2023
DOI: 10.1016/j.ceramint.2023.02.066
|View full text |Cite
|
Sign up to set email alerts
|

Characterization and thermal behavior of granite waste during heating

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
5
0

Year Published

2024
2024
2024
2024

Publication Types

Select...
3

Relationship

0
3

Authors

Journals

citations
Cited by 3 publications
(5 citation statements)
references
References 27 publications
0
5
0
Order By: Relevance
“…20 The quartz, kaolinite, and illite minerals are responsible for the red firing behavior as they promote vitrification and hematite crystallization at elevated temperatures around 950°C. 21 The SEM micrographs revealing particle morphology of the studied clay are shown in Figure 2. The images indicate loosely held plate-like pseudohexagonal particles characteristic of kaolinite.…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…20 The quartz, kaolinite, and illite minerals are responsible for the red firing behavior as they promote vitrification and hematite crystallization at elevated temperatures around 950°C. 21 The SEM micrographs revealing particle morphology of the studied clay are shown in Figure 2. The images indicate loosely held plate-like pseudohexagonal particles characteristic of kaolinite.…”
Section: Resultsmentioning
confidence: 99%
“…20 The quartz, kaolinite, and illite minerals are responsible for the red firing behavior as they promote vitrification and hematite crystallization at elevated temperatures around 950°C. 21…”
Section: Resultsmentioning
confidence: 99%
“…The main components include SiO 2 , Al 2 O 3 , CaO, Na 2 O, and K 2 O, which are closely related to feldspar minerals. Owing to the high Fe 2 O 3 content in the granite powder, the disproportionation reaction of Fe 2 O 3 occurs spontaneously at elevated temperatures, causing the self‐foaming of sintered glass‐ceramics 20 . Besides, the colored minerals containing iron and titanium render the black‐colored appearance of sintered glass‐ceramics, which destroys its decorativeness.…”
Section: Resultsmentioning
confidence: 99%
“…Owing to the high Fe 2 O 3 content in the granite powder, the disproportionation reaction of Fe 2 O 3 occurs spontaneously at elevated temperatures, causing the selffoaming of sintered glass-ceramics. 20 Besides, the colored minerals containing iron and titanium render the blackcolored appearance of sintered glass-ceramics, which destroys its decorativeness. Thus, they should be removed from the granite powder for practical utilizations.…”
Section: Characterization Of the Granite Powdermentioning
confidence: 99%
“…The crystals obtained at 1120℃ are densely distributed, and the crystal forms are relatively complete but very small. This is because at 1120℃, the nucleation rate of crystals is greater than the crystal growth rate [8], and crystal growth is slow due to low temperature and large viscosity of glaze melt. With the increase of the holding temperature, the individual crystals gradually become larger and grow in clusters, and there is no obvious vitreous body on the enamel surface, but when the temperature reaches 1180℃, the individual crystals are larger and intact, but the entire glaze layer crystals become dispersed and sparse.…”
Section: Effect Of Crystallization Temperature On Quality and Crystal...mentioning
confidence: 99%