mechanism of the oxidation of hydrazoic acid by tetrachloroaurate(iii) ion
TRANSCRIPT
Mechanism of the oxidation of hydrazoic acidby tetrachloroaurate(III) ion
Vimal Soni Æ Raj N. Mehrotra
Received: 19 October 2007 / Accepted: 11 December 2007 / Published online: 26 January 2008
� Springer Science+Business Media B.V. 2008
Abstract The oxidation of hydrazoic acid in perchloric
acid in the absence of added chloride under pseudo first-order
conditions ([HN3] » [AuCl4-]) is first order in [Au(III)].
Michaelis–Menten type of dependence (linear plots of kobs-1 vs
[HN3]-1) is observed with respect to [HN3]. The kobs is
independent of ionic strength and the plot between kobs-1 and
[H+] is linear. The inner-sphere mechanism is consistent with
the formation of an axial complex (K = 25 dm3 mol-1)
between AuCl3(HO)- ion and HN3 prior to its rate deter-
mining decomposition (k = 0.0182 s-1). It is inferred that
the free radicals N3• do not oxidise Au(II). The reaction
becomes outer-sphere in the presence of added Cl- ions
which are inferred to form a cage around the hydronium ion
surrounding the AuCl4- ions. The penetration of N3
- through
the cage is rate controlling and within the cage, the electron
transfer from N3- ion to AuCl4
- is fast. The value of the rate
determining constant k2 is 0.547 dm3 mol-1 s-1 and the
equilibrium constant KCl for the cage formation is 5 dm3
mol-1 at 25 �C. It is calculated that the minimum HN3
concentration required before the reaction exhibits zero-
order dependence in HN3 is 0.31 mol dm-3 when
[H+] = 0.18 mol dm-3 at 25 �C.
Introduction
The chemistry of azide ion has been reviewed more than once
[1–4]. Depending on the nature of the oxidant, both inner and
outer-sphere mechanisms have been observed. The
oxidations by one-electron oxidants such as Co3+(aq) [5],
Mn3+(aq) [6], [Mn(bipy)2OH]2+ [7], [Mn(edta)(H2O]- [8],
Ce4+(aqV) [9], [Ni(bipy)3]3+ [10] and [Co(III)O4W12O36]5-
(abbreviated to [Co(III)W]5-) [11] in acidic medium, and
by two-electron oxidants viz. [Ag(OH)4]- [12], [CuIII
(H2TeO6)2]5- and [AgIII(H2TeO6)2]5- [13] in alkaline
medium and [(CH2)2(C2N5H6)2Ag]3+, ethylenebisbigua-
nidesilver(III) in acidic medium [14] are inner-sphere.
A reinvestigation of an earlier study [15] with IrCl62-, IrBr6
2-
and [Fe(bpy)3]3+ ions made in the presence of N-tert-butyl-a-
phenylnitrone (PBN) and 5,5-dimethyl-1-pyrroline N-oxide
(DMPO), traps for the free radical N3•, suggested that the
reactions are outer-sphere [16]. The outer-sphere nature of
the reactions is supported by the application of the Marcus
cross relation [17].
Concerted efforts have been made to understand the
oxidations of organic and inorganic substrates, such as
oxalic acid [18], hydroxylamine [19], histidine [20], gly-
cine [21], Pt(CN)42- [22], I- [23], 4-thio-20-deoxyuridine
and 4-thiouridine 50-monophosphate [24], dimethyl sul-
phide [25], thiocyanate [26], HNO2 [27], HSO3- [28] and
As(III) [29] by various gold(III) complexes. It is suggested
that Au(III) complexes are reduced to the corresponding
Au(I) complexes by soft nucleophiles [30] either by a
direct two-electron transfer without observable intermedi-
ates [23] or by rapid and/or consecutive substitutions
followed by reductive elimination through attack on the
complex by the reducing agent [31].
In the light of the above observations, we have studied
the oxidation of azide ion, a relatively hard nucleophile, by
acidic AuCl4- to know whether the mechanism of this
reaction has any resemblance to the oxidation by
Ag(OH)4-, since AuCl4
- is isoelectronic with Ag(OH)4-. It
was also of interest to know whether the oxidation involves
two-electron transfer in a single step, or one-electron
V. Soni � R. N. Mehrotra (&)
Department of Chemistry, JNV University,
Jodhpur 342 005, India
e-mail: [email protected]
123
Transition Met Chem (2008) 33:367–376
DOI 10.1007/s11243-007-9052-9
transfer in two steps as in the case of [CuIII(H2TeO6)2]5-
oxidation [13]. The results indicate an inner-sphere
mechanism, which is consistent with the behaviour of azide
ion as a ligand for the transition metals [32].
Experimental
Sodium azide (Fluka, purum) was crystallised once and its
solution was standardised with sulphatocerate(IV) solution
using ferroin as indicator. Though the azide solution is
stable over several days [16], fresh solutions were prepared
and used. The solution of NH4AuCl4 (Johnson Matthey)
was prepared in perchloric acid (e = 4.82 9 103 against
literature value = 4.86 9 103 dm3 mol-1 cm-1 [27(b),
33]), or in distilled water (e287 = 3,133 dm3 mol-1 cm-1).
LiClO4, prepared as described elsewhere [34] was used to
adjust the ionic strength. Mixtures of LiCl (Sigma) and
LiClO4 solutions were used to study the effect of [Cl-] on
the observed rate at constant ionic strength and [Li+].
