scholarly journals Reclaim of Synthetic Rutile Fines Produced In Ilmenite Beneficiation Process by Agglomeration

2022 ◽  
Vol 9 (1) ◽  
pp. 1057-1061
Author(s):  
◽  
G. Lijith ◽  
I. K. Shaju ◽  
P. K. Manikuttan ◽  
◽  
...  
Keyword(s):  
1949 ◽  
Vol 2 (4) ◽  
pp. 166-167
Author(s):  
W. F. Eppler
Keyword(s):  

1949 ◽  
Vol 2 (2) ◽  
pp. 35-44
Author(s):  
W. F. Eppler
Keyword(s):  

Crystals ◽  
2021 ◽  
Vol 11 (8) ◽  
pp. 888
Author(s):  
Helin Fan ◽  
Ruixiang Wang ◽  
Zhifeng Xu ◽  
Huamei Duan ◽  
Dengfu Chen

Synthetic rutile was prepared from titanium slag melt with low energy consumption and a small amount of additive (B2O3) in our previous work. The modification mechanism of titanium slag was not clear enough. The migration and enrichment behaviors of Ca and Mg elements during cooling and crystallization of boron-bearing titanium slag melt were characterized by XRF, FESEM, EMPA, and XPS. Results show that when additive (B2O3) is added, Ti elements are migrated and enriched in the area to generate rutile, while Ca, Mg, and B elements are migrated and enriched in another area to generate borate. With the additive (B2O3) amount increased, Ca and Mg element migration is complete and more thorough. Additive (B2O3) promotes rutile formation and inhibits the formation of anosovite during cooling and crystallization of titanium slag melt. With the additive (B2O3) amount increasing from 0% to 6%, the proportion of Ti3+ in the modified titanium slag reduces from 9.15% to 0%, and the proportion of Ti4+ increases from 90.85% to 100% under the same cooling and crystallization condition. The result will lay the foundation for the efficient preparation of synthetic rutile by adding B2O3 to the titanium slag melt.


1948 ◽  
Vol 16 (12) ◽  
pp. 1166-1166 ◽  
Author(s):  
S. Zerfoss ◽  
R. G. Stokes ◽  
C. H. Moore

2011 ◽  
Vol 100 (3-4) ◽  
pp. 166-171 ◽  
Author(s):  
Andrew Adipuri ◽  
Yan Li ◽  
Guangqing Zhang ◽  
Oleg Ostrovski
Keyword(s):  

2013 ◽  
Vol 52 (13) ◽  
pp. 4924-4931 ◽  
Author(s):  
L. Zhang ◽  
J. H. Zhang ◽  
W. Zhang ◽  
G. Q. Li

2005 ◽  
Vol 69 (3) ◽  
pp. 345-358 ◽  
Author(s):  
G. D. Bromiley ◽  
N. Hilairet

AbstractThe solubility and incorporation mechanisms of H and various trivalent and divalent cations in synthetic rutile have been investigated. Experiments performed using different bulk Fe2O3contents demonstrate that Fe3+substitutes onto the main Ti site, charge-balanced by oxygen vacancies. Under more reducing conditions in Fe-poor systems, the concentration of Ti interstitials in rutile is increased, resulting in a decrease in H solubility. Variation in the solubility of different oxides in rutile as a function of ionic radius implies substitution onto the main Ti site, probably charge-balanced by oxygen vacancies. To a lesser degree, substitution of trivalent and divalent cations is locally charge-balanced by H incorporation. Variation in OH-stretching frequencies in infrared spectra as a function of composition implies that octahedral defects and structurally-incorporated H are coupled. However, in all samples, some of the H is also decoupled from substitutional impurities, as is evident from an OH-absorption band at 3279 cm–1. This band corresponds to the main OH band seen in spectra of many natural rutiles, implying that in most rutiles, H defects are decoupled from substitutional defects.


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