Publicación Artículo científico (article).

Quantitative mineralogical comparison between HPGR and ball mill products of a Sn-Ta ore

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  • Hamid, Sarbast
  • Alfonso Abella, María Pura|||0000-0002-1515-4999
  • Anticoi Sudzuki, Hernán Francisco|||0000-0003-4316-5203
  • Guasch Cascallo, Eduard|||0000-0001-6929-8843
  • Oliva Moncunill, Josep|||0000-0001-6214-5713
  • Dosbaba, Marek
  • García-Vallès, Maite
  • Chugunova, Marina
The mineralogy and liberation characteristics of the comminuted Penouta leucogranite host of the Sn-Ta ore were determined. Grinding developed by a combination of high-pressure grinding rolls (HPGR) followed by a ball mill (BM) was compared with a single ball mill process. The mineral characteristics of the grinding products were analyzed using a Tescan Integrated Mineralogical Analyzer (TIMA-X) and X-ray powder diffraction (XRD). The ore contains 103 ppm of Ta and is mainly composed of quartz, albite, microcline, muscovite, and kaolinite. Nb, Ta-rich minerals are columbite-(Mn) and tantalite-(Mn), as well as minor microlite and wodginite. The liberation in the product is high in the size fraction of less than 250 m (51–52 wt % for columbite-group minerals (CGM) and 74–80 wt % for cassiterite) and reduced in larger particles (8.8–17 wt % for CGM and 28–37 wt % for cassiterite). The recovery in the ¿250 m fraction was high, while in the larger fraction it is limited, remaining up to 80 ppm in some tailings. The combined use of HPGR and a BM reduces the particle size distribution of the product and, thus, increases the liberation of the ores. Smaller fractions can be treated directly using gravity methods; however, particles of a size greater than +250 m should be ground more., Peer Reviewed
 

DOI: http://hdl.handle.net/2117/117853, https://dx.doi.org/10.3390/min8040151
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HANDLE: http://hdl.handle.net/2117/117853, https://dx.doi.org/10.3390/min8040151
UPCommons. Portal del coneixement obert de la UPC
oai:upcommons.upc.edu:2117/117853
 
Ver en: http://hdl.handle.net/2117/117853, https://dx.doi.org/10.3390/min8040151
UPCommons. Portal del coneixement obert de la UPC
oai:upcommons.upc.edu:2117/117853

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