[Ru(NH3)5(H2O)]2+ was prepared as described [35]. Twice
distilled water was used for the preparation of the solutions.
Rate measurements
The rates were measured, under pseudo first-order condi-
tions ([HN3] » [AuCl4-]) at constant ionic strength
(l, LiClO4), in terms of disappearance of Au(III) at
360 nm, at which Beers law is obeyed at different hydro-
gen ion concentrations and HN3 is transparent, using a
Spectrochem Mk (II) colorimeter. The pseudo first-order
rate constant kobs was calculated as 2.303 9 the slope of
the linear plots of log (At - A?) against time, which were
linear for more than two half-lives of the reaction. A? was
taken as zero because the spent reaction mixture was col-
ourless. Some representative plots are shown in Fig. 1. The
EXCEL program was used to draw the plots and the least-
square values of the slopes and intercepts. The reproduc-
ibility of the pseudo first-order rate constant, kobs, was
within ±5%. The program Act-e by H. Strahlow was used
to calculate the activation parameters.
Stoichiometry
A number of reaction mixtures (0.5 C [H+] C 0.1 mol
dm-3) with different initial concentrations of AuCl4- and
HN3 were prepared such that [AuCl4-] was always in
excess. The optical density of the reaction mixture was
measured at 360 nm, with the same colorimeter that was
used for the rate measurements, until it became constant.
The concentration of unreacted AuCl4- in all the reaction
mixtures indicated that D[AuCl4-]/D[HN3] = 0.51 ± 0.02,
which suggested that the stoichiometry of the reaction is
given by Eq. 1.
AuCl�4 þ 2HN3 �! 3N2 þ AuCl�2 þ 2Hþ þ 2Cl� ð1Þ
Characterisation of the reaction products
No quantitative measurements were carried out for the N2
evolved during the reaction though its formation was
qualitatively established. The reaction was carried out at
room temperature. Pure argon gas was passed through the
reaction mixture for sufficient time and the outgoing gas
was passed through a solution of [Ru(NH3)5(H2O)]2+ from
which a red complex, [(NH3)5Ru(N2)Ru(NH3)5]4+, was
isolated [13]. The Raman spectra of this complex shows a
strong m(N:N) band around 3,100 cm-1 [13] which is due
to the coordinated N2.
The spent reaction mixture was evaporated and the dry
residue was dissolved in nitric acid and evaporated again.
The process was repeated several times to ensure complete
decomposition of hydrazoic acid. The residue was finally
dissolved in the minimum volume of hot aqua regia. The
cooled solution on treatment with benzidine produced a
blue colour confirming the presence of Au(III) in the solu-
tion [36] and therefore AuCl2- as the product of the reaction.
Test for free radicals and spectroscopic studies
The solutions of AuCl4- and N3
- were purged with N2 and
to each solution was added 1–2 ml of acrylonitrile. There
appeared no cloudiness or precipitate over several minutes
0
0.15
0.3
0.45
0.6
0.75
0 100 200 300 400 500 600Time (s)
1 +
log
(At -
A∞)
Fig. 1 The plots of 1 + log (At - A?) against time under
experimental conditions: (d) 102[HN3] = 0.1, [H+] = 0.03,
l = 0.087 mol dm-3 at 29 �C; (�) 102[HN3] = 0.5, [H+]
= 0.1, l = 0.7 mol dm-3 at 15 �C; (h) 102[HN3] = 0.1, [H+]
= 0.015, l = 0.087 mol dm-3 at 29 �C
368 Transition Met Chem (2008) 33:367–376
123
before the solutions were mixed to initiate the reaction.
There resulted no cloudiness or thick precipitate in the
reaction mixture even after a prolonged time.
Since the reaction was fast, the reactant solutions of
desired concentrations were cooled in an ice–salt mixture for
sufficient time and so was the quartz cell of 1 cm path-length.
The reactant solutions were mixed and the reaction mixture
was transferred to the quartz cell in quick succession. The
cell was immediately returned to the cell compartment of a
Hewlett-Packard 8452A UV-vis diode array spectropho-
tometer1 having a band width of 2 nm over 350–500 nm.
The entire process was competed within 20–25 s and the
spectral measurement was triggered immediately. A red shift
in the kmax of AuCl4- solution from 310 to 327 nm indicated
the formation of a complex by HN3 with AuCl4- ions.
Fractional distribution of Au(III) and HN3 species
in acidic solution
The fraction of each species (=concentration of the species/
total analytical concentration of the reagent), calculated over
0.005 B [H+] B 0.3 mol dm-3 using KH = 4.17 9 10-5
[37], Khy = 1.6 9 10-5 [38] and Ka = 0.23 mol dm-3 [39]
for the equilibria (2)–(4) respectively, are shown in Fig. 2.
It is seen that the N3- fraction is almost negligible
compared to that of HN3 even at the lowest H+ concen-
tration. Hence, HN3 is considered as the reactive entity of
azide and consequently this equilibrium has nothing to do
with the rate retardation by H+ ion.
The fractional distribution of Au(III) species indicates
that all the three species are present in concentrations hard
to ignore. The concentration2 of AuCl4- increases and that
of AuCl3(OH)- decreases approaching that of AuCl3(OH2)
which increases continuously with [H+] and finally exceeds
that of AuCl3(OH- around [H+] % 0.25 mol dm-3. The
consequences of considering one or a combination of these
species are discussed below.
