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Handbook of Solvents - George Wypych - ChemTech - Ventech!

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10.4 Acid-base equilibria in ionic solvents 627<br />

Hence, the use <strong>of</strong> a majority <strong>of</strong> proposed bases for quantitative studies <strong>of</strong> oxoacidity is not<br />

possible, especially for acids having apparent oxidizing properties (chromates, vanadates,<br />

etc.).<br />

Oxide ions in molten nitrates exist as the so-called pyronitrate ions N 2O 7 4- which was a<br />

strong base with the basicity approximately equal to those for CO 3 2- . 55 The modern point <strong>of</strong><br />

view excludes the existence <strong>of</strong> nitrogen compounds with the coordination number exceeding<br />

3 by oxygen, hence pyronitrate was hardly existing in the mentioned conditions. Indeed,<br />

following oxoanion studies 51 have demonstrated the absence <strong>of</strong> the mentioned ion in basic<br />

nitrate solutions. A possible way for the stabilization <strong>of</strong> O 2- in nitrate melts is the formation<br />

<strong>of</strong> silicates due to reactions with walls <strong>of</strong> the container (usually it is pyrex).<br />

The anomalous behavior <strong>of</strong> the electrode Pt(O 2) has been noted and explained by “peroxide”<br />

function <strong>of</strong> the gas oxygen electrodes (<strong>of</strong> the first type). 57,58 On the contrary to gas<br />

electrodes, metal-oxide electrodes (<strong>of</strong> the second type) were reversible with the slope corresponding<br />

to the reaction:<br />

1/ 2O + 2e<br />

= O<br />

2<br />

2−<br />

[10.4.36]<br />

The acid-base equilibria in complex solutions based on nitrates containing phosphates<br />

and molybdates were attributed 59,60 to the formation <strong>of</strong> heteropolyacids in molten nitrates.<br />

This is confirmed by cryoscopic studies. 61<br />

Some features <strong>of</strong> potentiometric titration techniques in molten salts have been discussed.<br />

62,63 The automatic potentiometric titration described in details 62 consists <strong>of</strong> the following.<br />

A rod, prepared as frozen K2Cr2O7 solution in the melt, was immersed into the melt<br />

containing a base with the constant rate. e.m.f. data were recorded by the recording potentiometer.<br />

Such a routine may be used only for the detection <strong>of</strong> equivalence points in melts<br />

(with accuracy <strong>of</strong> ~3.5 %).<br />

The effect <strong>of</strong> acidic oxides on the thermal stability <strong>of</strong> molten NaNO3 has been investigated.<br />

64 The increase <strong>of</strong> oxide acidity results in the decrease <strong>of</strong> the melt decomposition temperature.<br />

This is explained by the reduction <strong>of</strong> the activation energy <strong>of</strong> the decomposition<br />

owing to fixing oxide ions by acids. But there was also another explanation: decreasing temperature<br />

<strong>of</strong> melt decomposition is caused by the equilibrium shift towards the oxide-ions<br />

and nitrogen oxide formation under the action <strong>of</strong> the acid. Acidic properties <strong>of</strong> oxides decrease<br />

in the sequence SiO2>TiO2>ZrO2>Al2O3>MgO. Potentiometric method 65-67 used metal-oxide electrodes (Nb|Nb2O5, Ta|Ta2O5, Zr|ZrO2) for oxoacidity studies in the nitrate melt. The empirical acidity scale in molten potassium<br />

nitrate at 350 o C was constructed: NH4VO3>NaPO3>NaH2PO4>K2Cr2O7>K2HPO4> Na4P2O7>NaHAsO4>K2CO3>Na2O2. This sequence includes some acids seldom existing in<br />

molten salts. NH4VO3 at 350 o C should be completely transformed into V2O5 with a partial<br />

reduction <strong>of</strong> the latter by ammonia. Acidic salts mentioned were decomposed to corresponding<br />

pyro- and meta-salts. Therefore the scale obtained contains a number <strong>of</strong> errors.<br />

10.4.4.2 Sulphate melts<br />

Sulphate melts are referred to melts with the own acid-base dissociation equilibrium:<br />

2<br />

SO = SO ↑ + O<br />

− 2−<br />

4<br />

3,<br />

l l<br />

[10.4.37]

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