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Abstract

 

This article in SSSAJ

  1. Vol. 43 No. 4, p. 793-799
     
    Received: Mar 14, 1978
    Accepted: Mar 19, 1979


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doi:10.2136/sssaj1979.03615995004300040036x

High Gradient Magnetic Separation of Iron Oxides and other Magnetic Minerals from Soil Clays1

  1. D. G. Schulze and
  2. J. B. Dixon2

Abstract

Abstract

A filter of ferromagnetic stainless steel wool, placed in a strong magnetic field, provides the magnetic field gradients necessary to trap weakly magnetic clay size particles from a flowing suspension.

Of the total dithionite-citrate-bicarbonate extractable Fe2O3 in the 2–0.2 µm size fraction of six soils, 70 to 94% was recovered in the magnetic fraction which consisted of 1.6 to 27.7% free Fe2O3 by weight. For the <0.2 µm size fraction, 11 to 40% of the total free Fe2O3 in the size fraction was recovered in the magnetic fraction which contained 2.8 to 53.1% free Fe2O3 by weight. Larger particles are captured more efficiently because of their greater overall magnetic attraction. Goethite, hematite, lepidocrocite, and anatase are concentrated in the magnetic fraction, while quartz is concentrated in the tailings. Chlorite is effectively concentrated in the magnetic fraction. Although mica, vermiculite, and smectite are often found in both the tailings and the magnetic fraction, vermiculite and mica appear to be more concentrated in the magnetic fraction. The concentration effect on kaolinite appears to be dependent on the particle size and rate of flow through the magnetic filter.

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