Visible and Near Infrared Absorption Coefficients of Kaolinite and Related Clays.

Abstract

TRA, Kaolinite, ReflectanceHalloysite, DickiteClay minerals, by their very nature, are always composed of aggregates of fine particles, a situation which makes conventional transmission spectroscopy and application of the Bouguer-Lambert law difficult, because of the intense scattering of light in the sample. For this reason only qualitative information about the absorption spectra of such minerals is available. Although such spectra are very useful in studies of the structure of minerals, more quantitative absorption information is needed to assess the effect of clay particles on the propagation of light. This work is intended to provide a quantitative estimate of the absorption coefficient of kaolinite clays by application of a method based on the Kubelka-Munk theory of diffuse reflectance.

Document Details

Document Type
Technical Report
Publication Date
Nov 01, 1973
Accession Number
AD0770920

Entities

People

  • James D. Lindberg
  • Michael S. Smith

Organizations

  • United States Army Communications-Electronics Command

Tags

DTIC Thesaurus Topics

  • Absorption
  • Absorption Coefficients
  • Absorption Spectra
  • Coefficients
  • Diffraction
  • Minerals
  • Particles
  • Phyllosilicates
  • Reflectance
  • Scattering
  • Sorption
  • Spectra
  • Spectroscopy

Readers

  • Agricultural Chemistry/Soil Science
  • Spectroscopy.