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Title: Soil-gas radon analyses in the Mt. Rose and Lovelock areas, west-central Nevada

Abstract

Soil-gas radon has been sampled and analyzed in two area of differing surficial geology in west-central Nevada. Elevated levels of indoor radon have been found in both area. The Mt. Rose alluvial fan complex, located just southwest of Reno, is an alluvial fan/pediment formed by flow from major drainages in the Carson Range. The surface of the Mt. Rose fan is dominated by glacial outwash deposits believed to be of Donner Lake and Tahoe age. These two units have somewhat differing lithologies and degrees of soil development. The Donner Lake outwash is dominated by volcanic clasts and typically has a thick argillic B-horizon and a moderately to strongly developed duripan. The Tahoe outwash has a mixture of volcanic and granitic clasts and typically has a thinner argillic B-horizon and no duripan. Soil-gas radon levels are generally higher in the Tahoe outwash, probably reflecting either greater emanation from granitic clasts or differences in soil gas permeability. Radon levels along Holocene faults cutting these outwash deposits are fairly typical for the study area and minor differences may be due to the faults' effects on soil gas permeability. Lovelock, about 90 miles northeast of Reno, is located within the Humboldt Sink, one ofmore » the lowest parts of the pluvial Lake Lahontan basin. Surficial geology in this area is dominated by fine-grained lacustrine deposits and overbank alluvium from the Humboldt River. During interpluvial periods, this is commonly a marshy area resulting from Humboldt River flow into the basin. Elevated radon levels are likely due to uranium accumulation in black, organic-rich clay layers.« less

Authors:
; ;  [1]
  1. (Univ. of Nevada, Reno, NV (United States))
Publication Date:
OSTI Identifier:
5023398
Report Number(s):
CONF-9305259--
Journal ID: ISSN 0016-7592; CODEN: GAAPBC
Resource Type:
Conference
Resource Relation:
Journal Name: Geological Society of America, Abstracts with Programs; (United States); Journal Volume: 25:5; Conference: 89. annual meeting of the Cordilleran Section and the 46th annual meeting of the Rocky Mountain Section of the Geological Society of America (GSA), Reno, NV (United States), 19-21 May 1993
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; ALLUVIAL DEPOSITS; NATURAL RADIOACTIVITY; NEVADA; RADON; RADIOECOLOGICAL CONCENTRATION; RADIONUCLIDE MIGRATION; MONITORING; SOIL CHEMISTRY; SOILS; CHEMISTRY; DEVELOPED COUNTRIES; ECOLOGICAL CONCENTRATION; ELEMENTS; ENVIRONMENTAL TRANSPORT; FLUIDS; GASES; GEOLOGIC DEPOSITS; MASS TRANSFER; NONMETALS; NORTH AMERICA; RADIOACTIVITY; RARE GASES; USA 580000* -- Geosciences

Citation Formats

Ramelli, A.R., Rigby, J.G., and LaPointe, D.D.. Soil-gas radon analyses in the Mt. Rose and Lovelock areas, west-central Nevada. United States: N. p., 1993. Web.
Ramelli, A.R., Rigby, J.G., & LaPointe, D.D.. Soil-gas radon analyses in the Mt. Rose and Lovelock areas, west-central Nevada. United States.
Ramelli, A.R., Rigby, J.G., and LaPointe, D.D.. 1993. "Soil-gas radon analyses in the Mt. Rose and Lovelock areas, west-central Nevada". United States. doi:.
@article{osti_5023398,
title = {Soil-gas radon analyses in the Mt. Rose and Lovelock areas, west-central Nevada},
author = {Ramelli, A.R. and Rigby, J.G. and LaPointe, D.D.},
abstractNote = {Soil-gas radon has been sampled and analyzed in two area of differing surficial geology in west-central Nevada. Elevated levels of indoor radon have been found in both area. The Mt. Rose alluvial fan complex, located just southwest of Reno, is an alluvial fan/pediment formed by flow from major drainages in the Carson Range. The surface of the Mt. Rose fan is dominated by glacial outwash deposits believed to be of Donner Lake and Tahoe age. These two units have somewhat differing lithologies and degrees of soil development. The Donner Lake outwash is dominated by volcanic clasts and typically has a thick argillic B-horizon and a moderately to strongly developed duripan. The Tahoe outwash has a mixture of volcanic and granitic clasts and typically has a thinner argillic B-horizon and no duripan. Soil-gas radon levels are generally higher in the Tahoe outwash, probably reflecting either greater emanation from granitic clasts or differences in soil gas permeability. Radon levels along Holocene faults cutting these outwash deposits are fairly typical for the study area and minor differences may be due to the faults' effects on soil gas permeability. Lovelock, about 90 miles northeast of Reno, is located within the Humboldt Sink, one of the lowest parts of the pluvial Lake Lahontan basin. Surficial geology in this area is dominated by fine-grained lacustrine deposits and overbank alluvium from the Humboldt River. During interpluvial periods, this is commonly a marshy area resulting from Humboldt River flow into the basin. Elevated radon levels are likely due to uranium accumulation in black, organic-rich clay layers.},
doi = {},
journal = {Geological Society of America, Abstracts with Programs; (United States)},
number = ,
volume = 25:5,
place = {United States},
year = 1993,
month = 4
}

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