2007
DOI: 10.1016/j.mineng.2007.03.017
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Fundamental studies of Rhodococcus opacus as a biocollector of calcite and magnesite

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Cited by 78 publications
(46 citation statements)
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“…The findings of FTIR spectra of corundum are in agreement with [16] and the results obtained by [15] for interaction of hematite before and after with R. erythropolis have shown that after interaction, new surface species were found and it also proved that adsorption occurs mainly chemical adsorption which makes hematite surface hydrophobic and enhance the floatability. Similar functional groups in quartz have been observed by [17] wherein they have shown that in presence of R. opacus calcite showed the characteristic bands of carbonates. The FTIR spectra of cell free extract interacted with minerals were observed by [16] and the shift in peaks was observed due to the presence of polysaccharides on hematite and corundum.…”
Section: Discussionsupporting
confidence: 81%
“…The findings of FTIR spectra of corundum are in agreement with [16] and the results obtained by [15] for interaction of hematite before and after with R. erythropolis have shown that after interaction, new surface species were found and it also proved that adsorption occurs mainly chemical adsorption which makes hematite surface hydrophobic and enhance the floatability. Similar functional groups in quartz have been observed by [17] wherein they have shown that in presence of R. opacus calcite showed the characteristic bands of carbonates. The FTIR spectra of cell free extract interacted with minerals were observed by [16] and the shift in peaks was observed due to the presence of polysaccharides on hematite and corundum.…”
Section: Discussionsupporting
confidence: 81%
“…1(a) shows the zeta potential of the microorganism at different pH values. Initially, we observed an isoelectric point (IEP) of approximately 2.8, as found in previous works (Botero et al, 2007(Botero et al, , 2008Mesquita et al, 2003;Merma et al, 2013). According to several authors (Rao and Subramanian, 2007;Natarajan, 2006;Vilinska and Rao., 2008;Faharat et al, 2008;Van Der Wal et al, 1997), this acidic value is related to the higher presence of anionic functional groups compared with cationic groups.…”
Section: Zeta Potential Studiessupporting
confidence: 82%
“…Thus, considering that phosphate ores are associated with several gangue minerals, especially quartz, carbonates and silicates, then a detailed bioflotation study of each component is necessary to establish the bioflotation of phosphate ores. One bacteria, quite recently used in mineral bioflotation, is Rhodococcus opacus (Botero et al, 2007;Mesquita et al, 2003;Botero et al, 2008;Merma et al, 2013). It is a Gram positive bacterium with different types of components on their cell-wall, which are primarily polysaccharides, carboxylic acids, lipid groups and mycolic acids, that result in amphoteric behavior (hydrophobic and/or hydrophilic properties) of the bacteria (Mesquita et al, 2003;Natarajan, 2006;Vilinska and Rao., 2008).…”
Section: Introductionmentioning
confidence: 99%
“…Especially, flotation is one of the most effective methods to increase the recovery of fine-grained and low-grade magnesite. In recent years, mineral processors dealing with magnesite have faced a difficult problem in that the flotation results of magnesite are not ideal in the presence of carbonate minerals, such as calcite and dolomite [3,4]. Dolomite (CaMg(CO 3 ) 2 ) which is one of the most common and typical carbonate gangues, often coexists with rhodochrosite, smithsonite, magnesite, and pyrite [5][6][7][8][9][10].…”
Section: Introductionmentioning
confidence: 99%