Results
The plots of kobs against [HN3], Table 1, Fig. 3, are curves
and do not show any sign of saturation at high [HN3] within
the concentration range used. The plots of kobs-1 against
[HN3]-1, shown in Fig. 4, are linear with intercepts on the
rate ordinate within the range of concentrations used. These
Michaelis–Menten plots indicate that Au(III) and hydrazoic
acid complex(es) intervene in the mechanism. The forma-
tion of the complex(es) is supported by the red shift in the
spectrum of Au(III) solution on adding hydrazoic acid as
described above.
To summarise our experimental observations, the kobs
decreased with increasing [H+], Table 2, and the plots of
kobs-1 against [H+], Fig. 5, are linear with positive intercepts on
the rate ordinate. The dependence of kobs on [Cl-], Table 3,
indicates that kobs decreases with increasing [Cl-] and the
plot of kobs-1 against [Cl-], Fig. 6, is linear with positive
intercept on the rate ordinate. However, the kobs is inde-
pendent of the ionic strength, Table 4, indicating that the
reaction partners are either molecular species or an ion and a
molecular species. The present reaction in this respect is
different from the similar oxidation with 12-tungstocobalt
(III) ion [11].
0
0.2
0.4
0.6
0.8
1
0 0.1 0.2 0.3
[H+] (mol dm-3)
frac
tion
of th
e sp
ecie
s
Fig. 2 The plot of the fraction of AuCl4-(D), AuCl3(OH2) (�) and
AuCl3(OH)- ion (d), (m) N3- and (9) HN3 against [H+] at 25 �C for
the initial concentration of gold(III)-complex = 1 9 10-4 mol dm-3
and that of azide = 0.035 mol dm-3
0
5
10
15
20
25
30
35
0 0.01 0.02 0.03 0.04
[HN3] (mol dm-3)
103 k ob
s (s-1
)
Fig. 3 The non-linear plots of kobs against [HN3] at temperatures 25
(d), 30 (h), 35 (D) and 40 �C (�) 104 [Au(III)] = 1.0, [HClO4] =
1.0 and I = 1.5 M
1 The instrument having no facility for maintaining the constant
temperature was not used for the kinetic study.
2 In making the calculations [Cl-] equal to the initial gold(III)
complex is assumed to be present.
Transition Met Chem (2008) 33:367–376 369
123
Mechanism and discussion
Chloroauric acid, HAuCl4, like manganic acid, HMnO4, is
a strong acid and is, therefore, completely ionised even in
dilute solutions of strong mineral acids. AuCl4- ion,
however, exists in equilibrium with other Au(III) species
as shown in equilibria (3) and (4). The consequence of
considering AuCl4- ion as the sole reactive species would
require the reaction to be independent of H+ and Cl- ions,
which is contrary to our observations. The equilibrium (3)
is helpful in explaining the rate retardation by Cl- ions on
the assumption that AuCl4- ion is less reactive than
AuCl3(H2O). Similarly, the equilibrium (4) can be instru-
mental to explain the retardation of the rate by H+ ions by
considering AuCl3(OH-) to be more reactive than
AuCl3(H2O). In conclusion, the reactivity of Au(III) species
is in the order: AuCl3(OH)- [ AuCl3(H2O) [ AuCl4-. The
0
200
400
600
800
1000
1200
1400
1600
1800
0 200 400 600 800 1000 1200
[HN3]-1 (dm3 mol-1)
k obs-1
(s)
Fig. 4 The linear plots of kobs-1 against [HN3]-1 at temperatures at
temperatures 25 (e), 30 (h), 35 (D) and 40 �C (�). 104 [Au(III)] =
1.0; [HClO4] = 1.0 and l = 1.5 mol dm-3
Table 1 Dependence of kobs on the initial [HN3] at different tem-
peratures 104 [AuCl4-] = 1.0, [H+] = 0.18 and l = 0.215 mol dm-3
[HN3] (mol dm-3) 0.001 0.005 0.010 0.015 0.020 0.030 0.035
103kobs
(s-1, 25 �C)
0.566 2.52 4.42 5.92 7.14 8.93 9.62
103kobs
(s-1, 30 �C)
0.951 4.15 7.19 9.43 11.2 13.9 14.9
103kobs
(s-1, 35 �C)
1.54 6.54 11.0 14.3 16.7 20.2 21.5
103kobs
(s-1, 40 �C)
2.48 10.3 17.0 21.6 25.0 29.7 31.1
Table 2 Dependence of kobs on [H+] at different temperatures 104
[AuCl4-] = 1.0, [HN3] = 0.001 and l = 0.037 mol dm-3
[H+] (mol dm-3) 0.001 0.005 0.01 0.015 0.020 0.030 0.035
103kobs
(s-1, 17 �C)
12.1 5.68 3.68 2.91 2.30 1.59 1.37
103kobs
(s-1, 21 �C)
14.8 7.39 4.96 3.83 3.05 2.14 1.92
103kobs
(s-1, 25 �C)
19.2 9.59 6.92 4.63 4.09 2.99 2.59
103kobs
(s-1, 29 �C)
23.5 12.1 8.10 6.17 4.93 3.71 3.14
103kobs
(s-1, 33 �C)
30.2 14.9 10.0 7.84 6.44 4.54 3.85
0
100
200
300
400
500
600
700
800
k obs-1
(s)
0 0.01 0.02 0.03 0.04
[H+] (mol dm-3)
Fig. 5 The plots of kobs-1 against [H+] at temperatures 17 (�), 21 (h),
25 (d), 29 (D) and 33 �C (j) 104 [AuCl4-] = 1.0; 103 [HN3] 1.0 and
l = 0.1 mol dm-3
2
2.5
3
3.5
4
4.5
5
5.5
0 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4
[Cl-] (mol dm-3)
10-3 k
obs -1
(s)
Fig. 6 The linear plot of kobs-1 against [Cl-] at 25 �C. 104 [AuCl4
-] = 1.0;
103 [HN3] 1.0 and l = 0.1 mol dm-3
370 Transition Met Chem (2008) 33:367–376
123
rational consequence of AuCl4- being the least reactive is to
assume it to be inactive. The AuCl3(H2O) is also unlikely to
be the reactive species of choice since H2O is a stronger
nucleophile than OH- ion. Therefore, the substitution of
H2O in AuCl3(H2O) by HN3 is unlikely. Thus, AuCl3(OH)-
is the most likely reactive species.
