| Literature DB >> 35446995 |
Valentin Radtke1, Niklas Gebel1, Denis Priester1, Andreas Ermantraut1, Monika Bäuerle1, Daniel Himmel1, Regina Stroh1, Thorsten Koslowski2, Ivo Leito3, Ingo Krossing1.
Abstract
Utilizing the "ideal" ionic liquid salt bridge to measure Gibbs energies of transfer of silver ions between the solvents water, acetonitrile, propylene carbonate and dimethylformamide results in a consistent data set with a precision of 0.6 kJ mol-1 over 87 measurements in 10 half-cells. This forms the basis for a coherent experimental thermodynamic framework of ion solvation chemistry. In addition, we define the solvent independent pe abs H 2 O - and the E abs H 2 O values that account for the electronating potential of any redox system similar to the pH abs H 2 O value of a medium that accounts for its protonating potential. This E abs H 2 O scale is thermodynamically well-defined enabling a straightforward comparison of the redox potentials (reducities) of all media with respect to the aqueous redox potential scale, hence unifying all conventional solvents' redox potential scales. Thus, using the Gibbs energy of transfer of the silver ion published herein, one can convert and unify all hitherto published redox potentials measured, for example, against ferrocene, to the E abs H 2 O scale.Entities:
Keywords: electrochemistry; ionic liquids; salt bridges; single ion Gibbs transfer energy; thermodynamics
Mesh:
Substances:
Year: 2022 PMID: 35446995 PMCID: PMC9401597 DOI: 10.1002/chem.202200509
Source DB: PubMed Journal: Chemistry ISSN: 0947-6539 Impact factor: 5.020
Figure 1a) The redox system Ag+(solv)/Ag(s) in H2O and in a hypothetical solvent Sh in the presentation of the conventional pHS and SHES scales at a(Ag+,S)=1. The zero points of these scales cannot be discriminated due to the standard states used. They are defined analogously by the infinitely dilute solution of the proton. Nevertheless, the zero points are inevitably different, as each solvent has individual properties; in other words, the standard states are solvent dependent. Thus, the intersolvent comparison of acidity and reducity (reduction power) is not possible. The start of an arrow, (the arrow represents an observable) indicates the zero point of the respective scale. The end of the arrow indicates the standard potential value E S°. In this example, Ag+ seems to be less de‐electronating (oxidizing) in Sh than in H2O. b) The same systems and the system H+(solv)/H2(g) (red line) represented in the PPM. The unifying standard states are defined as the ideal electron gas (peabs 0) and the ideal proton gas (pHabs 0) at standard conditions. The Gibbs energy of hydration ▵solv G°(H+, H2O)=−1104.5 kJ mol−1 is the only anchor used to tie the standard states to the solvent water and thereby to pHabs and peabs, respectively. The relative position of the redox systems in the different solvents can easily be identified. This is due to the knowledge of Gibbs energies of transfer ▵tr G°(i, H2O→Sh) of an ion i from H2O to Sh on the one hand, and due to the unifying standard state serving as a zero point that is valid for all solvents on the other. The transfer energies (indicated by dotted arrows) are the key magnitudes for the realization of an experimental PPM. However, these are elusive quantities so far accessible only with the help of extra‐thermodynamic assumptions (see below). In this example, it follows that Ag+ is indeed more de‐electronating in Sh than in H2O. Note that both dotted red arrows are equivalent, indicating the Gibbs energy of transfer of the proton from water to Sh. If one of the elusive transfer quantities were known, the other could be determined in a thermodynamic cycle. The value is equivalent to the pHabs value being aligned to the zero value of the scale, is defined by Equation (3).
Figure 2Volumes and electrostatic potentials (plotted on an area of constant electron density of 0.01 e Å−3) of the Z− anions used in this work as counterions for the Ag+ ion. The data were obtained from DFT calculations (RI‐BP86/def‐TZVP). The ionic volumes were obtained by optimizations with COSMO and scaled by using the equation V −=1.031 V −,calc+4 Å3 (for more details see ref. [37]).
Figure 3Sketch of the network of the half‐cells, indicated by red digits … , with the solvents S=H2O, AN, PC and DMF at different AgZ‐concentrations (c) in mmol L−1 and with different Z− anions (indicated by colors; Tf=SO2CF3, [PF]=[Al{OC(CF3)3}4]). Overall 87 measurements over 10 half‐cells were performed. Each arrow between two points of the network symbolizes one distinct implementation of cell II. The starting point of the arrows is the right half‐cell and the endpoint the left half‐cell. The numbers in the circles superimposed on the arrows are the measured potential differences of cell II E II in mV with the respective salts AgZ (encoded by colors). Some values are averages. E opt is the optimized potential value with respect to half‐cell 1 as the right half‐cell obtained by the network analysis (see text).
