K. K. Bhasin, M.-J. Crawford, H. D. B. Jenkins, T. M. Klapötke, J. F. Liebman
Table 1 Formula Unit Volumes, Vm /nm3, Lattice Potential Energy, UPOT/kJ molϪ1 andStandard Entropy, S0298/J KϪ1 molϪ1
.
Ag[ClO3]
[NO2][SbF6]
Ag[SbF6]
0.1195 [5]
[NO2][ClO3]
Ag[ClO4]
[NO][ClO4]
a)
d)
d)
a, h)
V(salt) / nm3
0.0711
0.143 0.014
0.143 0.014
0.0832
0.0861
0.0924 [6]
0.092 0.006
b)
b)
a, h)
b)
0.079 0.006
0.1444
b)
0.0880 ϩ 0.013
641[1]
UPOT(salt) / kJ molϪ1
ρ (salt) / g cmϪ3
670 [1]
651 14 [1]
550 10 [1]
511[1]
580 [1]
618 18 [1]
623 [1]
624 18 [1]
635[1]1
631 23 [1]
2.806 [2]
4.37 [2]
4.43 [3]
191.319
M (salt)
207.319
UPOT(salt) / kJ molϪ1
666
668
576
c)
c)
c)
Average UPOT(salt) / kJ molϪ1
664 ( 6)
152 [3]
551 10
211
580
176
618 18
144
621 23
162 [3]
623
140
S0 / J KϪ1 molϪ1
e)
e)
e)
e)
298
a) Crystal structure data (ref. [2]). b) Ion additivity (see footnote 1)). c) Calculated using the density based equation (footnote 2), [4]). d) Estima-
ted by taking the alkali metal (M) salts, V(MSbF6) from ref. [5] and estimating V([NO2][SbF6]) from V(MSbF6) Ϫ V(Mϩ) ϩ V(NO2
using V(NO2ϩ) ϭ 0.022 0.011 nm3. e) Estimated from equation: S0298/JKϪ1 molϪ1 ϭ kVm ϩ c, k ϭ 1360 JKϪ1 molϪ1 nm3.
)
ϩ
The large error stems from the uncertainty in the volume
data, which itself arises because of the nature of the salts
themselves and the experimental difficulties in their hand-
ling. The corresponding entropy change for reaction (1),
∆S(1) is given by the difference in their standard entropies:
Using the lattice energy data in table 1 and thermo-
chemical data [9] and values of ∆fH0(ClO3Ϫ, g)3) and
∆fH0(ClO4Ϫ, g)4) from reference [9] we estimate that:
∆H(2) ഠ ϩ49 ( 82) kJ molϪ1
(10)
∆S(1) ϭ S0 (Ag[SbF6]) ϩ S0 ([NO2][ClO3])
298
298
3) ∆fH0(ClO3Ϫg) Ϫ this value is estmated using a thermochemical
cycle involving latticeenergies of alkali metal chlorates, MClO3
(estimated from crystal structure volumes and using the volume-
based equation (1), their standard enthalpies of formation and the
enthalpy of formation of the gaseous alkali metal ion, Mϩ.
Ϫ S0 (Ag[ClO3]) Ϫ S0 ([NO2][SbF6]) (6)
298
298
Invoking our isomegethic rule [7] and the relationship be-
tween entropy and volume2) we conclude that:
∆S(1) ഠ 0 J KϪ1 molϪ1
(7)
∆fH0(ClO3Ϫ, g) ϭ UPOT(MClO3)ϩ /2 RT ϩ ∆fH0(MClO3, s)
1
Ϫ ∆fH0(Mϩ, g)
and therefore, that
∆G(1) ഠ ∆H(1) ഠ ϩ17 ( 25) kJ molϪ1
(8)
1
Salt
UPOT(MClO3)
/
RT
∆fH0(MClO3Ϫ, s) ∆fH0(Mϩ, g) ∆fH0(ClO3Ϫ, g)
2
kJ molϪ1
kJ molϪ1 kJ molϪ1
kJ molϪ1
kJ molϪ1
The borderline nature of this result (with its considerable
uncertainty) spans into the thermodynamically favourable
regime and makes an attempt at this preparation of the tar-
get nitryl chlorate, [NO2][ClO3] entirely warranted. The fact
that no [NO2][ClO3] could be detected accords though with
the prediction made by VBT in (8) however.
