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

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118<br />

VII <strong>Tin</strong> oxygen and hydrogen compounds and complexes<br />

<strong>Tin</strong>(II) oxide decomposes at ambient pressure at temperatures above 500 K<br />

into metallic tin and an intermediate tin oxide either according to disproportionation<br />

Reactions (VII.11) and (VII.<strong>12</strong>) [1947SPA/KOH]<br />

4 SnO → Sn 3 O 4 + Sn (VII.11)<br />

Sn 3 O 4 → 2 SnO 2 + Sn<br />

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

or according to disproportionation Reactions (VII.13) and (VII.14) [1973MUR/TRO]<br />

3 SnO → Sn 2 O 3 + Sn (VII.13)<br />

2 Sn 2 O 3 → 3 SnO 2 + Sn. (VII.14)<br />

The intermediate reaction products could not be separated as pure phases due<br />

to their nano-crystalline nature. As indicated by Reactions (VII.11) and (VII.13) the<br />

stoichiometry <strong>of</strong> the intermediate phase is still under discussion. Sn 3 O 4 , Sn 2 O 3 , Sn 2 O 6 or<br />

Sn 5 O 8 are considered as possible intermediates [2005GIE/POR], [2008SEK/TOG],<br />

[2010TAN/SEK]. A first structural study by electron diffractometry yielded a triclinic<br />

unit cell for a suggested stoichiometry Sn 3 O 4 [1967LAW]. From a recent precession<br />

electron diffraction study [2010WHI/MOR] the complete crystal structure was derived<br />

confirming the unit cell <strong>of</strong> [1967LAW] and the epitaxial relationships between the<br />

various oxide structures <strong>of</strong> tin. From coulometric titrations in a high-temperature<br />

galvanic cell Yang et al. [1994YAN/SUI] derived a temperature function for the Gibbs<br />

energy <strong>of</strong> formation <strong>of</strong> Sn 3 O 4 , which was used subsequently in phase diagram modeling<br />

<strong>of</strong> the system SnO-SnO 2 [2003CAH/DAV]. Although stoichiometry and structure <strong>of</strong> the<br />

elusive intermediate tin oxides Sn 3 O 4 and Sn 2 O 3 have been studied and an attempt was<br />

made to ascertain thermodynamic properties <strong>of</strong> Sn 3 O 4 , the latter do not qualify for<br />

selection <strong>of</strong> standard values in this review.<br />

SnO 2 occurs naturally as the mineral cassiterite and is the main ore <strong>of</strong> tin.<br />

Cassiterite has the rutile-type structure [1964WYC] (tetragonal, space group<br />

P4(2)/mmm, a = 4.7373 Å, c = 3.1864 Å, Z = 2, unit cell volume = 71.51 Å 3 ).<br />

Cassiterite dissolves easily in alkali hydroxides; from these solutions brucite like<br />

hydroxides such as K 2 Sn(OH) 6 [1976HON/ZUC] can be crystallised. Double oxides<br />

may form by combination <strong>of</strong> K 2 O and SnO 2 (K 4 SnO 4 , K 2 Sn 3 O 7 and K 2 SnO 3 ). A mixed<br />

valence oxide Sn 3 O 4 has also been reported [1984GRE/EAR]. The structure is triclinic<br />

with space group P1(2) and V cell = 233.56 Å 3 .<br />

VII.2.2<br />

SnO(cr)<br />

VII.2.2.1 Enthalpy <strong>of</strong> formation <strong>of</strong> SnO(cr)<br />

Humphrey and O'Brien [1953HUM/OBR] determined the enthalpy <strong>of</strong> formation <strong>of</strong><br />

ο<br />

SnO(cr) comparatively early. They obtained a value <strong>of</strong> Δ fHm(SnO, cr, 298.15 K) =<br />

− (286.00 ± 1.34) kJ·mol –1 from the heat <strong>of</strong> combustion <strong>of</strong> tin.<br />

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

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