Phase Assemblages in Hydrated Portland Cement, Calcined Clay and Limestone Blends From Solid-State 27Al and 29Si MAS NMR, XRD, and Thermodynamic Modeling

Author(s):  
Zhuo Dai ◽  
Wolfgang Kunther ◽  
Sergio Ferreiro ◽  
Duncan Herfort ◽  
Jørgen Skibsted
1999 ◽  
Vol 130 (1) ◽  
pp. 147-156
Author(s):  
Xavier Helluy ◽  
Jörg Kümmerlen ◽  
Christoph Marschner ◽  
Angelika Sebald

1996 ◽  
Vol 118 (1-2) ◽  
pp. 171-181 ◽  
Author(s):  
Cecil Dybowski ◽  
Edward J. Gaffney ◽  
Ali Sayir ◽  
Martin J. Rabinowitz

2019 ◽  
Author(s):  
Przemyslaw Rzepka ◽  
Zoltán Bacsik ◽  
Andrew J. Pell ◽  
Niklas Hedin ◽  
Aleksander Jaworski

Formation of CO<sub>3</sub><sup>2-</sup> and HCO<sub>3</sub><sup>-</sup> species without participation of the framework oxygen atoms upon chemisorption of CO<sub>2</sub> in zeolite |Na<sub>12</sub>|-A is revealed. The transfer of O and H atoms is very likely to have proceeded via the involvement of residual H<sub>2</sub>O or acid groups. A combined study by solid-state <sup>13</sup>C MAS NMR, quantum chemical calculations, and <i>in situ</i> IR spectroscopy showed that the chemisorption mainly occurred by the formation of HCO<sub>3</sub><sup>-</sup>. However, at a low surface coverage of physisorbed and acidic CO<sub>2</sub>, a significant fraction of the HCO<sub>3</sub><sup>-</sup> was deprotonated and transformed into CO<sub>3</sub><sup>2-</sup>. We expect that similar chemisorption of CO<sub>2</sub> would occur for low-silica zeolites and other basic silicates of interest for the capture of CO<sub>2</sub> from gas mixtures.


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