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Marble Powder and Dolomite for CO2 capture and in-situ XRD analysis

https://doi.org/10.3390/ma14164379

“The use of wastes of marble powder (WMP) and dolomite as sorbents for CO2 capture is extremely promising to make the Ca-looping (CaL) process a more sustainable and eco-friendly technology. ”

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Table 1 shows that the WMP, such as the limestone, is mainly composed of CaO and CO2. ASTM C119-16 [54] classifies limestone and marble in different groups of rocks, marble is a carbonate rock that has acquired a distinctive crystalline texture by recrystallization, usually due to high heat and pressure during metamorphism, and is mainly composed of the carbonate minerals calcite and dolomite, individually or in combination. Dolomite belongs to the limestone group and, besides CO2, contains two main oxides in its composition: CaO and MgO. A ratio of Ca/Mg (wt.%) of 2.4 was obtained, so this sorbent is classified as a calcitic dolomite. Compared to the WMP, lower amounts of Si, Al and Fe were found in dolomite.”

“The carbonation–calcination cycles using WMP and dolomite as sorbents were performed within an in-situ XRD chamber, and the evolution of CaCO3 and CaO crystalline phases present in each one of the materials samples was recorded in the XRD diffractograms in the range 28–39° in 2θ.

Figure 3a,b show results obtained when the calcination was performed under N2 at 800 °C. In the case of WMP (Figure 3a), the relative amount of CaO that is not converted to CaCO3 at the end of the carbonation stage increases with the number of carbonation cycles (black rectangle line). However, in the case of dolomite (Figure 3b), the amount of CaO that is not carbonated after the carbonation stage (dotted line rectangle), though increasing, is less significant.”
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Figure 3. in-situ XRD diffractograms of WMP (a) and dolomite (b) obtained along the carbonation–calcination cycles: carbonation with 15% of CO2 at 700 °C and calcination with 100% of N2 at 800 °C.”

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