TY - JOUR
T1 - Production of alinite-chlormayenite clinker and its hydration behavior with increasing gypsum content
AU - Simoni, Marco
AU - Baral, Aniruddha
AU - Ren, Zhili
AU - Duvallet, Tristana Y.
AU - Jewell, Robert B.
AU - Rößler, Christiane
AU - Hanein, Theodore
N1 - Publisher Copyright:
© 2024 The Authors
PY - 2025/3
Y1 - 2025/3
N2 - An alternative low-energy alinite-chlormayenite clinker was produced and its hydration with different gypsum content was studied. The clinker was produced at 1225 °C using reagent-grade materials in an electric kiln with alinite, larnite, and chlormayenite content of 48, 24, and 16 wt%, respectively. The hydration kinetics of the clinker with different gypsum additions (0,10, 20, and 40 wt%) did not have a distinct induction period, and the hydration was faster than Portland cement. Alinite was in general more reactive than chlormayenite. In the presence of a limited amount of gypsum (10 and 20 wt%), alinite consumed gypsum to form ettringite within the first hour of hydration, and both alinite and chlormayenite formed Friedel's salt after gypsum was exhausted. Sufficient gypsum availability (40 wt%) slowed down the dissolution of alinite and chlormayenite for the first hour of hydration but enabled both chlormayenite and alinite to form ettringite.
AB - An alternative low-energy alinite-chlormayenite clinker was produced and its hydration with different gypsum content was studied. The clinker was produced at 1225 °C using reagent-grade materials in an electric kiln with alinite, larnite, and chlormayenite content of 48, 24, and 16 wt%, respectively. The hydration kinetics of the clinker with different gypsum additions (0,10, 20, and 40 wt%) did not have a distinct induction period, and the hydration was faster than Portland cement. Alinite was in general more reactive than chlormayenite. In the presence of a limited amount of gypsum (10 and 20 wt%), alinite consumed gypsum to form ettringite within the first hour of hydration, and both alinite and chlormayenite formed Friedel's salt after gypsum was exhausted. Sufficient gypsum availability (40 wt%) slowed down the dissolution of alinite and chlormayenite for the first hour of hydration but enabled both chlormayenite and alinite to form ettringite.
KW - Alinite
KW - Chlorine
KW - Chlormayenite
KW - Ettringite
KW - Friedel's salt
KW - Gypsum
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U2 - 10.1016/j.cemconres.2024.107774
DO - 10.1016/j.cemconres.2024.107774
M3 - Article
AN - SCOPUS:85211463126
SN - 0008-8846
VL - 189
JO - Cement and Concrete Research
JF - Cement and Concrete Research
M1 - 107774
ER -