https://ogma.newcastle.edu.au/vital/access/ /manager/Index ${session.getAttribute("locale")} 5 Insights into chemical stability of Mg-silicates and silica in aqueous systems using <sup>25</sup>Mg and <sup>29</sup>Si solid-state MAS NMR spectroscopy: Applications for CO<inf>2</inf> capture and utilisation https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:49540 Mon 22 May 2023 08:45:16 AEST ]]> The utilisation of feed and byproducts of mineral carbonation processes as pozzolanic cement replacements https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:37516 Mon 15 Feb 2021 11:37:42 AEDT ]]> Structure of silica polymers and reaction mechanism for formation of silica-rich precipitated phases in direct aqueous carbon mineralization https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:38019 29Si solid-state nuclear magnetic resonance (29Si SS NMR), inductively coupled plasma-optical emission spectrometry (ICP-OES), and matrix-assisted laser desorption ionization time-of-flight mass spectrometry (MALDI-TOF MS) to characterize carbonation products and to understand the mechanism of formation and the structure of silica-rich byproducts. Thermodynamic analysis predicts the formation of magnesite and amorphous silica in the process of direct aqueous carbonation of heat-activated lizardite under the experimental conditions studied. Characterization of carbonation products disclosed the presence of magnesite, amorphous silica, and magnesium silicate phases. Analysis of supernatant solutions obtained from direct aqueous carbonation by MALDI spectroscopy showed the presence of silica polymers, which precipitate during the carbonation experiments. The precipitated amorphous silica on the surface of reacting particles was found to subsequently adsorb the dissolved magnesium (Mg) from the solution to form a magnesium silicate phase.]]> Fri 23 Jul 2021 15:47:33 AEST ]]>