scholarly journals Magnetic separation and evaluation of magnetization of Brazilian soils from different parent materials

Geoderma ◽  
2000 ◽  
Vol 96 (1-2) ◽  
pp. 81-99 ◽  
Author(s):  
M.P.F. Fontes ◽  
T.S. de Oliveira ◽  
L.M. da Costa ◽  
A.A.G. Campos
Soil Science ◽  
2000 ◽  
Vol 165 (10) ◽  
pp. 825-834 ◽  
Author(s):  
Teogenes S. de Oliveira ◽  
Mauricio P. F. Fontes ◽  
Liovando M. da Costa ◽  
Adolf Heinrich Horn

2018 ◽  
Vol 161 ◽  
pp. 385-394 ◽  
Author(s):  
Giovana Clarice Poggere ◽  
Alberto Vasconcellos Inda ◽  
Vidal Barrón ◽  
Nestor Kämpf ◽  
Angela Dayana Barrera de Brito ◽  
...  

1989 ◽  
Vol 29 (3) ◽  
pp. 150-155
Author(s):  
Takeshi OHARA
Keyword(s):  

Author(s):  
Meina FANG ◽  
Takaya TERADA ◽  
Fumihito MISHIMA ◽  
Yoko AKIYAMA ◽  
Yoshinobu IZUMI ◽  
...  

2017 ◽  
Vol 184 (8) ◽  
pp. 2505-2513 ◽  
Author(s):  
Xiaoting Ji ◽  
Haoyuan Lv ◽  
Minghui Ma ◽  
Binglin Lv ◽  
Caifeng Ding

2005 ◽  
Vol 293 (1) ◽  
pp. 106-110 ◽  
Author(s):  
Takuya Kinoshita ◽  
Satoshi Seino ◽  
Yoshiteru Mizukoshi ◽  
Yohei Otome ◽  
Takashi Nakagawa ◽  
...  

Author(s):  
Yasmin Kaveh-Baghbaderani ◽  
Raphaela Allgayer ◽  
Sebastian Patrick Schwaminger ◽  
Paula Fraga-García ◽  
Sonja Berensmeier

Minerals ◽  
2021 ◽  
Vol 11 (3) ◽  
pp. 245
Author(s):  
Toyohisa Fujita ◽  
Taichi Aoki ◽  
Josiane Ponou ◽  
Gjergj Dodbiba ◽  
Chunlin He ◽  
...  

This study investigated the removal of sulfur and iron from shungite rocks through different methods after fine grinding: flotation, magnetic separation, microwave treatment, and chemical leaching. In this work, first, a mineralogical study of shungite was conducted. The carbon, silica, iron, and sulfur compositions in the as-received shungite were 45.4%, 38.3%, 4.6%, and 2.4%, respectively. In flotation, a sulfur grade of 1.4% was obtained. In the wet high-gradient magnetic separation at a magnetic flux density of 1 tesla, the iron and sulfur grades in the nonmagnetic fraction were 2.8% and 1.9%, respectively. Furthermore, the sulfur reduced to 0.2% by the 9 min microwave irradiation. In addition, chemical leaching using chelating reagents and inorganic acids was utilized to remove iron and sulfur. Nitrilotriacetic acid (NTA) could reduce the iron and sulfur grades to 2.0% and 0.9%, respectively. For leaching using reverse aqua regia, the iron and sulfur grades were reduced to 0.9% and 0.23%, respectively. For leaching using a 6N HCl with H2O2 aqueous solution, the iron and sulfur grades were reduced to 0.8% and 0.34%, respectively. Overall, chemical leaching using HCl with H2O2 was the most effective for iron and sulfur removal from shungite.


Minerals ◽  
2021 ◽  
Vol 11 (4) ◽  
pp. 346
Author(s):  
Renata Hiraga ◽  
Otávio Gomes ◽  
Reiner Neumann

Maghemite (γ-Fe2O3) is a mineral formed from magnetite oxidation at low temperatures, an intermediate metastable term of the magnetite to hematite oxidation and could be mixed with both. It has magnetic susceptibility similar to magnetite, crystal structure close to magnetite with which it forms a solid solution, while compositionally it equals hematite. Maghemite is thus easily misidentified as magnetite by Χ-ray diffraction and/or as hematite by spot chemical analysis in iron ore characterization routines. Nonstoichiometric magnetite could be quantified in samples of Brazilian soils and iron ores by the Rietveld method using a constrained refinement of the Χ-ray patterns. The results were confirmed by reflected light microscopy and Raman spectroscopy, thus qualitatively validating the method. Χ-ray diffraction with the refinement of the isomorphic substitution of Fe2+ by Fe3+ along the magnetite-maghemite solid solution could help to suitably characterize maghemite in iron ores, allowing for the evaluation of its ultimate influence on mineral processing, as its effect on surface and breakage properties.


Sign in / Sign up

Export Citation Format

Share Document