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The relative humidity and saturated water vapor pressure resulted from the reversible equilibrium dissociation of crystalline NaBH4·2H2O in the temperature range 0–36°C were determined. Based on the data obtained for NaBH4·2H2O, the equilibrium water vapor pressure as a function of temperature ln P = –6567.1T–1 + 23.863, enthalpy ∆Н0 = 54 ± 0.8 kJ mol–1 and entropy ∆S0 =198 ± 2 J mol–1 K–1 of NaBH4·2H2O dissociation into NaBH4 and H2O, standard enthalpy ∆H°= –783 kJ mol–1 and entropy ∆S° = 281 J mol–1 K–1 of formation of NaBH4·2H2O were calculated. An equation was derived for the humidity vs. temperature, which determines the regions of NaBH4·2H2O formation or its dissociation Rh = 0.334t + 17.5. It was shown that the pressure of saturated water vapor over a concentrated NaBH4 solution (30 wt %) at temperatures up to 45°C has higher values compared to NaBH4·2H2O samples synthesized by two different methods.
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Shikhovtsev et al. (2023) studied this question.
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