[article]
Titre : |
Gravity separation of coarse particles using the Reflux Classifier |
Type de document : |
texte imprimé |
Auteurs : |
K. P. Galvin, Auteur ; A.M. Callen, Auteur ; S. Spear, Auteur |
Année de publication : |
2011 |
Article en page(s) : |
pp. 339–349 |
Note générale : |
Génie Minier |
Langues : |
Anglais (eng) |
Mots-clés : |
Coal preparation Gravity concentration Separation Fluidization Particle Sedimentation Inclined sedimentation Elutriation Oxide ores Diamonds |
Résumé : |
A comprehensive study examining the potential of the Reflux Classifier to be applied to the beneficiation of coarser coal up to 8 mm in size was undertaken. It was demonstrated that efficient combustible recovery and control of the separation density to target low ash products could be achieved. The major finding from the study was the critical importance of providing sufficient fluidization water, though beyond the critical level the process was largely insensitive to the fluidization rate. It was concluded the required fluidization velocity is nominally 10 m/h per mm of top-size, hence for a nominal 4 mm top size the required velocity is 40 m/h. In an extended campaign the control of the process was investigated by varying the set point density from high to low levels and then returning the process to the original settings, and demonstrating a return to the original separation. Further analysis was conducted to determine the partition curves and the shift in the separation density with particle size. The variation in the D50 with particle size approaches a level that is independent of the particle size. Previous data ( [Galvin et al., 2002] and [Galvin et al., 2004]) covering particles up to 2 mm in size are consistent with the results from this study, involving feeds with top sizes of 4 mm and 8 mm. Beyond a particle size of 2 mm the Ep is typically less than 0.05 and approaches about 0.03 as the particle size increases to 8 mm. |
DEWEY : |
622 |
ISSN : |
0892-6875 |
En ligne : |
http://www.sciencedirect.com/science/article/pii/S0892687509002398 |
in Minerals engineering > Vol. 23 N° 4 (Mars 2010) . - pp. 339–349
[article] Gravity separation of coarse particles using the Reflux Classifier [texte imprimé] / K. P. Galvin, Auteur ; A.M. Callen, Auteur ; S. Spear, Auteur . - 2011 . - pp. 339–349. Génie Minier Langues : Anglais ( eng) in Minerals engineering > Vol. 23 N° 4 (Mars 2010) . - pp. 339–349
Mots-clés : |
Coal preparation Gravity concentration Separation Fluidization Particle Sedimentation Inclined sedimentation Elutriation Oxide ores Diamonds |
Résumé : |
A comprehensive study examining the potential of the Reflux Classifier to be applied to the beneficiation of coarser coal up to 8 mm in size was undertaken. It was demonstrated that efficient combustible recovery and control of the separation density to target low ash products could be achieved. The major finding from the study was the critical importance of providing sufficient fluidization water, though beyond the critical level the process was largely insensitive to the fluidization rate. It was concluded the required fluidization velocity is nominally 10 m/h per mm of top-size, hence for a nominal 4 mm top size the required velocity is 40 m/h. In an extended campaign the control of the process was investigated by varying the set point density from high to low levels and then returning the process to the original settings, and demonstrating a return to the original separation. Further analysis was conducted to determine the partition curves and the shift in the separation density with particle size. The variation in the D50 with particle size approaches a level that is independent of the particle size. Previous data ( [Galvin et al., 2002] and [Galvin et al., 2004]) covering particles up to 2 mm in size are consistent with the results from this study, involving feeds with top sizes of 4 mm and 8 mm. Beyond a particle size of 2 mm the Ep is typically less than 0.05 and approaches about 0.03 as the particle size increases to 8 mm. |
DEWEY : |
622 |
ISSN : |
0892-6875 |
En ligne : |
http://www.sciencedirect.com/science/article/pii/S0892687509002398 |
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