Minerals Beneficiation - The Behavior of Mesabi Iron and Silicate Minerals in 20-Kilogauss Magnetic Fields

The American Institute of Mining, Metallurgical, and Petroleum Engineers
J. E. Lawver J. L. Wright H. R. Kokat
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
10
File Size:
1967 KB
Publication Date:
Jan 1, 1969

Abstract

Mesabi semitaconite and oxidized taconite ores that cannot be concentrated by froth flotation can be rendered amenable to flotation through partial concentration in a high-in tensity wet magnetic separator. Since 1964, a method for accomplishing this precon-centration has been under development at the Minnesota Mines Experiment Station, where several hundred tons of ore have been successfully processed. This paper is an analysis of the performance of the separators used at the Station. At present the United States is producing about 85 million tons of iron ore a year, and nearly 55 million tons of this comes from Minnesota. Nearly half of Minnesota's production is in the form of magnetite taconite pellets —the remainder being wash ore and gravity concentrates. As the demands of the blast furnace operators become more stringent - and they are becoming more so yearly — these demands are met by improved iron ore beneficiation technology. Furthermore, there is no doubt that as magnetite taconite, gravity ores, and wash ores are exhausted, new processes will be developed to produce a product comparable to magnetite taconite pellets from Minnesota's vast reserves of oxidized taconite and semitaconite. The magnetite taconite ores are rather easily bene-ficiated by conventional, low-intensity (500- to 1400-gauss) magnetic separators, followed, in some plants, by froth flotation of the magnetic concentrates.
Citation

APA: J. E. Lawver J. L. Wright H. R. Kokat  (1969)  Minerals Beneficiation - The Behavior of Mesabi Iron and Silicate Minerals in 20-Kilogauss Magnetic Fields

MLA: J. E. Lawver J. L. Wright H. R. Kokat Minerals Beneficiation - The Behavior of Mesabi Iron and Silicate Minerals in 20-Kilogauss Magnetic Fields. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1969.

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