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

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VIII.1 Halide compounds<br />

147<br />

SnCl 2 (cr) + 2 H 2 O(l) → SnCl 2·2H 2 O(cr)<br />

an entropy change <strong>of</strong> – 61.59 J·K –1·mol –1 .<br />

(VIII.1)<br />

From calorimetric dissolution experiments <strong>of</strong> anhydrous tin(II) chloride and its<br />

dihydrate in aqueous HCl containing H 2 O 2 Vasiliev et al. [1973VAS/VAS2] determined<br />

the standard enthalpies <strong>of</strong> formation:<br />

anhydrous tin(II) chloride:<br />

f<br />

ο<br />

m<br />

tin(II) chloride dihydrate:<br />

f<br />

Δ H (SnCl 2 , cr, 298.15 K) = − (327.9 ± 2.2) kJ·mol –1<br />

ο<br />

m<br />

Δ H (SnCl 2 .2H 2 O, cr, 298.15 K) = − (918.26 ± 1.42) kJ·mol –1 .<br />

These values are selected.<br />

This yields:<br />

Δ G (SnCl 2·2H 2 O, cr, 298.15 K) = − (760.68 ± 1.49) kJ·mol –1 .<br />

f<br />

ο<br />

m<br />

From the difference <strong>of</strong> the formation enthalpies using the same value <strong>of</strong> the<br />

standard enthalpy <strong>of</strong> formation <strong>of</strong> water as the authors (= − 285.829 kJ·mol –1 ) for<br />

Reaction (VIII.1) an enthalpy change <strong>of</strong> − 18.7 kJ·mol –1 is obtained. Combining the<br />

entropy and enthalpy change the standard Gibbs energy <strong>of</strong> hydration becomes<br />

− 0.34 kJ·mol –1 . However, this value means that regardless <strong>of</strong> speciation the dihydrate<br />

would never exist as an equilibrium phase in aqueous solutions.<br />

According to Section VIII.2.2.1, a solution saturated with tin(II) chloride<br />

dihydrate is <strong>12</strong>.3 molal at 25 °C. Assuming that this solution would be in equilibrium<br />

also with the anhydrous phase the equilibrium constant <strong>of</strong> Reaction (VIII.2) could be<br />

calculated.<br />

SnCl 2 (cr) + 2 H 2 O(l) SnCl 2·2H 2 O(s).<br />

(VIII.2)<br />

From the value <strong>of</strong> the Gibbs energy <strong>of</strong> hydration <strong>of</strong> − 0.34 kJ·mol –1 the<br />

equilibrium water activity <strong>of</strong> Reaction (VIII.2) would be 0.934, which is much too high.<br />

With the mole fraction <strong>of</strong> water x(w) = 0.819 in the saturated solution and even in case<br />

<strong>of</strong> an ideal solution a Δ rGm<br />

= 2RT ln(0.819) = − 0.99 kJ·mol –1 would be nessecary to<br />

enable formation <strong>of</strong> the dihydrate. Since the real solution has water activity coefficients<br />

below 1 the nessecary Δ r G m must be more negative. Also the equilibrium relative<br />

humidity above the solid hydrate would be 93.4% according to the Gibbs energy <strong>of</strong><br />

hydration, which seems to be too high for a bivalent metal halide.<br />

A later calorimetric work <strong>of</strong> Vasiliev et al. [1976VAS/KOK] yields even a less<br />

negative value <strong>of</strong> the hydration enthalpy (approx. – (16.7 ± 1.7) kJ·mol –1 ) comparing<br />

directly the dissolution enthalpies <strong>of</strong> the anhydrous salt and the dihydrate obtained by<br />

formal integration <strong>of</strong> the Cp<br />

( T ) function from the measurements <strong>of</strong> [1974MAT/OGU].<br />

In conclusion the entropy <strong>of</strong> the dihydrate is maybe too negative by at least 3 to<br />

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

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