J. Zarpellon et al. / Electrochimica Acta 53 (2007) 2002–2008
2007
The molecular structure of the SSac is similar to saccharin
with sodium atoms replacing the hydrogen bound to nitrogen.
The influence of SSac in the electrodeposition of Fe deposits on
Sicanbeexpectedtoleadtothesamebehavior. Ourexperimental
observations confirm results published in the literature, concern-
ing the influence of saccharin on Fe-group deposits. Notably,
the addition of SSac results in a fairly broad Fe reduction wave,
superimposed to hydrogen evolution and nucleation potentials
shifts towards more negative potentials with respect to the cycle
of the solution without SSac. It is difficult, however, to ascertain
what is the cause for the observed shifts in the reduction waves,
since different electron transfer paths for the reduction of elec-
troactive species at the Si/electrolyte interface could occur due
to SSac affinity with the ions present in the solution and change
the diffusion of cations towards the cathode because of this com-
plexation [29]. It is also reliable that changes in the hydrogen
evolution occurs due to SSac addition. It has been shown that
the general chemical formula of the metal–saccharin complex
has the iron ion bound to the nitrogen atom in the sulfonamide
group. SSac adsorption in the H-terminated Si/electrolyte inter-
face could promote variations in the ion discharging ability along
the substrate surface altering the Schottky barrier height (SBH)
formation in the n-type Si/eletrolyte interface. A SBH value of
about 0.7 eV is reported for CoFe/Si interface [30], however
this value cannot explain the necessary cathodic potential for
the nucleation wave observed in our experiments. Since Fe sili-
cides formation [11] is tremendously inhibited by addition of
SSac and current densities exhibit drastic changes for deposition
times (smaller than 100 s) corresponding to a coverage fraction
of Si substrate smaller than 30–40% of total area, we cannot
discard that important changes are introduced in the nucleation
and growth processes by the addition of SSac and its adsorption
on the hydrogen-terminated Si surface. Therefore, SSac adsorp-
tion on hydrogen-terminated Si surface and freshly nucleated Fe
together with complexation mechanism in solution are closely
related to the small cathodic shifts observed at the onset the
cathodic current in the cyclovoltammograms presented in Fig. 1.
Many changes in growth kinetics and deposit structure are
introduced by the addition of SSac in the solution indicating the
influence of SSac adsorption on freshly nucleated Fe. The poten-
tiostatic transients taken at a potential of −1200 mV exhibit an
evolution in a time scale of several hundred seconds, as shown
in Fig. 2. We describe the time evolution of potentiostatic tran-
sients as follows. Atthe beginning, a sporadic andheterogeneous
nucleation occurs due to a random occupation of the prefer-
ential active sites on the initial surface. Next, the number of
nuclei growing on the Si surface is rapidly saturated and, sub-
sequently, a further reduction of Fe ionic species on the already
deposited nuclei predominates; i.e., nucleation and growth are
in favor of the deposition on the covered zones. The average
granule sizes scattered in micrometer scale in the AFM images
and Si photoemission signal observed by XPS corroborate these
assumptions and is also indicating that Volmer–Weber three-
dimensional growth mode [14–19] occurs. The addition of SSac
increases the Fe ion discharging ability, facilitating a diffusion-
limited aggregation of ions in juxtaposed three-dimensional
islands with a slightly flat growth front. The inhibition of silicide
and oxy-hydroxide formation occurs with an enlargement of the
granule sizes. As mentioned in Section 3.4, the investigation
of deposition in presence of 1.5 g/L SSac under a potential of
−1500 mV reveals the SSac dissociation with sulfur incorpora-
tion in deposits with evidence of local disruption of the film due
to a severe hydrogen evolution. The potentiostatic transients, in
this case, exhibit current densities reaching stationary values as
2
large as 80 A/cm with high noise level as a consequence of
the hydrogen gas bubble evolution. Compact and smooth (RMS
roughness is 21 nm) deposits are formed with small granule
sizes (0.8 m). However, the formation of Fe silicides and oxy-
hydroxides is observed by XRD. It is indicating that moderate
cathodic potential to inhibit SSac dissociation and incorporation
in the deposits are necessary to avoid silicide and oxy-hydroxide
formation.
Fe growth on a clean Si surface in non-equilibrium condi-
tions (like electrochemical conditions) easily leads to unusual
silicides formation as a result of stress accommodation at the
interface, variations in the stoichiometry of initial deposit and
islanding kinetic factors. In our previous work [11], XRD and
XPS data present evidence that metastables Fe2Si and Fe Si3 are
5
formed and their Bragg reflection peaks increase upon anneal-
ing together with a clear increase in the Fe crystalline quality
attested by intensity increase of the ␣-Fe(0 1 1). In the present
case, the XRD patterns shown in Fig. 4(a) reveal that ␣-Fe is
formed. Although significant, only small relaxation (2.2–2.1%)
of the expanded Fe lattice is observed in the presence of SSac
(from 0.5 to 1.1 g/L SSac). It was found a crystalline texture
with predominance of the densest atomic plane (1 1 0) of ␣-Fe
in the film plane predominates when increasing SSac, as shown
in Fig. 4(b). However, the addition of SSac while keeping the pH
and temperature of the electrolyte stable have a small influence
in the residual strain. It is probably connected with the higher
growth rates imposed by SSac (as shown in Fig. 2). A faster
nucleation is more effective to inhibit the interface reaction than
induce a strain relaxation in the deposits.
A predominant metallic Fe nature of deposits even exposed to
the air is confirmed by XPS. Comparing the XPS spectra evolu-
tion of Fig. 5(a) and (b) for equivalent etching times, we observe
that a metallic Fe component becomes predominant for deposits
obtained from solutions with a higher SSac concentration. Since
the surface morphology and ion decapping can be considered the
same, we may conclude that SSac tends to inhibit the oxidation
of the samples exposed to the air. This assumption is also cor-
roborated by XRD analyses since a higher (1 1 0)-texture in the
deposits with 1.5 g/L SSac tends to reduce their oxidation front.
The structural changes imposed by SSac present in the solu-
tions are apparently significant to affect the room temperature
hysteresis cycle of the ferromagnetic deposits. The small strain
relaxation and densest juxtaposition of grains are probably asso-
ciated with reduction of the coercive fields when increasing
SSac. Besides, bulk Fe has an easy and hard magnetic axis along
the ꢀ1 0 0ꢁ and ꢀ1 1 1ꢁ crystalline directions, respectively. Then,
the crystalline texture with (1 1 0) planes preferentially oriented
parallel to the strain-relaxed film plane is reasonable to result
in almost isotropic easy magnetic plane with a small remanence
ratio as observed. Thus, concerning the change of the texture of