∆H(2) can be estimated for reaction (2) by incorporating
the reaction into a thermochemical cycle involving the lat-
tice energies of the salts Ag[ClO3], [NO2][SbF6], Ag[SbF6]
and Ag[ClO4] and the standard states of the elements.
∆H(2) can be written:
NaClO3 655
KClO3 642
RbClO3 634
CsClO3 624
1.2
1.2
1.2
1.2
Ϫ365.8
Ϫ397.7
Ϫ402.9
Ϫ411.7
609.0
514.3
490.0
458.0
Ϫ319
Ϫ269
Ϫ258
Ϫ245
The value of ∆fH0(ClO3Ϫ, g) / kJ molϪ1 is far from consistent
averaging to Ϫ 275 ( 44) and differs from the value assigned by
Marcus [10] (Ϫ 200 kJ molϪ1) but is similar to that given by the
WebBook [11] (Ϫ 285 ( 26) kJ molϪ1). If this average value is
used then ∆H(2) ഠ Ϫ 236 ( 67) kJ molϪ1. These salts are difficult
to handle experimentally and have always provided a range of
values for their (constant) properties [12].
4) ∆fH0(ClO4Ϫ, g) Ϫ this value is estmated using a thermochemical
cycle involving latticeenergies of alkali metal perchlorates, MClO4
(estimated from crystal structure volumes and using the volume-
based equation (1), their standard enthalpies of formation and the
enthalpy of formation of the gaseous alkali metal ion, Mϩ.
∆H(2) ϭ 2 UPOT(Ag[ClO3]) ϩ UPOT([NO2][SbF6])
Ϫ UPOT(Ag[SbF6]) Ϫ UPOT(Ag[ClO4]) ϩ 2 RT
1
Ϫ 2 ∆fH0(ClO3Ϫ, g) Ϫ ∆fH0(NO2ϩ, g) Ϫ /2 ∆fH0(H2O, l)
1
ϩ ∆fH0(ClO4Ϫ, g) ϩ ∆fH0(HClO4, l) ϩ /2 ∆fH0(N2O, g) (9)
∆fH0(ClO4Ϫ, g) ϭ UPOT(MClO3)ϩ /2 RT ϩ ∆fH0(MClO4, s)
1
Ϫ ∆fH0(Mϩ, g)
1
Salt
UPOT(MClO4)
/
RT
∆fH0(MClO4Ϫ, s) ∆fH0(Mϩ, g) ∆fH0(ClO4Ϫ, g)
2
2) Recent work has shown a direct proportionality [8a] between
kJ molϪ1
kJ molϪ1 kJ molϪ1
kJ molϪ1
kJ molϪ1
standard entropy, S0 and molecular (formula unit) volume, Vm
298
of the form: S0 ϭ k Vm ϩ c, where k ϭ 1360 JKϪ1 molϪ1 nm3
NaClO4 635
KclO4 624
RbClO4 616
CsClO4 608
1.2
1.2
1.2
1.2
Ϫ383.3
Ϫ432.8
Ϫ437.2
Ϫ443.1
609.0
514.3
490.0
458.0
Ϫ356
Ϫ382
Ϫ310
Ϫ292
298
and c ϭ 15 J KϪ1 molϪ1. A similar form is valid for organic materi-
als [8b]. Thus for any metathetical reaction such as (1) since the
ions are identical on both sides, the overall volume change for the
reaction, ∆V(1) ϭ 0 nm3 and hence correspondingly using the
equation above, ∆S(1) ഠ 0 JKϪ1molϪ1 and hence for reaction (1):
∆H(1) ഠ ∆G(1)
The value of ∆fH0(ClO4Ϫ, g) / kJ molϪ1 is far from consistent
averaging to Ϫ 335 ( 47). This value is close to that assigned by
Marcus [10] and Jenkins and Pratt [13] (Ϫ344 kJ molϪ1).
898
2006 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Z. Anorg. Allg. Chem. 2006, 897Ϫ900