The reaction is first-order in Au(III)-complex, fractional
order in HN3, and each molecule of AuCl4- consumes two
molecules of hydrazine. The formation of an intermediate
complex between Au(III)-complex and HN3 has spectral
evidence, the rate is independent of the ionic strength and
the free radical test is negative. This leads us to the sequence
of reactions in (2)–(8) (Scheme 1) as part of the most likely
mechanism in the absence of added Cl-. The mechanism in
the presence of Cl- is different as discussed later.
KH
HN3 H+ + N3– (2)
Khy
AuCl4– + H2O AuCl3(H2O) + Cl– (3)
Ka
AuCl3(H2O) AuCl3(OH)– + H+ (4)
K
AuCl3(OH)– + HN3 AuCl3(H2O)N3– (5)
K1
AuCl3(H2O) + N3– AuCl3(H2O)N3
– (6)
kAuCl3(H2O)N3
– AuCl3(H2O)2– + N3+ (7)
fastN3
+ + N3– 3N2 (8)
Scheme 1
Consistent with the known substitution of heterocyclic
amines L in AuLCl3 by N3- and the nucleophilic behaviour
of N3- in kinetics with Pt(II)-complexes [40], the formation
of an intermediate through the reaction (5) or its alternate
(6) with the rate determining step (7) involving two-elec-
tron transfer within the intermediate in a single step
resulting in the formation of N3+ ion is suggested.
The alternate reactions (5) and (6) are not kinetically
distinguishable because of the identity3 KKa = K1KH.
However, reaction (5) is likely to have precedence over
reaction (6) because it involves the fast process of
neutralisation of the OH- ion by the proton of hydrazoic
acid itself. The formation of such an intermediate has been
reported in the oxidation by [Ag(OH)4]- [12], [CuIII
(H2TeO6)2]5- and [AgIII(H2TeO6)2]5- [13] and [(CH2)2
(C2N5 H6)2Ag]3+ ions [14].
The rapid formation of a cyclic hexazine, which has
been supported by the spectral evidence in the decompo-
sition of cis-Pt(N3)2(PPh3)2 [41] through the reaction of N3+
with N3- is assumed in the oxidations by [Ag(OH)4]- [12],
[CuIII(H2TeO6)2]5- and [AgIII(H2TeO6)2]5- ions [13]. The
intermediate hexazine decomposes to N2 in the fast step.
Reaction (8) is thus consistent with the stoichiometry of the
reaction.
The proposed mechanism is similar to those proposed
in the similar oxidations by [CuIII(H2TeO6)2]5- and
[AgIII(H2TeO6)2]5- ions [13] and ethylenebisbiguanide-
Ag(III) [14] but is noticeably different from that by
[Ag(OH)4]- ion [12]. It might be mentioned that the plots in
Fig. 3 are curved towards the concentration axis whereas
similar plots in the oxidation by [Ag(OH)4]-, which has a
second-order dependence in N3-, were curved towards the
rate ordinate [12]. Two kinetically indistinguishable paths
were suggested to account for the second-order dependence
in N3-. In one path, the redox occurs within a five-coordinate
intermediate formed by azide attack on Ag(OH)3N3- and its
conjugate acid. The formation of both cis- and trans-diazido
complexes, Ag(OH)2(N3)2-, constituted the second path and
there was OH--catalysed transformation of the trans-
complex to cis-complex before redox occurred. Since the
ligands, tellurate in the Ag(III) and Cu(III) complexes [13],
ethylenebisbiguanide in the other Ag(III) complex [14] and
Cl- in AuCl4-, are not labile like OH- in Ag(OH)4
- and
there is no second-order dependence in N3-, therefore cis-
and trans-complexes have no existence in these oxidations.
