2010
DOI: 10.2298/hemind100322014i
|View full text |Cite
|
Sign up to set email alerts
|

Thermal treatment of kaolin clay to obtain metakaolin

Abstract: The metakaolin was produced by thermal treatment (calcination) of the starting high-quality kaolin clay from Serbia. The optimal calcination parameters, for which nearly complete dehydroxylation of the material was achieved, are: temperature 650°C and heating time of 90 min. The conversion of the kaolinite to metakaolin was confirmed by XRD and IR analyses of the starting and thermally treated kaolin samples. The pozzolanic activity was determined by Chapelle test. The obtained value 0.65 g Ca(OH)2/g of metaka… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

10
54
0
6

Year Published

2017
2017
2023
2023

Publication Types

Select...
7
3

Relationship

0
10

Authors

Journals

citations
Cited by 213 publications
(88 citation statements)
references
References 10 publications
10
54
0
6
Order By: Relevance
“…This study has looked into the use of metakaolin, a product of the calcination of kaolin clay as a partial replacement of cement in concrete. Metakaolin is produced from heat treating (calcination) of Kaolin clay, one of the most abundant soil minerals formed from the chemical weathering of rocks (feldspar rocks) in hot moist climate [1]. Metakaolin is a highly reactive alumino silicate pozzolan that is rich in Silica and Alumina.…”
Section: Introductionmentioning
confidence: 99%
“…This study has looked into the use of metakaolin, a product of the calcination of kaolin clay as a partial replacement of cement in concrete. Metakaolin is produced from heat treating (calcination) of Kaolin clay, one of the most abundant soil minerals formed from the chemical weathering of rocks (feldspar rocks) in hot moist climate [1]. Metakaolin is a highly reactive alumino silicate pozzolan that is rich in Silica and Alumina.…”
Section: Introductionmentioning
confidence: 99%
“…In contrast, the samples produced at lower temperatures are much less stable and lose up to 45% of their original mass. Here, the weight losses can be separated in three (although strongly overlapping) steps between 25 and 100 °C, 110 and ≈450 °C, and finally ≈450 to 900 °C [42]. The first loss can be assigned to the desorption of water adsorbed in the pores of the hybrid clay materials.…”
Section: Resultsmentioning
confidence: 99%
“…The mullite phase was not found in M1 and in M2's raw material; the mullite contribution was minor. After thermally treating kaolin at 873-973 K, the characteristic peaks for kaolinite (2h 12.41°, 20.21°and 25.49°) should disappear, while peaks assigned to quartz (2h 21.22°and 27.45°) should remain unchanged [22]. The occurrence of a kaolinite (Al 2 Si 2-O 5 (OH) 4 ) phase, which indicates the incomplete transformation of kaolinite into metakaolinite, was noted for M2.…”
Section: Geopolymer Characterisation Methodsmentioning
confidence: 97%