Solution-driven processing of calcium sulfate: The mechanism of the reversible transformation of gypsum to bassanite in brines
Metadatos
Mostrar el registro completo del ítemAutor
Stawski, Tomasz M.; Karafiludis, Stephanos; Pimentel, Carlos; Montes Hernández, German; Kochovski, Zdravko; Bienert, Ralf; Weimann, Karin; Emmerling, Franziska; Scoppola, Ernesto; Van Driessche, Alexander Edgard SuzanneEditorial
Elsevier
Materia
Gypsum Bassanite Calcium sulfate
Fecha
2024-01-29Referencia bibliográfica
Stawski, Tomasz M., et al. Solution-driven processing of calcium sulfate: The mechanism of the reversible transformation of gypsum to bassanite in brines. Journal of Cleaner Production 440 (2024) 141012 [10.1016/j.jclepro.2024.141012]
Patrocinador
Junta de Andalucia (Spain) through project PROYEXCEL_00771; European Union’s Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No. 101021894 [CARS-CO2]Resumen
Here, we show that calcium sulfate dihydrate (gypsum) can be directly, rapidly and reversibly converted to
calcium sulfate hemihydrate (bassanite) in high salinity solutions (brines). The optimum conditions for the
efficient production of bassanite in a short time (<5 min) involve the use of brines with c(NaCl) > 4 M and
maintaining a temperature, T > 80 ºC. When the solution containing bassanite crystals is cooled down to around
room temperature, eventually gypsum is formed. When the temperature is raised again to T > 80 ºC, bassanite is
rapidly re-precipitated. This contrasts with the better-known behaviour of the bassanite phase in low-salt environments.
In low-salinity aqueous solutions, bassanite is considered to be metastable with respect to gypsum
and anhydrite, and therefore gypsum-to-bassanite conversion does not occur in pure water. Interestingly, the
high-salinity transformation of gypsum-to-bassanite has been reported by many authors and used in practice for
several decades, although its very occurrence actually contradicts numerical thermodynamic predictions
regarding solubility of calcium sulfate phases. By following the evolution of crystalline phases with in situ and
time-resolved X-ray diffraction/scattering and Raman spectroscopy, we demonstrated that the phase stability in
brines at elevated temperatures was inaccurately represented in the thermodynamic databases. Most notably for
c(NaCl) > 4 M, and T > 80 ºC gypsum becomes readily more soluble than bassanite, which induces the direct
precipitation of the latter from gypsum. The fact that these transformations are controlled by the solution provides
extensive opportunities for precise manipulation of crystal formation. Our experiments confirmed that
bassanite remained the sole crystalline phase for many hours before reverting into gypsum. This property is
extremely advantageous for practical processing and efficient crystal extraction in industrial scenarios.