The rate of the reaction deduced from the reactions
(2)–(8) is expressed by Eq. 9
Table 3 Dependence of kobs on [Cl-] at 25 �C 104 [AuCl4-] = 1.0,
[N3-] = 0.001, [H+] = 0.1 and l = 0.687 mol dm-3
LiClO4 (mol dm-3) 0.586 0.500 0.400 0.300 0.200
LiCl (mol dm-3) 0.0 0.086 0.186 0.286 0.386
103kobs (s-1) 2.11 0.381 0.284 0.219 0.186
Table 4 The effect of the ionic strength on the rate of the reaction at
20 �C 104 [AuCl4-] = 1.0, [HN3] = 0.01, [H+] = 0.1 mol dm-3
[LiClO4] (mol dm-3) 0.014 0.064 0.164 0.264 0.364 0.464
l (mol dm-3) 0.114 0.164 0.264 0.364 0.464 0.564
103 kobs (s-1) 8.33 8.20 8.20 8.24 8.43 8.39
3
½AuCl3ðH2OÞN�3 � ¼KKa½AuCl3ðH2OÞ�½HN3�
½Hþ�¼ K1KH½AuCl3ðH2OÞ�½HN3�
½Hþ�
Transition Met Chem (2008) 33:367–376 371
123
�d½AuIII�odt
¼ kKKa½AuCl3ðH2OÞ�½HN3�½Hþ� ð9Þ
The mass balance for the species N3- and [AuCl3(H2O)]
in terms of the distribution of the respective species given
in Eqs. 2 and 3–5 is expressed by the Eqs. 10 and 11,
respectively.
½N�3 � ¼KH½HN3�oKH þ ½Hþ�
ð10Þ
½AuCl3ðH2OÞ�
¼ Khy½Hþ�½AuIII�oKhy½Hþ� þ KaKhy þ ½Hþ�½Cl�� þ K1Khy½Hþ�½N�3 �
� �
ð11Þ
Substituting the values of [N3-] and [AuCl3(H2O)] from
Eqs. 11 and 12 into Eq. 9 gives the Eq. 12.
Since [H+] » KH, Eq. 12 is reduced to Eq. 13.
�d½AuIII�odt
¼ kKKaKhy½AuIII�o½HN3�oKhy½Hþ�þKaKhyþ½Hþ�½Cl��þKKaKhy½HN3�o
ð13Þ
Reaction in the absence of Cl- ions
In the absence of Cl- ions, [H+][Cl-] is neglected and so is
the product KaKhy because of the low value of Khy. The
Eq. 13 is therefore modified to Eq. 14, the inverted form of
which is given in Eq. 15, which is consistent with the linear
plots of kobs-1 against [HN3]-1, Fig. 4, and that of kobs
-1
against [H+] (Fig. 5).
kobs ¼�d½AuIII�odt½AuIII�o
¼ kKKa½HN3�o½Hþ� þ KKa½HN3�o
ð14Þ
1
kobs
¼ ½Hþ�kKKa½HN3�
þ 1
kð15Þ
The close agreement between the k values at 25 �C,
0.0182 s-1 from the plot in Fig. 4 and 0.0190 s-1 from the
plot in Fig. 5, is a strong support for the proposed
mechanism. The so-calculated k values at different
temperatures are reported in Table 5 and the linear plot of
log k against 1/T is shown in Fig. 7. The activation
parameters DH� and DS� are also reported there. The
relatively small value of DH� could be attributed to the
formation of an intermediate in the equilibrium (5).
The formation of an axial bond between the positive AuIII
and N3- helps to stabilise the intermediate.
It is apparent from Eq. 15 that I/S = KKa/[H+] where I
and S are the intercept and slope of the plots in Fig. 4.
Therefore K is given by Eq. 16
K ¼ ½Hþ� � I
Kað¼ 0:23Þ � Sð16Þ
Using Eq. 16 and substituting the values of I = 54.8 s,
S = 1.7 mol dm-3 s, [H+] = 0.18 mol dm-3 and Ka =
0.23 mol dm-3, a value of K = 25 dm3 mol-1 at 25 �C is
obtained. Thus the value of K is within the range (0.1–100)
of formation constants of azido complexes [6(a)–8, 12, 13].
The values at other temperatures are not obtainable because
the values of Ka at other temperatures are not known.
The intercept on the rate ordinate of Fig. 3 is an indi-
cation that the hypothetical rate at infinite concentration of
HN3 has a finite value. This demands that the plot falls off
asymptotically to a constant kobs at high [HN3]. This situ-
ation in terms of Eq. 14 is achieved when
KKa[HN3] » [H+] so that the Eq. 14 changes to Eq. 17.
kobs ¼ k ð17Þ
The least value of [HN3] required under which the
inequality KKa[HN3] » [H+] holds good is calculated from
the simple relation KKa[HN3] = 10[H+]. For [H+] =
0.18 mol dm-3 and the known value of Ka = 0.23 mol
dm-3 [39] since K has a calculated value of 25 dm3 mol-1
(see above) at 25 �C, the minimum HN3 concentration is
calculated to be 0.31 mol dm-3 which is about nine times the
maximum concentration of HN3 used in Table 1.
The N3- ion is considered to coordinate axially because a
negative ion is generally preferably coordinated to the axial
position of a metal. Such coordination has been proposed in
the oxidations of hypophosphate [42], iodide [43] and
mandelate [44] by the square planar Ag(OH)4- complex.
The formation of a similar axial intermediate complex has
been proposed in the oxidation of histidine [20], SO32- ion
[45] and oxalic acid [18] by AuCl4- ion. This possibility is
most likely considering that AuCl3(OH)- ion is also
square-planar like Ag(OH)4- ion and that AuIII and AgIII are
�d½AuIII�odt
¼ kK1Khy½Hþ�½AuIII�oKhy½Hþ� þ KaKhy þ ½Hþ�½Cl�� þ K1Khy½Hþ�KH½HN3�o
KHþ½Hþ�
� �� KH½HN3�oKH þ ½Hþ�
ð12Þ
372 Transition Met Chem (2008) 33:367–376
123
isoelectronic. The graphical representation of the formation
of the axial complex and the electron transfer within this
complex are illustrated in Eqs. 18 and 19, respectively.
