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Characterization and Exploration of Placket–Burman-Designed Porous Calcium Carbonate (Vaterite) Microparticles

[Image: see text] The objective of the research was to identify significant variables that impact the porosity-related properties of CaCO(3) particles. The Placket–Burman design was employed to screen multiple variables, including pH, molar concentrations of calcium chloride and sodium carbonate, te...

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Detalles Bibliográficos
Autores principales: Singh, Avi, Das, Sabya Sachi, Verma, Priya Ranjan Prasad, Ruokolainen, Janne, Kesari, Kavindra Kumar, Singh, Sandeep Kumar
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2023
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10688156/
https://www.ncbi.nlm.nih.gov/pubmed/38046299
http://dx.doi.org/10.1021/acsomega.3c05050
Descripción
Sumario:[Image: see text] The objective of the research was to identify significant variables that impact the porosity-related properties of CaCO(3) particles. The Placket–Burman design was employed to screen multiple variables, including pH, molar concentrations of calcium chloride and sodium carbonate, temperature, concentration of Gelucire 44/14, Cremophor RH40, Solutol HS15, Labrasol, mixing rate, reaction time, and order of addition. The response variables were surface area, pore radius, and pore volume. Influential methodologies such as XRD, FTIR, Raman spectroscopy, and TGA were utilized to validate the precipitate type. The BET surface area ranged from 1.5 to 16.14 m(2)/g, while the pore radius varied from 2.62 to 6.68 nm, and the pore volume exhibited a range of 2.43 to 37.97 cc/gm. Vaterite structures with spherical mesoporous characteristics were observed at high pH, whereas calcite formations occurred at low pH. The order of addition impacted the surface area but did not affect the pore volume. To maximize the surface area, a lower reaction time and molar concentrations of sodium carbonate were found to be advantageous. The pore radius was influenced by the pH, surfactants, and reaction conditions. The sediments were categorized based on the percentage of vaterite formation. The instrumental techniques effectively characterized the precipitates and provided a valuable complementary analysis.