Bulk and Surface Characterization of Distinct Hematite Morphology: Implications for Wettability and Flotation Response

Author:

Faustino Lívia12,McFadzean Belinda3,Gouvêa Junior José2ORCID,Leal Filho Laurindo2ORCID

Affiliation:

1. Clariant Mining Solutions, 4132 Muttenz, Switzerland

2. Department of Mining and Petroleum Engineering, University of São Paulo, São Paulo 05508-220, Brazil

3. Center for Minerals Research, University of Cape Town, Cape Town 7700, South Africa

Abstract

To understand why hematite of different genesis behave diversely in flotation systems, this study assesses the flotation response at pH 5 of bulk (morphology, texture, Crystal Preferential Orientation (CPO)) plus interfacial (surface area, zeta potential, immersion enthalpy, contact angle, induction time) characteristics of species formed under distinct metamorphic conditions: low-strain deformation (Hematite-1) versus high-strain deformation (Hematite-2). Hematite-2 (predominantly composed of specular and lamellar morphologies) shows (001) CPO and exhibits fewer Fe sites on its surface that undergo doubly coordinated Fe-OH when exposed to moisture. This results in a less reactive surface associated with a less ordered adsorbed water layer than Hematite-1, which is predominantly composed of granular and sinuous hematite. Those characteristics lead to a naturally hydrophobic behavior characterized by the exothermic energy below the Critical Immersion Enthalpy (−∆Himm < 200 mJ/m2), lower values of zeta potential due to attenuated dissociation of Fe-OH(surf), lower induction time (47 ms vs. 128 ms), higher contact angle (39° vs. 13°), and higher flotation recovery (21% vs. 12%) than Hematite-1.

Funder

the Vale Institute of Technology and National Council for Scientific and Technological Development

the Brazilian Nanotechnology National Laboratory (LNNano) of the Brazilian Center for Research in Energy and Materials

Publisher

MDPI AG

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3. Halder, S. (2017). Genesis of BIF-Hosted Iron Ore Deposits in the Carajás Mineral Province, Brazil: Constraints from In-Situ Fe Isotope Analysis and Whole-Rock Geochemistry. [Ph.D. Thesis, Faculty of Energy and Management Science, Clausthal University of Technology].

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5. Textural and mineralogical variations during metamorphism of the Proterozoic Itabira Iron Formation in the Quadrilátero Ferrífero, Minas Gerais, Brazil;Pires;An. Da Acad. Bras. De Ciências,1995

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