My Account: Log In | Join | Renew
Search
Author
Title
Vol.
Issue
Year
1st Page

Abstract

 

This article in SSSAJ

  1. Vol. 3 No. C, p. 20-25
     
    Published: 1939


 View
 Download
 Alerts
 Permissions

doi:10.2136/sssaj1939.036159950003000C0004x

Further Results on the Mineralogical Subdivision of Soil Separates by Means of Heavy Liquid Specific Gravity Separations1

  1. R. W. Pearson and
  2. E. Truog2

Summary

Summary

Following the work previously reported regarding the mineralogical subdivision of soil material by means of heavy liquid specific gravity separations, an attempt has been made to improve the procedure. The special centrifuge tube previously described for specific gravity separations was redesigned so as to be of simpler construction and of larger capacity.

The results of specific gravity separations of various mechanical separates of soil and nontronite are given. Petrographic methods were employed to check the sharpness of the separations in the case of material of particle size greater than 1.0µ in diameter. Quantitative separations of the mineral groups in sand and silt fractions were effected. In the case of coarse clay (particles 2.0 to 0.2µ in diameter) the separations were quantitative except for traces of talc and biotite in the lighter fractions. The bulk of the base exchange material in the Lufkin clay, and in nontronite, was found in the specific gravity fraction 2.18 to 2.33. It was also found that the quantity of minerals of low specific gravity increases greatly with diminishing particle size.

The results obtained in this study indicate that separation by means of the specific gravity procedure outlined, offers considerable promise as a means of separating and concentrating the mineral species in not only the coarser but also the finer soil separates. This should be of great help in mineralogical studies of soil material by the use of petrographic, chemical. and x-ray methods.

  Please view the pdf by using the Full Text (PDF) link under 'View' to the left.

Copyright © . Soil Science Society of America

Facebook   Twitter