https://doi.org/10.1002/cssc.202002078
“A crucial aspect of the kinetics of the carbonation reaction is the growth mechanism of the CaCO3 product on the CaO surface. Hypothetically, CaCO3 can grow on CaO as a uniform layer, in the form of islands or in a combination of both modes.34, 43 A study by Li et al.,34 in which CaO single crystals were carbonated at different temperatures and subsequently analyzed by AFM, tentatively indicates that CaCO3 starts to grow in the form of islands, which eventually merge. As displayed in Figure 4a, the size and distribution of the CaCO3 islands depends on the carbonation temperature. Higher carbonation temperatures result in larger islands and lower island densities. At high conversions, the islands have merged into a CaCO3 layer that fully covers the CaO surface as visualized by FIB-TEM (Figure 4c).44 Figure 4c shows a CaO particle covered by a CaCO3 layer with a thickness of about 90 nm. A visualization of the morphology of the product layer at the end of the kinetically-controlled reaction regime has not been reported yet, due to the difficulty to ‘freeze’ the reaction exactly at the transition from the kinetically-controlled to the diffusion-controlled reaction regime.”
“Figure 4 AFM graphs of CaO single crystals after treatment in CO2 at (a) 500 °C and (b) 600 °C. Adapted with permission from [34]; copyright American Chemical Society, 2012 (c) FIB-TEM image showing the CaCO3 product layer. Adapted with permission from Ref. [44]; copyright Royal Society of Chemistry, 2019.”