A semiquantitative X-ray diffraction method to determine mineral composition in stream sediments with similar mineralogy

Environmental Technology Letters
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Abstract

A semiquantitative X‐ray diffraction procedure has been developed that can be used to acquire reproducible mineralogic data from geographically unrelated stream‐sediment samples having similar mineralogy. Weight percentages for quartz, total‐feldspar, and total‐clay can be determined by direct comparison of intensities with standard‐mineral mixtures of known weight percent. Matrix effects and mass‐absorption differences are circumvented by taking the ratio of peak‐intensity, in counts per second, for quartz relative to that of other minerals being quantified. Mineral percentages generally are reproducible to within 10 percent.

Publication type Article
Publication Subtype Journal Article
Title A semiquantitative X-ray diffraction method to determine mineral composition in stream sediments with similar mineralogy
Series title Environmental Technology Letters
DOI 10.1080/09593338909384803
Volume 10
Issue 9
Year Published 1989
Language English
Publisher Taylor & Francis
Contributing office(s) National Research Program - Eastern Branch
Description 12 p.
First page 833
Last page 844
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