Optimized values Δtr G°(Ag+, S1→S2) as obtained from the network analysis. All energies [kJ mol−1 (mol L−1 scale)]. The range of individually measured values is given where available. Columns 5, 7 and 9 refer to recommended values obtained with extra‐thermodynamic assumptions.[a]
|
S1 |
S2 |
This work |
TATB |
n‐LJP |
Fc[ | ||||
|---|---|---|---|---|---|---|---|---|---|
|
|
|
Opt. |
Range |
Rec. |
Range |
Rec. |
Calc.[b,c] |
Rec. |
Range |
|
AN |
H2O |
25.1 |
(24.9–25.5) |
23.2 |
(19.2–31.4) |
17.1 |
17.7[b,c] |
37.1 |
(31.4–39.4) |
|
H2O |
PC |
15.9 |
(16.3–16.6) |
18.8 |
(−11.7–22.1) |
22.3[a,c] |
21.2[b,c] |
8.6 |
– |
|
AN |
PC |
41.0 |
(39.7–41.8) |
42.0[c] |
– |
39.4 |
38.9[b,c] |
45.7[c] |
– |
|
DMF |
H2O |
21.3 |
(21.8–21.9) |
20.8 |
(13.1‐41.8) |
13.1[a,c] |
11.9[b,c] |
31.1 |
(27.4–31.1) |
|
AN |
DMF |
3.8 |
(3.9–4.3) |
2.4[c] |
– |
4.0 |
5.8[b,c] |
6.0[c] |
– |
|
DMF |
PC |
37.2 |
(36.5–37.0) |
39.6[c] |
– |
35.4[a,c] |
33.1[b,c] |
39.7[c] |
– |
[a] TATB: Δtr G°(TA+)=Δtr G°(TB−) for all S; n‐LJP: neglection of LJPs; Fc: Δtr G°(Fc)=Δtr G°(Fc+) for all S. These are discussed below. [a] Reference solvent AN; [b] reference solvent methanol; [c] calculated from the given column values (in case of [b] with additional values from Table V in ref. [34]), that is, not directly measurable (TATB and Fc methods) or measured (n‐LJP method).
Values of Δtr G° of the IL ions [N2225]+ and [NTf2]− for the transfer from S1→S2 as obtained from calculations at the DLPNO‐CCSD(T)/def2‐QZVPP level of theory including the CPCM solvation method. xII was calculated with Equation (9). Transfer energies in kJ mol−1 (mol L−1 scale).[a]
|
S1 |
S2 |
Δtr
|
xII/mV | |
|---|---|---|---|---|
|
|
|
[N2225]+ |
[NTf2]− |
|
|
AN |
H2O |
−3.28 |
−3.10 |
−0.90 |
|
H2O |
PC |
0.58 |
0.54 |
0.24 |
|
AN |
PC |
−2.69 |
−2.57 |
−0.66 |
|
DMF |
H2O |
−3.05 |
−2.87 |
−0.93 |
|
AN |
DMF |
−0.23 |
−0.24 |
0.03 |
|
DMF |
PC |
−2.46 |
−2.33 |
−0.69 |
[a] The relative permitivities of the solvents for the CPCM method were ϵ r=35.688 (AN), 78.355 (H2O), PC (64.92) and 37.219 (DMF).
A selection of redox systems including some common reference systems in the realm of unified reducity linked to the (Ag+(solv, S)/Ag(s)) values from this work. The physical state of the species is “solvated in the solvent S” (solv,S), if not otherwise stated (g=gaseous, s=solid). Note, that some authors did not specify E° but E°′ or E 1/2. Cc=cobaltocene=Co(η 5‐C5H5)2.
|
Redox system |
|
S |
Ref. |
|---|---|---|---|
|
Ag+/Ag(s) |
0.964 |
PC |
this work |
|
Ag+/Ag(s) |
0.799 |
H2O |
[63] |
|
I2/I− |
0.620 |
H2O |
[63] |
|
Ag+/Ag(s) |
0.579 |
DMF |
this work |
|
I3 −/I− |
0.540 |
H2O |
[64] |
|
Ag+/Ag(s) |
0.539 |
AN |
this work |
|
Fc+/Fc |
0.483 |
AN |
[65] |
|
Fc+/Fc |
0.445 |
PC |
[66] |
|
Fc+/Fc |
0.431 |
DMF |
[67] |
|
H+/H2(g) |
0.413 |
AN |
[68] |
|
Fc+/Fc |
0.400 |
H2O |
[69] |
|
H+/H2(g) |
0.369 |
PC |
[70] |
|
I2/I− |
0.373 |
AN |
[64] |
|
I2/I− |
0.364 |
PC |
[64] |
|
SCEH2O |
0.241 |
H2O |
[71] |
|
AgClH2O |
0.197 |
H2O |
[71] |
|
I3 −/I− |
0.163 |
AN |
[64] |
|
I3 −/I− |
0.135 |
PC |
[64] |
|
Me10Fc+/Me10Fc |
0.109 |
H2O |
[72] |
|
H+/H2(g) |
0.000 |
H2O |
[63] |
|
Me10Fc+/Me10Fc |
−0.027 |
AN |
[72] |
|
Me10Fc+/Me10Fc |
−0.049 |
DMF |
[72] |
|
Me10Fc+/Me10Fc |
−0.050 |
PC |
[72] |
|
H+/H2(g) |
−0.189 |
DMF |
[68] |
|
Cc+/Cc |
−0.85 |
PC |
[73] |
|
Cc+/Cc |
−0.87 |
AN |
[74] |
|
Cc+/Cc |
−0.87 |
DMF |
[73] |
|
Cc+/Cc |
−0.96 |
H2O |
[74] |