TY - JOUR
T1 - Analysis of chemical reaction between Li4SiO4 and CO2 by thermogravimetry under various CO2 partial pressures—Clarification of CO2 partial pressure and temperature region of CO2 absorption or desorption
AU - Kaniwa, Shingo
AU - Yoshino, Masatoshi
AU - Niwa, Eiki
AU - Yashima, Masatomo
AU - Hashimoto, Takuya
N1 - Funding Information:
The authors acknowledge Prof. K. Oh-ishi (Chuo University) and Prof. K. Sasaki (Hirosaki University) for advices to prepare single phase Li4SiO4. This work was partly supported by JSPS KAKENHI Grant Number JP16K05886.
Publisher Copyright:
© 2017 Elsevier Ltd
PY - 2017/10
Y1 - 2017/10
N2 - Chemical reaction between CO2 and Li4SiO4 was investigated using thermogravimetry under various P(CO2). Under P(CO2) of 1.0 bar, weight increase originating from CO2 absorption reaction was observed from ∼500 °C and abrupt weight reduction due to CO2 desorption was detected at ∼700 °C. With decreasing P(CO2), the latter temperature decreased. Since fair agreement was observed between the latter temperatures and thermodynamically calculated equilibrium temperatures of Li4SiO4 + CO2 ↔ Li2CO3 + Li2SiO3, the latter temperatures could be regarded as approximate equilibrium. Dependence of the calculated equilibrium temperatures and approximate equilibrium temperatures on P(CO2) was represented with Ellingham diagram, showing P(CO2) and temperature region of CO2 absorption or desorption. Approximate equilibrium temperature under P(CO2) of 1.0 bar agreed with the calculation, whereas deviation was observed under low P(CO2), resulted in larger apparent ΔS° and ΔH° than the calculated ones. Using specimen with smaller particle size, the deviation reduced due to enhancement of CO2 desorption kinetics.
AB - Chemical reaction between CO2 and Li4SiO4 was investigated using thermogravimetry under various P(CO2). Under P(CO2) of 1.0 bar, weight increase originating from CO2 absorption reaction was observed from ∼500 °C and abrupt weight reduction due to CO2 desorption was detected at ∼700 °C. With decreasing P(CO2), the latter temperature decreased. Since fair agreement was observed between the latter temperatures and thermodynamically calculated equilibrium temperatures of Li4SiO4 + CO2 ↔ Li2CO3 + Li2SiO3, the latter temperatures could be regarded as approximate equilibrium. Dependence of the calculated equilibrium temperatures and approximate equilibrium temperatures on P(CO2) was represented with Ellingham diagram, showing P(CO2) and temperature region of CO2 absorption or desorption. Approximate equilibrium temperature under P(CO2) of 1.0 bar agreed with the calculation, whereas deviation was observed under low P(CO2), resulted in larger apparent ΔS° and ΔH° than the calculated ones. Using specimen with smaller particle size, the deviation reduced due to enhancement of CO2 desorption kinetics.
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U2 - 10.1016/j.materresbull.2017.05.054
DO - 10.1016/j.materresbull.2017.05.054
M3 - Article
AN - SCOPUS:85020275207
SN - 0025-5408
VL - 94
SP - 134
EP - 139
JO - Materials Research Bulletin
JF - Materials Research Bulletin
ER -