Equations (18) and (19) correspond to Eqs. 5 and 7,
respectively. The product side of Eq. 19 could be suitably
modified to correspond to Eq. 20.
It has been pointed out that the activated pathway for
ligand substitution in four-coordinate planar d8 metal
complexes requires a five-coordinate transition state [46].
The six-coordinate species are unknown in solution though
these are known in the solid state [46]. The processes are
likely to require a high degree of orientation in the tran-
sition state as indicated by the large negative DS� value
[46].
The negative free radical test does not conclusively
eliminate the possibility of the formation of such species
which may decay rapidly before reaching the bulk sol-
vent for their detection. Thus the possibility of
successive one-electron transfer cannot be effectively
ruled out in view of the fact that Au(II) has been
reported as an intermediate in several redox reactions
[47–52], and its dithiolene and dicarbolyl compounds are
known [53].
Accordingly, Scheme 1 can be suitably modified by
replacing (7)–(8) by (20)–(22) (Scheme 2), the rate law
will have the same form except that k is replaced by
k1
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
3 3.1 3.2 3.3 3.4 3.5 3.6
103/T
2 +
log
k
Fig. 7 The linear plot of log k against 1/T where k is the rate
determining rate constant
Table 5 The k (s-1) values obtained from the plots in Figs. 4 (a) and 5 (b) at different temperatures with associated activation parameters
Temp (�C) 17 21 25 25 29 30 33 35 40
102k 1.37(b) 1.57(b) 1.82(a) 1.90(b) 2.42(b) 2.62(a) 3.23(b) 3.47(a) 4.78(a)
DH� = 40 ± 2 kJ mol-1
DS� = -126 ± 7 J K-1 mol-1
Au
ClCl
Cl
Au
ClCl
Cl−
+ HN N NK
OHOH 2
N
N
N −
(18)
Au
ClCl
Cl OH2
N
N
N −
kAuCl3(H 2 O)2− + N3
+(19)
Transition Met Chem (2008) 33:367–376 373
123
k1
AuCl3(H2O)N3– AuCl3(H2O) – + N3
• (20)
fast( k )′
AuCl3(H2O)– + N3– AuCl3(H2O)2– + N3
• (21)
fast( k )2N3
• 3N2 (22)
Scheme 2
The reaction (21) is proposed because the oxidation of
N3• radical either by Au(III) or Au(II) in the fast step
would violate the observed stoichiometry of the reaction.
However, on the other hand N3• happens to be a strong
oxidant, because the potential of N3-/N3
• couple is 1.33 V
[16], therefore it is likely that Au(II) may be oxidised back
to Au(III). Ideally, the measurement of the rate constant
for the reaction AuCl3- + N3
• would have provided the
right answer. Since this is not easily feasible4 the fol-
lowing considerations were helpful to conclude against the
possible feasibility of the reversibility of reaction (21).
The relatively high value of rate constant for the decay of
N3• radical to N2, 4.5 9 109 dm3 mol-1 s-1 [16] over that for
the disproportionation of Au(II), 1.4 9 109 dm3 mol-1 s-1,
generated from AuCl4- in the absence of Cl- ion in aque-
ous solution at pH 2, suggests that the build up of the
necessary concentration of N3• radical required to make the
reaction (21) reversible is most unlikely. Further, if the reac-
tion (23) happens to be reversible, then the usual first-order
plots for the disappearance of Au(III) would show a definite
deviation from linearity. Since this is not the case as shown by
the plots in Fig. 1, therefore the reversibility of the reaction
(21) is highly improbable.
Consideration of the potentials of Au+/Au++,\1.29 V vs
NHE. [54] and N3-/N3
• (1.33 V [16]) which are similar,
suggests that N3• can in no way oxidise Au++ ion to any
appreciable extent. For the reversibility of the reaction
(21), it is important that there is a necessary build up of N3•
concentration, which is highly unlikely in view of the high
rate of decay of N3• radical to N2 [16].
N�3 þ N�3 �fast
N��6 ð23Þ
The reaction (23) is another path for the decay of the N3•
radical into N2. The consideration of the equilibrium
constant, 0.33 dm3 mol-1 [55] suggests that it will be
a minor species, and since the forward rate constant,
1 9 106 dm3 mol-1 s-1 [16] is about 103 times smaller
than the rate constant k00 therefore it would be unable to
compete with the reaction (22).
Mechanism in the presence of Cl- ions
For the reaction in the presence of Cl-, the term [H+][Cl-]
is no more negligible, KaKhy is neglected as before and
Khy[H+] « [H+][Cl-], the Eq. 13 would change to Eq. 24
the inverted form of which is given in Eq. 25.
kobs ¼�d½AuIII�dt½AuIII�o
¼ kK1KHKhy½HN3�o½Hþ�½Cl�� þ K1KHKhy½HN3�o
ð24Þ
1
kobs
¼ ½Hþ�½Cl��kKKaKhy½HN3�
þ 1
kð25Þ
Equation (25) predicts that the intercept values of the plots
of kobs-1 against [X] ([X = H+ or Cl-]) should be the same.
However, the intercept derived from Fig. 4 (X = H+,
intercept = 52.7 s; k = 0.019 s-1) differed widely from
that obtained from Fig. 5 (X = Cl-, intercept = 1.82 s,
k = 0.55 s-1). The k value derived from Fig. 5 is about 30
times the value obtained from Fig. 4. This clearly indicates
that either the reactive species or the mechanism or both
are different in the presence and absence of chloride ions.
