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

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440<br />

B Ionic strength corrections<br />

0.509 Im<br />

D =<br />

1 + 1.5 I<br />

m<br />

(B.8)<br />

Δ ε = ε( qnm , , , N or X) + nε(H, X) − qε(N, L) − mε(M, X) (B.9)<br />

Here ( mzM − qzL<br />

− n)<br />

, z M and z L are the charges <strong>of</strong> the complex,<br />

MmL q(OH)<br />

n<br />

, the metal ion M and the ligand L, respectively.<br />

Equilibria involving H 2 O(l) as a reactant or product require a correction for<br />

the activity <strong>of</strong> water, a<br />

HO. The activity <strong>of</strong> water in an electrolyte mixture can be calculated<br />

as:<br />

2<br />

−φm<br />

∑ mk<br />

k<br />

log<br />

10<br />

aH2O = (B.10)<br />

ln(10)<br />

−1<br />

M<br />

HO 2<br />

where φ<br />

m<br />

is the osmotic coefficient <strong>of</strong> the mixture, M HO 2<br />

is the molar mass <strong>of</strong> H 2 O,<br />

and the summation extends over all solute species k with molality m k present in the<br />

solution. In the presence <strong>of</strong> an ionic medium NX as the dominant species, Eq. (B.10)<br />

can be simplified by neglecting the contributions <strong>of</strong> all minor species, i.e., the reacting<br />

ions. Hence, for a 1:1 electrolyte <strong>of</strong> ionic strength I m ≈ m NX , Eq. (B.10) becomes:<br />

− 2mNX<br />

φm<br />

log<br />

10<br />

aH2O = (B.11)<br />

ln(10)<br />

−1<br />

M<br />

HO 2<br />

Alternatively, water activities can be taken from Table B-1. These have been<br />

calculated for the most common ionic media at various concentrations applying Pitzer’s<br />

ion interaction model and the interaction parameters given in [1991PIT]. Data in italics<br />

have been calculated for concentrations beyond the validity <strong>of</strong> the parameter set applied.<br />

These data are therefore extrapolations and should be used with care.<br />

Values <strong>of</strong> osmotic coefficients for single electrolytes have been compiled by<br />

various authors, e.g., Robinson and Stokes [1959ROB/STO]. The activity <strong>of</strong> water can<br />

also be calculated from the known activity coefficients <strong>of</strong> the dissolved species. In the<br />

presence <strong>of</strong> an ionic medium, Nν X ,<br />

+ ν <strong>of</strong> a concentration much larger than those <strong>of</strong> the<br />

−<br />

reacting ions, the osmotic coefficient can be calculated according to Eq. (B.<strong>12</strong>) (cf. Eqs.<br />

(23-39), (23-40) and (A4-2) in [1961LEW/RAN]).<br />

Aln(10) z z<br />

1 − φ =<br />

⎡<br />

1+ Ba I − 2ln(1 + Ba I ) −<br />

1<br />

⎣<br />

+ −<br />

m<br />

⎢<br />

3<br />

j m j m<br />

Im( Baj) ⎢<br />

1+<br />

Baj Im<br />

ε<br />

νν<br />

+ −<br />

− ln(10) (N,X) mNX<br />

⎜ ⎟<br />

ν+ + ν−<br />

⎛<br />

⎝<br />

⎞<br />

⎠<br />

⎤<br />

⎥<br />

⎥⎦<br />

(B.<strong>12</strong>)<br />

with the general term Ba j = 1.5 kg ½·mol –½ , which is mainly used in NEA reviews (cf.,<br />

Section B.1.2), rather than the implied Ba j = 1.0 kg ½·mol –½ in the expressions in Lewis<br />

and Randall, and ν<br />

+<br />

and ν<br />

−<br />

are the number <strong>of</strong> cations and anions in the salt formula<br />

( ν z = ν z ) and in this case:<br />

+ + − −<br />

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

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