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Title: Trace element and REE composition of five samples of the Yucca Mountain calcite-silica deposits. Special report No. 8

Abstract

The attached materials document the results of part of a recent effort of geochemical sampling and analysis at Yucca Mountain and nearby regions. The efforts come as a result of interest in comprehensive analyses of rare earth elements (REE), lanthanum (La) through lutecium (Lu). Several additional, non-REE analyses were obtained as well. Commercially available REE analyses have proved to be insufficiently sensitive for geochemical purposes. Dr. Roman Schmitt at the Radiation Center at Oregon State University in Corvallis was sent five samples as a trial effort. The results are very encouraging. The purpose of compiling Dr. Schmitt`s report and the other materials is to inform the sponsor of his independent observations of these results and other information that sent to him. To provide a more complete appreciation of the utility of REE analyses a copy of Dave Vaniman`s recent article is included in which he notes that REE analyses from Yucca Mountain indicate the occurrence of two distinctly different REE patterns as do several other chemical parameters of the calcite-silica deposits. Our four samples with high equivalent CaCO{sub 3} were collected from sites we believe to be spring deposits. One sample, 24D, is from southern Crater Flat which is acknowledgedmore » by U.S.G.S. investigators to be a spring deposit. All four of these samples have REE patterns similar to those from the saturated zone reported by Vaniman.« less

Authors:
Publication Date:
Research Org.:
Technology and Resource Assessment Corp., Boulder, CO (United States)
Sponsoring Org.:
USDOE, Washington, DC (United States)
OSTI Identifier:
196469
Report Number(s):
DOE/NV/10461-T62
ON: DE96006626; TRN: 96:001820
DOE Contract Number:  
FG08-85NV10461
Resource Type:
Technical Report
Resource Relation:
Other Information: PBD: Jul 1993
Country of Publication:
United States
Language:
English
Subject:
05 NUCLEAR FUELS; YUCCA MOUNTAIN; SITE CHARACTERIZATION; HIGH-LEVEL RADIOACTIVE WASTES; UNDERGROUND DISPOSAL; GEOLOGIC DEPOSITS; CHEMICAL COMPOSITION; CALCITE; SILICA; RARE EARTHS; LANTHANUM; LUTETIUM; ELEMENTS; TRACE AMOUNTS

Citation Formats

Livingston, D. Trace element and REE composition of five samples of the Yucca Mountain calcite-silica deposits. Special report No. 8. United States: N. p., 1993. Web. doi:10.2172/196469.
Livingston, D. Trace element and REE composition of five samples of the Yucca Mountain calcite-silica deposits. Special report No. 8. United States. https://doi.org/10.2172/196469
Livingston, D. 1993. "Trace element and REE composition of five samples of the Yucca Mountain calcite-silica deposits. Special report No. 8". United States. https://doi.org/10.2172/196469. https://www.osti.gov/servlets/purl/196469.
@article{osti_196469,
title = {Trace element and REE composition of five samples of the Yucca Mountain calcite-silica deposits. Special report No. 8},
author = {Livingston, D},
abstractNote = {The attached materials document the results of part of a recent effort of geochemical sampling and analysis at Yucca Mountain and nearby regions. The efforts come as a result of interest in comprehensive analyses of rare earth elements (REE), lanthanum (La) through lutecium (Lu). Several additional, non-REE analyses were obtained as well. Commercially available REE analyses have proved to be insufficiently sensitive for geochemical purposes. Dr. Roman Schmitt at the Radiation Center at Oregon State University in Corvallis was sent five samples as a trial effort. The results are very encouraging. The purpose of compiling Dr. Schmitt`s report and the other materials is to inform the sponsor of his independent observations of these results and other information that sent to him. To provide a more complete appreciation of the utility of REE analyses a copy of Dave Vaniman`s recent article is included in which he notes that REE analyses from Yucca Mountain indicate the occurrence of two distinctly different REE patterns as do several other chemical parameters of the calcite-silica deposits. Our four samples with high equivalent CaCO{sub 3} were collected from sites we believe to be spring deposits. One sample, 24D, is from southern Crater Flat which is acknowledged by U.S.G.S. investigators to be a spring deposit. All four of these samples have REE patterns similar to those from the saturated zone reported by Vaniman.},
doi = {10.2172/196469},
url = {https://www.osti.gov/biblio/196469}, journal = {},
number = ,
volume = ,
place = {United States},
year = {Thu Jul 01 00:00:00 EDT 1993},
month = {Thu Jul 01 00:00:00 EDT 1993}
}