Extraction of rhenium from calcines of the oxidation roasting of low-grade molybdenite concentrate in a rotating tubular furnace

2007 ◽  
Vol 48 (2) ◽  
pp. 107-109 ◽  
Author(s):  
F. Sh. Balgaeva ◽  
A. S. Medvedev
2019 ◽  
Vol 1 (4) ◽  
Author(s):  
Ping Wang ◽  
Yajing Pan ◽  
Xiao Sun ◽  
Yongqiang Zhang

1996 ◽  
Vol 41 (2-3) ◽  
pp. 201-209 ◽  
Author(s):  
J.M. Juneja ◽  
Sohan Singh ◽  
D.K. Bose

1988 ◽  
Vol 1 (4) ◽  
pp. 337-342 ◽  
Author(s):  
S. Singh ◽  
M.K. Chetty ◽  
J.M. Juneja ◽  
J.C. Sehra ◽  
C.K. Gupta

2009 ◽  
Vol 50 (11) ◽  
pp. 2669-2674 ◽  
Author(s):  
Byung-Su Kim ◽  
Hoo-In Lee ◽  
Young-Yoon Choi ◽  
Sangbae Kim

2007 ◽  
Vol 86 (1-2) ◽  
pp. 56-62 ◽  
Author(s):  
Manoj Kumar ◽  
T.R. Mankhand ◽  
D.S.R. Murthy ◽  
R. Mukhopadhyay ◽  
P.M. Prasad

Rare Metals ◽  
2015 ◽  
Vol 34 (3) ◽  
pp. 207-214 ◽  
Author(s):  
Juan Yu ◽  
Hong-Ying Yang ◽  
Lin-Lin Tong ◽  
Jun Zhu

Author(s):  
Thomas R. McKee ◽  
Peter R. Buseck

Sediments commonly contain organic material which appears as refractory carbonaceous material in metamorphosed sedimentary rocks. Grew and others have shown that relative carbon content, crystallite size, X-ray crystallinity and development of well-ordered graphite crystal structure of the carbonaceous material increases with increasing metamorphic grade. The graphitization process is irreversible and appears to be continous from the amorphous to the completely graphitized stage. The most dramatic chemical and crystallographic changes take place within the chlorite metamorphic zone.The detailed X-ray investigation of crystallite size and crystalline ordering is complex and can best be investigated by other means such as high resolution transmission electron microscopy (HRTEM). The natural graphitization series is similar to that for heat-treated commercial carbon blacks, which have been successfully studied by HRTEM (Ban and others).


Author(s):  
V.K. Berry

There are two strains of bacteria viz. Thiobacillus thiooxidansand Thiobacillus ferrooxidanswidely mentioned to play an important role in the leaching process of low-grade ores. Another strain used in this study is a thermophile and is designated Caldariella .These microorganisms are acidophilic chemosynthetic aerobic autotrophs and are capable of oxidizing many metal sulfides and elemental sulfur to sulfates and Fe2+ to Fe3+. The necessity of physical contact or attachment by bacteria to mineral surfaces during oxidation reaction has not been fairly established so far. Temple and Koehler reported that during oxidation of marcasite T. thiooxidanswere found concentrated on mineral surface. Schaeffer, et al. demonstrated that physical contact or attachment is essential for oxidation of sulfur.


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