Groundwater dynamics in degrading, discontinuous permafrost

Thesis (M.S.) University of Alaska Fairbanks, 2014 In regions impacted by permafrost, discontinuities are areas of possible connection between the supra- and sub-permafrost portions of an aquifer. Permafrost discontinuities influence the transport of contaminants in an aquifer, necessitating delinea...

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Main Author: Barnes, Michelle L.
Other Authors: Barnes, David L., Shur, Yuri L., Schnabel, William E., Leigh, Mary Beth
Format: Thesis
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/11122/4896
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/4896 2023-05-15T17:55:17+02:00 Groundwater dynamics in degrading, discontinuous permafrost Barnes, Michelle L. Barnes, David L. Shur, Yuri L. Schnabel, William E. Leigh, Mary Beth 2014-12 http://hdl.handle.net/11122/4896 en_US eng http://hdl.handle.net/11122/4896 Department of Civil and Environmental Engineering Thesis ms 2014 ftunivalaska 2023-02-23T21:36:19Z Thesis (M.S.) University of Alaska Fairbanks, 2014 In regions impacted by permafrost, discontinuities are areas of possible connection between the supra- and sub-permafrost portions of an aquifer. Permafrost discontinuities influence the transport of contaminants in an aquifer, necessitating delineation of these discontinuities and their influence on groundwater flow. Means of identifying the locations of permafrost discontinuities have previously been limited to geophysical methods and the evaluation of well logs. In this study we use groundwater elevation trends and environmental tracers (e.g., stable isotopes and temperature) to evaluate the dynamics in a sulfolane-contaminated aquifer located in a region of discontinuous permafrost in the Interior of Alaska. Using tracers to identify areas of discontinuities in the permafrost should help us locate thawed through-taliks and may also improve our understanding of the interaction between the supra- and sub-permafrost groundwater in discontinuous permafrost. With this approach we identified at least three discontinuities within the study area. The locations of these discontinuities coincide with transport of the contaminant found in this aquifer. The primary source of recharge for this aquifer is the Tanana River, a major tributary to the Yukon River. The source of water for the Tanana River is glacial melt in the summer and groundwater during the winter. Through the isotopic composition of the supra-permafrost groundwater we show the occurrence of additional recharge to the supra-permafrost groundwater from sub-permafrost groundwater and precipitation. Understanding these dynamics is paramount to characterizing the contaminant transport in permafrost impacted aquifers. 1 Introduction -- 1.1 Thesis Objectives -- 2 Site Description -- 2.1.1 Sulfolane Contamination -- 2.1.1.1 Contaminant Characteristics -- 2.1.1.2 Groundwater Contamination -- 2.1.2 Climate, Land Use and Land Cover -- 2.1.3 Geology and Permafrost -- 2.1.4 Hydrology -- 2.1.4.1 Aquifer Recharge ... Thesis permafrost Yukon river Alaska Yukon University of Alaska: ScholarWorks@UA Fairbanks Yukon
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
description Thesis (M.S.) University of Alaska Fairbanks, 2014 In regions impacted by permafrost, discontinuities are areas of possible connection between the supra- and sub-permafrost portions of an aquifer. Permafrost discontinuities influence the transport of contaminants in an aquifer, necessitating delineation of these discontinuities and their influence on groundwater flow. Means of identifying the locations of permafrost discontinuities have previously been limited to geophysical methods and the evaluation of well logs. In this study we use groundwater elevation trends and environmental tracers (e.g., stable isotopes and temperature) to evaluate the dynamics in a sulfolane-contaminated aquifer located in a region of discontinuous permafrost in the Interior of Alaska. Using tracers to identify areas of discontinuities in the permafrost should help us locate thawed through-taliks and may also improve our understanding of the interaction between the supra- and sub-permafrost groundwater in discontinuous permafrost. With this approach we identified at least three discontinuities within the study area. The locations of these discontinuities coincide with transport of the contaminant found in this aquifer. The primary source of recharge for this aquifer is the Tanana River, a major tributary to the Yukon River. The source of water for the Tanana River is glacial melt in the summer and groundwater during the winter. Through the isotopic composition of the supra-permafrost groundwater we show the occurrence of additional recharge to the supra-permafrost groundwater from sub-permafrost groundwater and precipitation. Understanding these dynamics is paramount to characterizing the contaminant transport in permafrost impacted aquifers. 1 Introduction -- 1.1 Thesis Objectives -- 2 Site Description -- 2.1.1 Sulfolane Contamination -- 2.1.1.1 Contaminant Characteristics -- 2.1.1.2 Groundwater Contamination -- 2.1.2 Climate, Land Use and Land Cover -- 2.1.3 Geology and Permafrost -- 2.1.4 Hydrology -- 2.1.4.1 Aquifer Recharge ...
author2 Barnes, David L.
Shur, Yuri L.
Schnabel, William E.
Leigh, Mary Beth
format Thesis
author Barnes, Michelle L.
spellingShingle Barnes, Michelle L.
Groundwater dynamics in degrading, discontinuous permafrost
author_facet Barnes, Michelle L.
author_sort Barnes, Michelle L.
title Groundwater dynamics in degrading, discontinuous permafrost
title_short Groundwater dynamics in degrading, discontinuous permafrost
title_full Groundwater dynamics in degrading, discontinuous permafrost
title_fullStr Groundwater dynamics in degrading, discontinuous permafrost
title_full_unstemmed Groundwater dynamics in degrading, discontinuous permafrost
title_sort groundwater dynamics in degrading, discontinuous permafrost
publishDate 2014
url http://hdl.handle.net/11122/4896
geographic Fairbanks
Yukon
geographic_facet Fairbanks
Yukon
genre permafrost
Yukon river
Alaska
Yukon
genre_facet permafrost
Yukon river
Alaska
Yukon
op_relation http://hdl.handle.net/11122/4896
Department of Civil and Environmental Engineering
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