Hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: Grants, New Mexico

Study region: Lower San Mateo Creek Basin (SMCB), New Mexico Study focus: Groundwater in the alluvial aquifer of the lower SMCB has a high concentration of total dissolved solids, alkalinity, and dissolved uranium at concentrations above USEPA limits; the source of the water quality was investigated...

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Main Authors: Shannon Ulrich, Jeffrey Gillow, Shawn Roberts, Gregory Byer, Julie Sueker, Kathryn Farris
Format: Article
Language:English
Published: Elsevier 2019-12-01
Series:Journal of Hydrology: Regional Studies
Online Access:http://www.sciencedirect.com/science/article/pii/S221458181930134X
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spelling doaj-3e283325c3f347a3ab4cc3c3ed63d5792020-11-25T03:34:57ZengElsevierJournal of Hydrology: Regional Studies2214-58182019-12-0126Hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: Grants, New MexicoShannon Ulrich0Jeffrey Gillow1Shawn Roberts2Gregory Byer3Julie Sueker4Kathryn Farris5Arcadis North America, 11001 West 120th Avenue, Suite 200, Broomfield CO, 80021, United States; Corresponding author.Jacobs Engineering Group, 9191 South Jamaica Street, Englewood, CO 80112, United StatesArcadis North America, 735 Tank Farm Road, Suite 150, San Luis Obispo, CA 93401, United StatesArcadis North America, 150 West Market Street, Suite 728, Indianapolis IN 46204, United StatesArcadis North America, 11001 West 120th Avenue, Suite 200, Broomfield CO, 80021, United StatesArcadis North America, 855 Route 146 Suite 210, Clifton Park NY 12065, United StatesStudy region: Lower San Mateo Creek Basin (SMCB), New Mexico Study focus: Groundwater in the alluvial aquifer of the lower SMCB has a high concentration of total dissolved solids, alkalinity, and dissolved uranium at concentrations above USEPA limits; the source of the water quality was investigated through evaluation of geology, mineralogy, and geochemistry of sediments and groundwater. Surface-expressing bedrock in the larger Basin is dominated by uranium-bearing units such as the Morrison Formation and Dakota Sandstone; erosion of these units contributed sediment to Quaternary alluvium valley fill in the Basin with heterogeneous distribution of uranium. The potential for uranium-bearing alluvial fill to affect the groundwater quality was investigated upgradient of the Grants Reclamation Project (GRP), a former uranium milling facility in the lower SMCB, by hydrogeochemical and geophysical methods. New hydrological insights for the region: Uranium is primarily associated with fine-grained materials (clay/silt) and is labile depending upon sediment geochemical conditions. Natural occurrence of uranium minerals in SMCB alluvial sediments here results in concentrations in groundwater greater than the USEPA water quality standards; as such, site-specific standards are established and supported by the findings of this work. Regional groundwater systems, derived from weathered mineralized bedrock, require careful evaluation of water quality to understand background conditions; uranium in groundwater results from hydrogeochemical processes at the interface of fine and coarse grained sediments within the aquifer. Keywords: Grants mineral belt, San Mateo Creek Basin, Eroded sandstone bedrock, Alluvial aquifer, Uranium, Lithologic analysishttp://www.sciencedirect.com/science/article/pii/S221458181930134X
collection DOAJ
language English
format Article
sources DOAJ
author Shannon Ulrich
Jeffrey Gillow
Shawn Roberts
Gregory Byer
Julie Sueker
Kathryn Farris
spellingShingle Shannon Ulrich
Jeffrey Gillow
Shawn Roberts
Gregory Byer
Julie Sueker
Kathryn Farris
Hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: Grants, New Mexico
Journal of Hydrology: Regional Studies
author_facet Shannon Ulrich
Jeffrey Gillow
Shawn Roberts
Gregory Byer
Julie Sueker
Kathryn Farris
author_sort Shannon Ulrich
title Hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: Grants, New Mexico
title_short Hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: Grants, New Mexico
title_full Hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: Grants, New Mexico
title_fullStr Hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: Grants, New Mexico
title_full_unstemmed Hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: Grants, New Mexico
title_sort hydrogeochemical and mineralogical factors influencing uranium in background area groundwater wells: grants, new mexico
publisher Elsevier
series Journal of Hydrology: Regional Studies
issn 2214-5818
publishDate 2019-12-01
description Study region: Lower San Mateo Creek Basin (SMCB), New Mexico Study focus: Groundwater in the alluvial aquifer of the lower SMCB has a high concentration of total dissolved solids, alkalinity, and dissolved uranium at concentrations above USEPA limits; the source of the water quality was investigated through evaluation of geology, mineralogy, and geochemistry of sediments and groundwater. Surface-expressing bedrock in the larger Basin is dominated by uranium-bearing units such as the Morrison Formation and Dakota Sandstone; erosion of these units contributed sediment to Quaternary alluvium valley fill in the Basin with heterogeneous distribution of uranium. The potential for uranium-bearing alluvial fill to affect the groundwater quality was investigated upgradient of the Grants Reclamation Project (GRP), a former uranium milling facility in the lower SMCB, by hydrogeochemical and geophysical methods. New hydrological insights for the region: Uranium is primarily associated with fine-grained materials (clay/silt) and is labile depending upon sediment geochemical conditions. Natural occurrence of uranium minerals in SMCB alluvial sediments here results in concentrations in groundwater greater than the USEPA water quality standards; as such, site-specific standards are established and supported by the findings of this work. Regional groundwater systems, derived from weathered mineralized bedrock, require careful evaluation of water quality to understand background conditions; uranium in groundwater results from hydrogeochemical processes at the interface of fine and coarse grained sediments within the aquifer. Keywords: Grants mineral belt, San Mateo Creek Basin, Eroded sandstone bedrock, Alluvial aquifer, Uranium, Lithologic analysis
url http://www.sciencedirect.com/science/article/pii/S221458181930134X
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