Effect ofInitial Potassium Catalyst Concentrationon Its Activity and Fate in CO<sub>2</sub> Gasification of LigniteChar

K-catalyzed gasification of char and carbon has been studied for more than 40 years while many different types of relationships between specific rate of gasification (<i>r</i><sub>sp</sub> = dXdt(1−X), <i>X</i>; char conversion) and K concentration in gasifying char/carbon (<i>C</i><sub>K</sub>) have been reported. This work explored the mechanism causing such diversity in the <i>r</i><sub>sp</sub>–<i>C</i><sub>K</sub> profile. An ash-free lignite was impregnated with K<sub>2</sub>CO<sub>3</sub>, devolatilized, and then gasified with CO<sub>2</sub> at 800 °C and <i>C</i><sub>K</sub> at the start of gasification (<i>C</i><sub>K,0</sub>) of 0.15–2.66 mol-K/kg-daf-char. <i>C</i><sub>K</sub> was accurately determined by measuring the K volatilization rate as a function of <i>X</i>. For <i>C</i><sub>K,0</sub> = 0.15, <i>r</i><sub>sp</sub> increased linearly with <i>C</i><sub>K</sub> while the K catalyst activity (<i>k</i><sub>c</sub>′ = <i>r</i><sub>sp</sub>/<i>C</i><sub>K</sub>) remained unchanged at 0.013 min<sup>–1</sup> mol-K/kg-daf-char<sup>–1</sup>. The K species underwent transformation to much more active catalyst (<i>k</i><sub>c</sub>′ ≈ 0.130 min<sup>–1</sup> mol-K/kg-daf-char<sup>–1</sup>) for <i>C</i><sub>K,0</sub> = 0.64–2.66, where the <i>r</i><sub>sp</sub>–<i>C</i><sub>K</sub> profile was independent of <i>C</i><sub>K,0</sub>, and <i>r</i><sub>sp</sub> reached an upper limit due to saturation of gasifying char matrix with the catalyst. The catalyst transformation also occurred for <i>C</i><sub>K,0</sub> = 0.28–0.39 while <i>k</i><sub>c</sub>′ of the transformed catalyst was steady at 0.03–0.08 depending on <i>C</i><sub>K,0</sub>. Thus, the variety of the <i>r</i><sub>sp</sub>–<i>C</i><sub>K</sub> profile arose from that in <i>C</i><sub>K,0</sub>. Higher <i>C</i><sub>K,0</sub> led to greater d<i>X</i>/d<i>t</i> and then d<i>C</i><sub>K</sub>/d<i>t</i> under a steady supply of oxygen (as CO<sub>2</sub>) that anchored K on the char surface, allowing atomic-level dispersed C–O–K and/or K<sub>2</sub>CO<sub>3</sub> to transform into clusters consisting of K<sub><i>x</i></sub>O<sub><i>y</i></sub>(CO<sub>2</sub>)<sub><i>z</i></sub> (<i>y</i>/<i>x</i> > 0.5, <i>z</i>/<i>x</i> ≈ 0.16). The most active cluster was formed even during the period of devolatilization for <i>C</i><sub>K,0</sub> > 1.69. Increasing <i>C</i><sub>K,0</sub> from 0.15 to 2.66 (by a factor of 18) resulted in shortening of the time required for X = 0.50 and 0.99 by factors as large as 1/200 and 1/100, respectively, due to the above-mentioned <i>C</i><sub>K,0</sub> effect on the <i>r</i><sub>sp</sub>–<i>C</i><sub>K</sub> relationship.

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Figshare
Published
2025-03-22
DOI
https://doi.org/10.1021/acs.energyfuels.4c05914.s001
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Thermochemical Biomass Conversion Processes
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article

Effect ofInitial Potassium Catalyst Concentrationon Its Activity and Fate in CO2 Gasification of LigniteChar

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Thermochemical Biomass Conversion Processes
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Effect ofInitial Potassium Catalyst Concentrationon Its Activity and Fate in CO2 Gasification of LigniteChar

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Abstract

K-catalyzed gasification of char and carbon has been studied for more than 40 years while many different types of relationships between specific rate of gasification (<i>r</i><sub>sp</sub> = dXdt(1−X), <i>X</i>; char conversion) and K concentration in gasifying char/carbon (<i>C</i><sub>K</sub>) have been reported. This work explored the mechanism causing such diversity in the <i>r</i><sub>sp</sub>–<i>C</i><sub>K</sub> profile. An ash-free lignite was impregnated with K<sub>2</sub>CO<sub>3</sub>, devolatilized, and then gasified with CO<sub>2</sub> at 800 °C and <i>C</i><sub>K</sub> at the start of gasification (<i>C</i><sub>K,0</sub>) of 0.15–2.66 mol-K/kg-daf-char. <i>C</i><sub>K</sub> was accurately determined by measuring the K volatilization rate as a function of <i>X</i>. For <i>C</i><sub>K,0</sub> = 0.15, <i>r</i><sub>sp</sub> increased linearly with <i>C</i><sub>K</sub> while the K catalyst activity (<i>k</i><sub>c</sub>′ = <i>r</i><sub>sp</sub>/<i>C</i><sub>K</sub>) remained unchanged at 0.013 min<sup>–1</sup> mol-K/kg-daf-char<sup>–1</sup>. The K species underwent transformation to much more active catalyst (<i>k</i><sub>c</sub>′ ≈ 0.130 min<sup>–1</sup> mol-K/kg-daf-char<sup>–1</sup>) for <i>C</i><sub>K,0</sub> = 0.64–2.66, where the <i>r</i><sub>sp</sub>–<i>C</i><sub>K</sub> profile was independent of <i>C</i><sub>K,0</sub>, and <i>r</i><sub>sp</sub> reached an upper limit due to saturation of gasifying char matrix with the catalyst. The catalyst transformation also occurred for <i>C</i><sub>K,0</sub> = 0.28–0.39 while <i>k</i><sub>c</sub>′ of the transformed catalyst was steady at 0.03–0.08 depending on <i>C</i><sub>K,0</sub>. Thus, the variety of the <i>r</i><sub>sp</sub>–<i>C</i><sub>K</sub> profile arose from that in <i>C</i><sub>K,0</sub>. Higher <i>C</i><sub>K,0</sub> led to greater d<i>X</i>/d<i>t</i> and then d<i>C</i><sub>K</sub>/d<i>t</i> under a steady supply of oxygen (as CO<sub>2</sub>) that anchored K on the char surface, allowing atomic-level dispersed C–O–K and/or K<sub>2</sub>CO<sub>3</sub> to transform into clusters consisting of K<sub><i>x</i></sub>O<sub><i>y</i></sub>(CO<sub>2</sub>)<sub><i>z</i></sub> (<i>y</i>/<i>x</i> > 0.5, <i>z</i>/<i>x</i> ≈ 0.16). The most active cluster was formed even during the period of devolatilization for <i>C</i><sub>K,0</sub> > 1.69. Increasing <i>C</i><sub>K,0</sub> from 0.15 to 2.66 (by a factor of 18) resulted in shortening of the time required for X = 0.50 and 0.99 by factors as large as 1/200 and 1/100, respectively, due to the above-mentioned <i>C</i><sub>K,0</sub> effect on the <i>r</i><sub>sp</sub>–<i>C</i><sub>K</sub> relationship.

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Thermochemical Biomass Conversion Processes
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