A METHOD FOR QUANTITATIVE DETERMINATION OF SOIL MINERALS BY X-RAY DIFFRACTION (ABRIDGMENT)

This paper describes the theory and initial test results for a method of quantitatively determining the amount of various mineral components in a soil sample by comparing X-ray diffraction peak intensities of the mineral in the sample with the intensities of the same peak in specimens that are a mixture of the original soil sample and known additional amounts of the mineral in question. That is, the component being determined is used as an internal standard.

Media Info

  • Media Type: Print
  • Features: Figures; References;
  • Pagination: pp 75-80
  • Monograph Title: Stabilization
  • Serial:

Subject/Index Terms

Filing Info

  • Accession Number: 00134002
  • Record Type: Publication
  • ISBN: 0309024706
  • Files: TRIS, TRB
  • Created Date: Jul 22 1976 12:00AM