| 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. |
| Genre: | Article |
| ProdID: | 70015536 |
| Citation Author: | Webster, D. M. |
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| Citation End Page: | 844 |
| Citation Issue: | 9 |
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| Citation Language: | English |
| Citation Larger Work Title: | Environmental Technology Letters |
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| Citation Number Of Pages: | 12 |
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| Citation Search Results Text: | A semiquantitative X-ray diffraction method to determine mineral composition in stream sediments with similar mineralogy; 1989; Article; Journal; Environmental Technology Letters; Webster, D. M. |
| Citation Start Page: | 833 |
| Citation Volume: | 10 |
| Citation Year: | 1989 |
| Type: | citation/reference |
| Text: | A semiquantitative X-ray diffraction method to determine mineral composition in stream sediments with similar mineralogy; 1989; Article; Journal; Environmental Technology Letters; Webster, D. M. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1989 00:00 -0600 |
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