Universidad Complutense de Madrid
E-Prints Complutense

Precipitation of CaCO3 Polymorphs from Aqueous Solutions: The Role of pH and Sulphate Groups

Impacto

Downloads

Downloads per month over past year

Cuesta Mayorga, Iris and Astilleros García-Monge, José Manuel and Fernández-Díaz, Lourdes (2019) Precipitation of CaCO3 Polymorphs from Aqueous Solutions: The Role of pH and Sulphate Groups. Minerals, 9 (3). p. 178. ISSN 2075-163X

[img]
Preview
PDF
Creative Commons Attribution.

3MB

Official URL: https://www.mdpi.com/2075-163X/9/3/178



Abstract

In this work, we aimed to experimentally study the nucleation and growth of CaCO3 phases precipitated from supersaturated aqueous solutions in the presence of varying concentrations of sulphate oxyanion. The experiments were conducted under pH conditions close to neutral (7.6) and by considering a wide range of initial (SO42−)/(CO32−) ratios (0 to approx. 68) in the aqueous solution. We paid special attention to the evolution of the precipitates during ageing within a time framework of 14 days. The mineralogy, morphology, and composition of the precipitates were studied by X-ray diffraction, Fourier transform infrared spectroscopy, scanning electron microscopy, and EDX microanalysis. The concentration of sulphate ions in the reacted aqueous solution was studied by ICPs. The experimental results showed that the mineral composition of the precipitate recovered in each run varied with the (SO42−)/(CO32−) ratio in the parental solution, which influenced the mineral evolution of the precipitates during ageing. We observed that high concentrations of sulphate in the aqueous solution stabilized the vaterite precipitates and inhibited calcite formation. Furthermore, aragonite never precipitated directly from the solution, and it was only formed via a dissolution-precipitation process in solutions with a high (SO42−)/(CO32−) ratio after long reaction times. Finally, gypsum only precipitated after long ageing in those aqueous solutions with the highest concentration of sulphate. The reaction pathways during ageing, the morphology of the calcite crystals, and the composition of vaterite and calcite were discussed considering both kinetic and thermodynamic factors. These results showed a considerably more complex behavior of the system than that observed in experiments conducted under higher pHs and supersaturation levels and lower (SO42−)/(CO32−) ratios in the aqueous phase.


Item Type:Article
Uncontrolled Keywords:CaCO3 polymorphs, sulphate, ageing process, aragonite, gypsum
Subjects:Sciences > Geology > Mineralogy
ID Code:56911
Deposited On:04 Sep 2019 17:40
Last Modified:05 Sep 2019 08:04

Origin of downloads

Repository Staff Only: item control page