Although no systematic study on the effect of [HN3] on
the observed rate constant in the presence of chloride ions
was carried out, an indication of an outer-sphere mecha-
nism was provided by the rate constant which increased
almost by a factor of two on increasing the concentration of
hydrazoic acid by the same factor. The change from the
inner-sphere to outer-sphere mechanism, in the presence of
excess Cl- ions, is not caused by any change in the Au(III)
species considered in equilibria (3) and (4) because the
coordination shells in these species are full. The excess
Cl- ions may push the equilibrium (3) to the far left
affecting the equilibrium (4) to the extent that AuCl3(H2O)
and AuCl3(OH)- become negligible minor species leaving
AuCl4- as the only bulk species. The equilibrium (2),
however, remains unaffected.
The Cl- ions, in addition to affecting the equilibria (3)
and (4) as described above have another role in the system.
The excess chloride ions form a cage around hydronium ion
surrounded AuCl4-. The caged AuCl4
- species, ½AuCl�4 �Cl� ,
and AuCl4- are in equilibrium as shown in reaction (26). The
N3- and ½AuCl�4 �Cl� are the redox partners, and the reaction
is initiated by the penetration of the chloride cage by N3-,
which faces repulsive forces. Thus, the penetration is a slow
process or the rate determining step. The attack of AuCl4- by
N3- inside the cage is fast and may involve either a net two-
electron change with the formation of N3+ followed by the
reaction (8) as considered in the Scheme 1 or single-electron
transfer in two successive steps resulting in the formation of
N3• radical as considered in Scheme 2. The details of the
reactions in the latter possibility are considered below
where ½AuCl�4 ;N�3 �Cl� represents the presence of N3
- inside
the cage.
4 The rates reported for the corresponding reaction with IrCl63- in
[11] were measured at the Centre for Fast Kinetics Research at the
University of Texas at Austin.
374 Transition Met Chem (2008) 33:367–376
123
½AuCl�4 � þ Cl� �KCl ½AuCl�4 �Cl� ð26Þ
½AuCl�4 �Cl� þ N�3 �!k2 ½AuCl�4 ;N�3 �Cl�
chloride cage chloride cageð27Þ
½AuCl�4 ;N�3 �Cl� �!
fastAu(II)þ N�3 ð28Þ
Au(II)þ N�3 �!fast
Au(I)þ N�3 ð29Þ
The nature of Au(II) and Au(I) species in the present
context is not properly understood. The reaction (27) is rate
limiting, and the reactions (28) and (29) are followed by
the reaction (22) for the decay of N3•. The rate of the
reaction is expressed in Eq. 30.
�d½AuIII�odt
¼ k2½AuCl�4 �Cl� ½N�3 � ð30Þ
The proper substitution of the values of ½AuCl�4 �Cl� from
the consideration of equilibrium (26) and that of [HN3]o
given in Eq. 10 into Eq. 30 would change it to Eq. 31, the
inverted form of which is given in Eq. 32.
�d½AuIII�odt½AuIII�o
¼ kobs ¼k2KH½HN3�
½Hþ� þ KCl½Hþ�½Cl�� ð31Þ
1
kobs
¼ ½Hþ�k2KH½HN3�
þ KCl½Hþ�½Cl��k2KH½HN3�
ð32Þ
Equation (32) is consistent with Fig. 6 from which k2 =
0.546 dm3 mol-1 s-1 and KCl = 5 dm3 mol-1 are obtained
at 25 �C.
Conclusion
In conclusion, the oxidation of hydrazoic acid, in the
absence of added chloride ions, by tetrachloroaurate(IIII)
ion is inner-sphere in which hydrazoic acid is axially
coordinated to Au(III) ion, the free radicals N3• do not
oxidise Au(II) and the H+ ions retard the kobs. In presence
of added Cl- ions, the hydronium ion surrounded AuCl4- is
caged by chloride ions and the reaction is outer-sphere. The
penetration of the chloride cage by N3- is rate controlling.
The electron transfer within the cage is fast.
Acknowledgements Thanks are due to the UGC, F.12-59/1997 and
F.12-147/2001, for the financial support of the work. Thanks are also
due to Kriti Mehrotra, my grand daughter, at Cornell University, in
helping with certain references.
