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Handbook of Solvents - George Wypych - ChemTech - Ventech!

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626 Victor Cherginets<br />

Since even the pure salts containing mentioned hydroanions undergo the decomposition<br />

at temperatures much lower then 350 o C with the formation <strong>of</strong> corresponding meta- or<br />

pyro- salts, 68 equilibria [10.4.33] and [10.4.34] hardly take place in the absence <strong>of</strong> water vapor<br />

in atmosphere over the melt.<br />

The acidic properties <strong>of</strong> highest oxides <strong>of</strong> VI Group elements (Cr, Mo, W) were investigated.<br />

23,48,49 Similarly to Group V oxides 43-48 CrO 3 and MoO 3 destructed the nitrate melt<br />

with formation <strong>of</strong> Cr 2O 7 2- and Mo3O 10 2- , respectively. After the complete evolution <strong>of</strong> NO2,<br />

e.m.f. values were close to 0.5 V, what was in a good agreement other studies. 43-48 The<br />

potentiometric titration curves <strong>of</strong> the formed products contained only one drop <strong>of</strong> e.m.f. (or<br />

pO). Chromate and molybdate ions were the final products <strong>of</strong> the neutralization reactions.<br />

WO 3 was weaker acid and did not destruct the nitrate melt. Its titration was the one-stage<br />

process resulting in the tungstate formation. The acidities <strong>of</strong> oxides increased in the order:<br />

WO 3Sr>Ca>Pb <strong>of</strong> basicity decrease. The cation sequence was in a good correlation<br />

with the electronegativity <strong>of</strong> metals. The proposed method <strong>of</strong> investigation had an essential<br />

problem since the acids used for titration fixed oxide ions with the simultaneous<br />

destruction <strong>of</strong> carbonate and formed insoluble chromates and phosphates with the majority<br />

<strong>of</strong> cations studied. As it has been shown, 36,37 the addition <strong>of</strong> Ca 2+ into nitrate melts leads to<br />

the shift <strong>of</strong> the interaction Cr 2O 7 2- -NO3 - to formation <strong>of</strong> nitronium cation and the melt decomposition<br />

although the solution without Ca 2+ is stable. Such shift is explained by formation<br />

<strong>of</strong> slightly insoluble CaCrO 4 in nitrate melt and has no relation to Ca 2+ acidity. It is<br />

referred to the barium position in the sequence that gives evidence <strong>of</strong> the said complexes or<br />

precipitates formation, since their acidic properties are substantially weaker than those <strong>of</strong><br />

Li + . The formation <strong>of</strong> the BaCrO 4 precipitate leads to approaching <strong>of</strong> Ba 2+ acidity to Li +<br />

acidity. Probably, the same reason effected arrangement <strong>of</strong> others alkaline earth metals in<br />

this sequence.<br />

The relative strength <strong>of</strong> different Lux bases in nitrate melts was investigated. 54,55 The<br />

bases studied were divided into two groups: the oxide ion group (OH - ,O 2- ,O 2 2- ) and the carbonate<br />

ion group (CO 3 2- , HCO3 - , (COO)2 2- ,CH3COO - , HCOO - ). The bases belonging to the<br />

first group have been assumed 54,55 to be completely transformed into O 2- .The members <strong>of</strong><br />

the first group <strong>of</strong> bases were weaker than the second group bases. From the thermal data it<br />

may be seen that at experimental temperature (350 o C) all the second group bases are completely<br />

broken down to carbonate. The differences between single bases may be attributed<br />

to reduction properties - organic salts reduce nitrate ions to more basic nitrite ones and favor<br />

the accumulation <strong>of</strong> oxide and carbonate ions in the melt over the stoichiometric ratio.

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