Surface Spectroscopy of Pyrite Obtained during Grinding and Its Magnetisation

被引:7
作者
Reyes, Martin [1 ]
Herrera, Guadalupe [1 ]
Escudero, Ramiro [2 ]
Patino, Francisco [3 ]
Reyes, Ivan A. [4 ]
Flores, Mizraim [5 ]
Palacios, Elia G. [6 ]
Juarez, Julio [1 ]
Barrientos, Francisco [1 ]
机构
[1] Univ Autonoma Estado Hidalgo, Area Academ Ciencias La Tierra & Mat, Mineral De La Reforma 42186, Mexico
[2] Univ Michoacana, Inst Invest Metalurg, Morelia 58030, Michoacan, Mexico
[3] Univ Politecn Metropolitana Hidalgo, Ingn Energia, Tolcayuca 43860, Mexico
[4] Univ Autonoma San Luis Potosi, Inst Metalurgia, San Luis Potosi 78210, San Luis Potosi, Mexico
[5] Univ Tecnol Tulancingo, Area Electromecan Ind, Tulancingo 43642, Mexico
[6] Inst Politecn Nacl, Escuela Super Ingn Quim & Industrias Extract, Ciudad De Mexico 07738, Mexico
关键词
infrared; pyrite; magnetite; grinding; goethite; siderite; CARBONATE IONS; OXIDATION; IRON; FLOTATION; MEDIA; CHALCOPYRITE; ADSORPTION; JAROSITE; FES2;
D O I
10.3390/min12111444
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
During grinding with forged steel media, sulphides such as pyrite undergo surface changes due to the occurrence of oxidation-reduction reactions, which affect its depression during the concentration process. For this reason, in this work, the surface modification of pyrite during grinding was studied; FTIR, ICP-OES, XRD and SEM-EDS were used for the materials' characterisation. It was found that the pyrite obtained during grinding showed magnetic susceptibility due to the absorption and superficial formation of magnetite Fe3O4, Fe-O bonds identified by FTIR at 598 cm(-1), and of other species, such as oxy-hydroxy-sulphates at 696 cm(-1) and goethite alpha-FeOOH at 875 cm(-1). This caused the reversal of the zeta potential magnitude (zeta) from positive to negative at pH 8.3 and 30 min of grinding. The zeta of the pyrite throughout the studied pH ranges was, overall, positive, i.e., +5 mV. However, at pH 10.5 and 15 min of grinding, the zeta turned negative. This was associated with the formation of Fe-CO3 (-2) bonds in the siderite, which were identified with the absorption bands corresponding to 756, 1448 and 1493 cm(-1).
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页数:19
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