References
1. Audrieth LF (1934) Chem Rev 15:169
2. Evans BL, Yoffe AD, Gray P (1959) Chem Rev 59:515
3. Gray P (1963) Q Rev Chem Soc 17:441
4. Stedman G (1979) Adv Inorg Chem Radiochem 22:113
5. (a) Murmann RK, Sullivan JC, Thompson RC (1968) Inorg Chem
7:1876; (b) Wells CF, Mays D (1969) J Chem Soc A:2175; (c)
Thompson RC, Sullivan JC (1970) Inorg Chem 9:1590
6. (a) Wells CF, Mays D (1968) J Chem Soc A:1622; (b) Davies G,
Kirschenbaum LJ, Kustin K (1969) Inorg Chem 8:663; (c) Tre-
indl CFL, Mrakova M (1977) Chem Zvesti 31:145
7. Heyward MP, Wells CF (1988) J Chem Soc Dalton Trans 1331
8. Suwyn MA, Hamm RE (1967) Inorg Chem 6:2150
9. Wells CF, Husain M (1969) J Chem Soc A:2981
10. Brown JK, Fox D, Heyward MP, Wells CF (1979) J Chem Soc
Dalton Tran 735
11. Goyal B, Mehrotra M, Prakash A, Mehrotra RN (2000) Inorg
React Mech 1:289
12. Borish ET, Kirschenbaum LJ (1984) Inorg Chem 23:2355
13. Sen Gupta KK, Sanyal A, Ghosh SP (1995) J Chem Soc Dalton
Trans 1227
14. Bandyopadhyay P, Dhar BB, Bhattacharyya J, Mukhopadhyay S
(2003) Eur J Inorg Chem 4308
15. Wilmarth WK, Stanbury DM, Byrd JE, Po HN, Chua C-P (1983)
Coord Chem Rev 51:155
16. Ram MS, Stanbury DM (1986) J Phys Chem 90:3691
17. Marus RA (1963) J Phys Chem 67:853; (1964) Ann Rev Phys
Chem 15:155; (1965) J Chem Phys 43:679
18. Soni V, Sindal RS, Mehrotra RN (2007) Inorg Chim Acta
360:3141
19. (a) Soni V, Mehrotra RN (2003) Transition Met Chem 28:893;
(b) Sengupta KK, Basu B (1983) Transition Met Chem 8:6
20. Soni V, Sindal RS, Mehrotra RN (2005) Polyhedron 24:1167
21. Zou J, Guo Z, Parinson JA, Chen Y, Sadler PJ (1999) Chem
Commun 1359
22. Drougge L, Elding LI (1987) Inorg Chem 26:1073
23. (a) Elding LI, Skibsted LH (1986) Inorg Chem 25:4084; (b)
Elding LI, Olsson LF (1982) Inorg Chem 21:779
24. Ericson A, Arthur JC, Coleman RS, Elding LI, Elmorth SKC
(1998) J Chem Soc Dalton Tran 1687
25. Ericson A, Elding LI, Elmorth SKC (1997) J Chem Soc Dalton
Tran 1159
26. (a) Elmorth SKC, Elding LI (1996) Inorg Chem 35:2337; (b)
Elmorth S, Skibsted LH, Elding LI (1989) Inorg Chem 28:2703
27. (a) Berglund J, Voigt R, Fronaeus S, Elding LI (1994) Inorg
Chem 33:3346; (b) Sengupta KK, Sanyal A, Sen PK (1994)
Transition Met Chem 19:534
28. Sengupta KK, Das S, Sen Gupta S (1988) Transition Met Chem
13:261
29. Sen Gupta KK, Basu B (1984) Polyhedron 3:805
30. Skibsted LH (1986) Adv Inorg Bioinorg Mech 4:137
31. References 3–15 in Ref. 21.
32. Cotton FA, Wilkinson G (1986) Advanced inorganic chemistry,
3rd edn. Wiley Eastern. New Delhi, p 353
33. Fry FH, Hamilton GA, Turkevich J (1966) Inorg Chem 5:1943
34. Rekha Ms, Prakash A, Mehrotra RN (1991) Can J Chem 71:2164
35. Seddon EA, Seddon KR (1984) The chemistry of ruthenium.
Elsevier, p 251
36. Feigl F, Anger V, Oesper R (1972) Spot tests in inorganic anal-
ysis, 6th English edn. Elsevier Amsterdam, p 241
37. Martell AE, Smith RM (1989) Critical stability constants, vol 4.
Plenum, New York, p 45
38. Robb W (1967) Inorg Chem 6:382
39. Peshchevitskii BI, Belevantsev VI, Kurbatova NV (1971) Russ J
Inorg Chem (Engl Transl) 16:1007
40. Cattalini L, Tobe ML (1966) Coord Chem Rev 1:106
41. Volger A, Wright RE, Kunkley H (1980) Angew Chem Int Ed
Engl 19:717
42. Mehrotra RN, Kirschenbaum LJ (1989) Inorg Chem 28:4327
43. Kouadio I, Kirschenbaum LJ, Mehrotra RN (1990) J Chem Soc
Dalton Trans 1929
Transition Met Chem (2008) 33:367–376 375
123
44. Kouadio I, Kirschenbaum LJ, Mehrotra RN, Sun Y (1990)
J Chem Soc Dalton Trans 2123
45. Berglund J, Elding LI (1995) Inorg Chem 34:513
46. Cattalini L, Marangoni G, Paolucci G, Pitteri B, Tobe ML (1987)
Inorg Chem 26:2450
47. Refs. 17(b) and 26
48. (a) Sen Gupta KK, Basu B, Sen Gupta S, Nandi S (1983) Poly-
hedron 2:983; (b) Ref. 27
49. Sen Gupta KK, Maiti S, Ghosh SP (1980) Indian J Chem
19(A):869
50. Brown A, Higginson WCE (1972) J Chem Soc Dalton Trans 166
51. Foresberg HG, Widdel H, Erwall LG (1960) J Chem Educ 37:44
52. Basalo F, Pearson RG (1977) Mechanism of inorganic reactions,
2nd edn. Wiley Eastern, New Delhi, p 414
53. Ref. 30, p 1044
54. Latimer WM (1953) The oxidation states of the elements and
their potentials in aqueous solutions, 2nd edn. Prentice-Hall,
p 197
55. Butler J, Land EJ, Swallow AJ, Pritz W (1984) Radiat Phys Chem
23:65
376 Transition Met Chem (2008) 33:367–376
123