2008
DOI: 10.1007/s10973-007-8853-6
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Characterization of FDR fly ash and brick/lime mixtures

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Cited by 8 publications
(8 citation statements)
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“…Finally, in the last zone, at temperature higher than 900°C a lower than 1100°C, the CA formation occurs according to DTA. The formation of the different aluminate phases agrees to the XRD results and the bibliographic data [13,14].…”
Section: Precursor Characterizationsupporting
confidence: 85%
See 1 more Smart Citation
“…Finally, in the last zone, at temperature higher than 900°C a lower than 1100°C, the CA formation occurs according to DTA. The formation of the different aluminate phases agrees to the XRD results and the bibliographic data [13,14].…”
Section: Precursor Characterizationsupporting
confidence: 85%
“…The pattern of precursor obtained at pH 7 can be assigned to 3CaOÁAl 2 O 3 ÁCaCl 2 Á 10H 2 O (JCPDS 35-0105) which is a hydrated calcium aluminate with partial substitution of oxygen by chloride. The presence of this phase reveals the formation of reactive aluminate phases in the early stage of precursor formation, when CaO is added to the oxy-hydroxide aluminium gel [13]. The same phase is observed as the unique crystalline phase for precursor at pH 10.…”
Section: Precursor Characterizationmentioning
confidence: 77%
“…To further study the variation of the internal composition of the specimens with the degree of hydration, the variation law of chemically bound water and Ca(OH) 2 in the specimens at different ages was analyzed by TG. As can be seen from Figures 9 and 10 the weight loss of the specimen can be divided into four stages: −30-105 • C, 105-400 • C, 400-500 • C, and 500-800 • C. Where the weight loss below 105 • C is the evaporation of free water, 105-400 • C can be identified as C-(A)-S-H gel to remove chemically bound water, 400-500 • C is the dehydration of Ca(OH) 2 , and 500-800 • C is the decomposition of CaCO 3 [52,53].…”
Section: Tg Analysismentioning
confidence: 99%
“…Η κορυφή στα ~465 cm -1 σχετίζεται με την ύπαρξη δεσμών Si-O και / ή Al-O σε αργιλοπυριτικά υλικά ( [Yu et al, 1999], [Ζαχαράκη, 2009]), και βρίσκεται τόσο στο φάσμα της ποζολάνης όσο και στα φάσματα της σύνθεσης (με αμετάβλητη την ένταση με την αύξηση του χρόνου ενυδάτωσης. Ubbriaco et al, 2008], [Giergiczny, 2006], [Moropoulou et al, 2004a], [Bakolas et al, 2008], [Bruno et al, 2004], [Silva et al, 2005], [Frias and Cabrera, 2001], [Ubbriaco and Tasselli, 1998] Ubbriaco and Tasselli, 1998], [Frias and Cabrera, 2001], [Moropoulou et al, 2004a], [Bakolas et al, 2008], [Miller et al, 2010] ).…”
Section:  σύνθεση Cahg3unclassified
“…Μελέτη του μηχανισμού πήξης κονιαμάτων τύπου ασβέστη -φυσικής ποζολάνης Μαρία Τζιότζιου 130 [Ubbriaco and Tasselli, 1998], [Ubbriaco et al, 2008] ΙΙΙ.44 α, β, γ, δ, ε, ζ, η, θ, ι).…”
unclassified