L. Dukan et al., PHOTOFRAGMENTATION OF HYDRATED IRON IONS FE(H2O)(N)(-9) AT 532, 355 AND 266 NM() (N = 1), The European Physical Journal. D: Atomic, molecular and optical physics, 3(3), 1998, pp. 257-265
Photofragmentation of Fe(H2O)(n)(+) clusters (n = 1-9) is investigated
at three different wavelengths, 532, 355 and 266 nm. Two fragmentatio
n pathways are observed depending essentially on the photon energy, bu
t also on the parent size n. The fragmentation products belong to two
ion families, Fe(H2O)(m)(+) and FeOH(H2O)(m)(+), which correspond to d
ehydration and intracluster dehydrogenation reactions respectively. Th
e ion yields are studied as a function of the laser fluence in order t
o determine the number of photons implied in the photofragmentation pr
ocess. This allows us to estimate that the D[(H2O)(n-1)Fe+-(H2O)] blon
d energy is ranging between 0.44 eV and 0.55 eV for 5 less than or equ
al to n less than or equal to 9. Photon absorption cross sections are
also derived from the fluence experiments, and two different behaviors
are observed: i) At 355 nm, far away from any Fe+ transition; progres
sive solvation of the metal ion results in an increasing absorption cr
oss section from n = 2 to n = 9. This can be attributed to a forbidden
transition of bare Fe+, which becomes progressively allowed because o
f the interaction with more and more water ligands. ii) At 266 nm, clo
se to several allowed transitions of bare Fe+, a distinct maximum is o
bserved for the absorption of Fe(H2O)(2)(+) ion. It may be attributed
to a change in the spin multiplicity when switching from Fe+ and Fe(H2
O)(+) on one hand to Fe(H2O)(n greater than or equal to 2)(+) on the o
ther.