Mm. Jaksic et al., ELECTROCHEMICAL-BEHAVIOR OF PLATINUM IN ALKALINE AND ACIDIC SOLUTIONSOF HEAVY AND REGULAR WATER, International journal of hydrogen energy, 18(10), 1993, pp. 817-837
Citations number
54
Categorie Soggetti
Energy & Fuels","Environmental Sciences","Physics, Atomic, Molecular & Chemical
The behaviour of Pt as an electrode for hydrogen (protium and deuteriu
m) and oxygen evolution in both alkaline and acidic, heavy and regular
water solutions has been investigated primarily by cyclic voltammetry
. The main features, such as adsorption and underpotential deposition
of hydrogen (both protium and deuterium), as well as the specific char
ge capacity for monolayer oxide growth with successive increase in oxy
gen content (preceding hydrogen and oxygen evolution, respectively, wi
th characteristic desorption peaks), were more or less marked in both
electrolytes. Some distinctly different behaviour, however, has been o
bserved, revealing that heavy and regular water behave almost as diffe
rent solvent ambients. The hydrogen evolution reaction (HER) particula
rly in alkaline heavy water occurs at substantially more negative pote
ntials, while oxygen evolution becomes shifted to considerably more po
sitive potential values. Hydrogen absorption, besides adsorption, of b
oth protium and deuterium, has been marked clearly by the continuously
growing charge capacity of the diffusional desorption peak, whose ext
ent depends on the evolving rate and contact time of hydrogen evolutio
n and distinctly exceeds both one-to-one hydrogen to platinum (H/Pt or
D/Pt) atom coverage on the exposed electrode surface, and relative to
the corresponding reversible adsorption wave charge area for its unde
rpotential deposition. In addition, the hydrogen oxidation peak immedi
ately following its desorption (in particular from acidic heavy water)
has also been clearly marked on voltammograms. A distinct merging and
melding together of two initial deuterium reversible desorption peaks
into the diffusional desorption peak in acidic heavy water has been d
iscernibly scanned, too. Oxide formation usually starts at more anodic
potentials together with deuterium oxidation and, specifically in aci
dic media, proceeds vigorously with higher and continuously growing ra
tes and merging together with evolving molecular oxygen, while the pre
vailing oxygen evolution thereby becomes shifted to more positive pote
ntial values. These features reveal that, owing to its distinctly diff
erent steric factor, heavy water (in particular in acidic media) behav
es as a stronger oxidizing agent than regular water. Some discernible
properties of the interplay between hydrogen and oxygen on the Pt elec
trode in both electrolytes along the potential axis have been clearly
marked and pointed out. The Rowland or EDTA effect on the potentiodyna
mic features of Pt has also been scanned and displayed.