSTEM/, Journal of physical chemistry, 100(50), 1996, pp. 19502-19511
Infrared reflection-absorption spectroscopy (IRAS) measurements along
with work-function (Phi) and temperature-programmed desorption (TPD) d
ata are reported for deuterated water dosed onto Pt(111) in ultrahigh
vacuum (uhv) in the presence of adsorbed chlorine and potassium in ord
er to assess the nature and extent of hydration of a ''chemisorbed'' (
or specifically adsorbed) anion in the absence and presence of a catio
n ''countercharge'', and vice versa. As studied previously (ref 6a), p
otassium constitutes an ideal ''cation'' for this purpose since it ind
uces large Phi decreases even for small K coverages (theta(K) less tha
n or equal to 0.08) that are modified substantially by hydration; this
primary solvation also yields downshifted O-D stretching (nu(OD)) vib
rations (ca. 2300-2500 cm(-1)) that are diagnostic of cation-induced w
ater reorientation, Adsorption of atomic chlorine (dosed as Cl-2) yiel
ds milder yet nonmonotonic Phi changes, suggestive of only partial cha
rge transfer to form Cl-delta. The presence of adsorbed Cl attenuates
the large (ca. 1.2 eV) Phi decreases produced by water dosing onto cle
an Pt(111), yet in largely featureless fashion. An absence of strong C
l hydration, suggested by these data and from TPD measurements, is als
o indicated by lack of solute-induced nu(OD) bands in the correspondin
g infrared spectra, except at high Cl coverages (theta(Cl)) and submon
olayer D2O dosages. Markedly different behavior, however, is observed
in the presence of both Cl and K adsorbates. Addition of roughly stoic
hiometric Cl coverages to adsorbed K in the absence of water yields su
bstantial (ca. 1.5 eV) increases followed by only minor changes for hi
gher theta(Cl) values, suggesting intimate electrostatic K/Cl interact
ions involving K+... e(-)/ Cl-... e(+) dipole polarization. Furthermor
e, water addition to K/Cl mixtures where theta(Cl) greater than or equ
al to theta(K) triggers only minor Phi changes, in contrast to the sit
uation for the absence of Cl. This evidence that the interfacial hydra
tion of both ''ionic'' solutes is being modified in their combined pre
sence is further indicated by corresponding nu(OD) infrared fingerprin
ts that differ substantially from corresponding spectra obtained for e
ach solute separately, Thus, the K+ ''hydration shell'' nu(OD) signatu
re is largely removed in the presence of Cl, and a new feature (at 262
0 cm(-1)) appears; the latter is most likely associated with solvation
of Cl-delta-/K+ pairs. Further evidence for the coupled nature of thi
s hydration is also gleaned from the marked cooperative influences of
Cl and/or K adsorption upon the water desorption temperatures. The qua
litative implications of these findings to the conventional picture of
solvation in the electrochemical double layer are also noted.