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Handbook of Solvents - George Wypych - ChemTech - Ventech!

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21.3 Oxide solubilities in ionic melts 1485<br />

from melt took place not only because <strong>of</strong> the cation acidity but owing to formation <strong>of</strong> new<br />

phase - the precipitate <strong>of</strong> the oxide. Therefore, works in which the estimations <strong>of</strong> cation<br />

acidities were based on measurements <strong>of</strong> changes in oxide concentration before and after<br />

cation addition 3 or by interactions between, e.g., carbonates with Lux acids 4,5 contained distorted<br />

results. The latter works 4,5 contain the additional error - insoluble metal carbonates<br />

MeCO 3 after interaction with acid K 2Cr 2O 7 4 or NaPO3 5 were transformed into insoluble<br />

chromates or phosphates - all reactions were heterogeneous. The above may be also referred<br />

to works <strong>of</strong> Slama 6,7 where cation acidities were estimated on the base <strong>of</strong> reactions<br />

2+<br />

− +<br />

Me + NO = MeO ↓ + NO<br />

[21.3.6]<br />

3 2<br />

+ −<br />

NO + NO = 2NO<br />

↑ + O<br />

[21.3.7]<br />

2 3 2<br />

1 2 2<br />

there was no evidence <strong>of</strong> homogeneity <strong>of</strong> reaction [21.3.6].<br />

The mentioned method seems to have no wide usage for studying behavior <strong>of</strong> oxides<br />

in molten salts, solubility studies by isothermal saturation and potentiometric titration<br />

methods are more precise and informative.<br />

From the listed above scheme <strong>of</strong> equilibria [21.3.1-21.3.4] it follows that the fixation<br />

<strong>of</strong> oxide ions by metal cations is in common case a heterogeneous process resulting in the<br />

formation <strong>of</strong> a new phase and cation acidity may have no connection with the completeness<br />

<strong>of</strong> interaction Me 2+ -O 2- in molten salts.<br />

From eq. [21.3.1] it is clear that molecular oxide concentration in the saturated solution<br />

is not dependent on the constituent ion concentrations but connected with the precipitate<br />

properties, mainly with the molar surface <strong>of</strong> the deposit, σ.<br />

Since the concentration <strong>of</strong> the non-dissociated oxide in the saturated solution, as a<br />

rule, is hardly determined, for practical purposes the solubility product, the magnitudes <strong>of</strong><br />

PMeO (used below pP≡-logP),<br />

P = a a ≈m<br />

m<br />

MeO 2+ 2− 2+ 2 −<br />

[21.3.8]<br />

Me O Me O<br />

are usually employed for the description <strong>of</strong> the saturated solutions. The known values <strong>of</strong><br />

P MeO and K MeO give possibility to estimate the concentration <strong>of</strong> the non-dissociated oxide,<br />

s MeO, in the saturated solution:<br />

s<br />

MeO<br />

PMeO<br />

= [21.3.9]<br />

K<br />

MeO<br />

It should be noted, however, that there was no reliable method for determining dissociation<br />

constants and sMeO. Let us consider two generally accepted methods for oxide solubility<br />

determinations.<br />

21.3.1.1 Isothermal saturation method<br />

This method is simple enough and includes some modifications:<br />

1. placing baked sample <strong>of</strong> the oxide in the melt-solvent and regular tests <strong>of</strong> the metal<br />

concentration in the melt up to the saturation. Known test routines are either radiochemical 8<br />

or complexonometric 9 analysis <strong>of</strong> cooled samples <strong>of</strong> the saturated solutions;

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