dc.contributor.author |
Perraki, Th |
en |
dc.contributor.author |
Kakali, G |
en |
dc.contributor.author |
Kontori, E |
en |
dc.date.accessioned |
2014-03-01T02:43:10Z |
|
dc.date.available |
2014-03-01T02:43:10Z |
|
dc.date.issued |
2005 |
en |
dc.identifier.issn |
1388-6150 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/31266 |
|
dc.subject |
Calcination |
en |
dc.subject |
Pozzolanic activity |
en |
dc.subject |
Zeolite |
en |
dc.subject.classification |
Chemistry, Analytical |
en |
dc.subject.classification |
Chemistry, Physical |
en |
dc.subject.other |
Calcination |
en |
dc.subject.other |
Characterization |
en |
dc.subject.other |
Crystal lattices |
en |
dc.subject.other |
Differential thermal analysis |
en |
dc.subject.other |
Fourier transform infrared spectroscopy |
en |
dc.subject.other |
Heat treatment |
en |
dc.subject.other |
Pozzolan |
en |
dc.subject.other |
Thermogravimetric analysis |
en |
dc.subject.other |
X ray diffraction analysis |
en |
dc.subject.other |
Chapelle test |
en |
dc.subject.other |
Heulandite |
en |
dc.subject.other |
Pozzolanic activity |
en |
dc.subject.other |
Zeolites |
en |
dc.title |
Characterization and pozzolanic activity of thermally treated zeolite |
en |
heal.type |
conferenceItem |
en |
heal.identifier.primary |
10.1007/s10973-005-0849-5 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1007/s10973-005-0849-5 |
en |
heal.language |
English |
en |
heal.publicationDate |
2005 |
en |
heal.abstract |
The pozzolanic reactivity of thermally treated zeolites was studied on the basis of the Chapelle test combined with X-ray diffraction (XRD) and Fourier Transform (FTIR) spectroscopy, as well as thermogravimetric analysis (TG/DTG) and differential thermal analysis (DTA). The raw zeolite samples are from the Pentalofos area, Thrace, NE Greece. Their main mineral constituent is 'heulandite type-II', an intermediate type of the heulandite-clinoptilolite isomorphous series. Calcination of the samples was carried out up to 400, 500, 600, 700 and 1000°C for 15 h. The changes were recorded using the above methods. The deformation of the zeolite crystal lattice starts at about 400°C and proceeds as the temperature of thermal treatment rises. The thermal treatment of zeolite at 400°C improves its pozzolanic reactivity and accelerates the reaction with Ca(OH)2. © 2005 Akadémiai Kiadó, Budapest. |
en |
heal.publisher |
SPRINGER |
en |
heal.journalName |
Journal of Thermal Analysis and Calorimetry |
en |
dc.identifier.doi |
10.1007/s10973-005-0849-5 |
en |
dc.identifier.isi |
ISI:000233245600016 |
en |
dc.identifier.volume |
82 |
en |
dc.identifier.issue |
1 |
en |
dc.identifier.spage |
109 |
en |
dc.identifier.epage |
113 |
en |