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Chemical Thermodynamics of Tin - Volume 12 - OECD Nuclear ...

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22 II Standards, conventions and contents <strong>of</strong> the tables<br />

In addition, Δ<br />

rG ο<br />

m<br />

(II.26) = 0, Δ<br />

rH ο<br />

m(II.26) = 0, Δ<br />

rS ο<br />

m<br />

(II.26) = 0 by definition,<br />

at all temperatures, and therefore Δ<br />

rG ο<br />

m(II.25) = Δ<br />

rG ο<br />

m(II.24). From Δ<br />

rG ο<br />

m(II.26) and<br />

the values given at 298.15 K in selected auxiliary data for H 2 (g) and H + , the corresponding<br />

values for e – can be calculated to be used in thermodynamic cycles involving half<br />

cell reactions. The following equations describe the change in the redox potential <strong>of</strong><br />

Reaction (II.24), if and a are equal to unity (cf. Eq. (II.22)):<br />

p<br />

H +<br />

2 H<br />

⎛<br />

E(II.24) = E ο 2+<br />

Fe<br />

(II.24) – RT ln a ⎞<br />

⎜a<br />

⎟<br />

3+<br />

⎝ Fe ⎠<br />

(II.31)<br />

For the standard hydrogen electrode a e<br />

− = 1 (by the convention expressed in<br />

Eq. (II.30)), while rearrangement <strong>of</strong> Eq. (II.29) for the half cell containing the iron perchlorates<br />

in cell (II.23) gives:<br />

⎛a<br />

−log10 a =<br />

e − log10<br />

K ο 2+<br />

⎞<br />

Fe<br />

(II.25) – log10<br />

⎜<br />

a ⎟<br />

3+<br />

⎝ Fe ⎠<br />

and from Eq. (II.27):<br />

⎛a<br />

−log10 a =<br />

e − log10<br />

K ο 2+<br />

⎞<br />

Fe<br />

(II.24) – log10<br />

⎜<br />

a ⎟<br />

3+<br />

⎝ Fe ⎠<br />

(II.32)<br />

and<br />

F<br />

−log 10<br />

a − =<br />

E (II.24)<br />

e<br />

RT ln(10)<br />

(II.33)<br />

which is a specific case <strong>of</strong> the general equation (II.28).<br />

The splitting <strong>of</strong> redox reactions into two half cell reactions by introducing the<br />

−<br />

symbol “ e ”, which according to Eq. (II.27) is related to the standard electrode<br />

potential, is arbitrary, but useful (this e – notation does not in any way refer to solvated<br />

electrons). When calculating the equilibrium composition <strong>of</strong> a chemical system, both<br />

+<br />

“ e − ”, and H can be chosen as components and they can be treated numerically in a<br />

similar way: equilibrium constants, mass balance, etc. may be defined for both.<br />

+<br />

However, while H represents the hydrated proton in aqueous solution, the above<br />

equations use only the activity <strong>of</strong> “ e − −<br />

”, and never the concentration <strong>of</strong> “ e ”.<br />

Concentration to activity conversions (or activity coefficients) are never needed for the<br />

electron (cf. Appendix B, Example B.3).<br />

In the literature on geochemical modelling <strong>of</strong> natural waters, it is customary to<br />

represent the “electron activity” <strong>of</strong> an aqueous solution with the symbol “pe” or “pε”<br />

( =− log a 10 − ) by analogy with pH ( = − log +<br />

e 10<br />

a ), and the redox potential <strong>of</strong> an<br />

H<br />

aqueous solution relative to the standard hydrogen electrode is usually denoted by either<br />

“Eh” or “ E H<br />

” (see for example [1981STU/MOR], [1982DRE], [1984HOS],<br />

[1986NOR/MUN]).<br />

In this review, the symbol E ο ' is used to denote the so-called “formal<br />

potential” [1974PAR]. The formal (or “conditional”) potential can be regarded as a<br />

CHEMICAL THERMODYNAMICS OF TIN, ISBN 978-92-64-99206-1, © <strong>OECD</strong> 20<strong>12</strong>

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