| 2006 Philadelphia Annual Meeting (22–25 October 2006) | |
| Paper No. 143-2 | |
| Presentation Time: 8:00 AM-12:00 PM | ||
PREPARATION AND X-RAY FLUORESCENCE (XRF) ANALYSIS OF RIVERBED SEDIMENTS FROM VARYING LITHOLOGY | ||
|
GOLDSMITH, Steven1, CAREY, Anne E.2, and BHATTIPROLU, Sreenivas2, (1) Geological Sciences, The Ohio State University, 275 Mendenhall Laboratory, 125 South Oval Mall, Columbus, OH 43210-1308, goldsmith.35@osu.edu, (2) Department of Geological Sciences, The Ohio State Univ, 275 Mendenhall Lab, 125 South Oval Mall, Columbus, OH 43210 Recent advances in sample preparation and x-ray fluorescence (XRF) analytical techniques have allowed these measurements of soil and sediment samples to be included in published studies. Previous studies have often faced limitations in the number of elements analyzed due to sample size considerations. In the case of riverine sediments, dilution of elemental concentration can come as the result of input from varying watershed lithology. Additional loss of sample quantity via loss on ignition, particularly from organic carbon, has also been found to complicate these measurements. Furthermore, many studies currently publishing XRF analytical data for soil and sediment do not provide precision and accuracy values for known standards analyzed as samples. Herein we present results for riverbed sediments of mixed lithology prepared and analyzed via XRF microscopy for major oxides and select minor and trace elements at both 1:4 and 1:10 sample to flux ratios. Our results reveal publication quality results can be readily achieved and reproduced with as little as one gram of sample. | ||
|
2006 Philadelphia Annual Meeting (22–25 October 2006)
General Information for this Meeting | ||
| Session No. 143--Booth# 35 Sigma Gamma Epsilon Student Research (Posters) Pennsylvania Convention Center: Exhibit Hall C 8:00 AM-12:00 PM, Tuesday, 24 October 2006 Geological Society of America Abstracts with Programs, Vol. 38, No. 7, p. 352 | ||
© Copyright 2006 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. | ||