Lability of dissolved organic carbon in Arctic rivers on the North Slope of Alaska

Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2007.

Bibliographic Details
Main Author: Frazer, Breton B
Other Authors: Robert (Max) Holmes and Roger Summons.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2018
Subjects:
Online Access:http://hdl.handle.net/1721.1/114329
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author Frazer, Breton B
author2 Robert (Max) Holmes and Roger Summons.
author_facet Robert (Max) Holmes and Roger Summons.
Frazer, Breton B
author_sort Frazer, Breton B
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description Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2007.
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spelling mit-1721.1/1143292019-04-11T08:43:41Z Lability of dissolved organic carbon in Arctic rivers on the North Slope of Alaska Frazer, Breton B Robert (Max) Holmes and Roger Summons. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Earth, Atmospheric, and Planetary Sciences. Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2007. Cataloged from PDF version of thesis. Includes bibliographical references (pages 16-18). Rivers are an important pathway of organic carbon-mobilization in the arctic, and their influence is projected to grow as precipitation and soil temperatures increase in response to highlatitude warming. This study addresses the bioactivity of arctic riverine dissolved organic carbon (DOC) in three North Slope Alaskan rivers: the Kuparuk, the Colville, and the Sagavanirktok. While lability experiments have previously been conducted during late summer discharge on arctic rivers, none have analyzed the early hydrograph spring-melt peak DOC. During the summer of 2006, water samples were taken from significant periods of the hydrograph (upswing, peak, downswing, and quasi-stable summer) of the three rivers for DOC lability experiments. DOC from spring melt discharge proved to be highly labile and therefore dynamically different from summer DOC. Over a three-month sample incubation period, these samples lost up to 40 and 33 percent of their DOC (with and without added nutrients, respectively) while samples taken later in summer lost merely 9 and 5 percent. As spring melt contributes half of the total annual discharge and DOC flux of winter-freezing rivers, a significant portion of annual arctic DOC is labile and is therefore a large input of bioactive organic DOC to the Arctic Ocean carbon cycle. by Breton B. Frazer. S.B. 2018-03-27T14:17:45Z 2018-03-27T14:17:45Z 2007 2007 Thesis http://hdl.handle.net/1721.1/114329 1028748527 eng MIT theses are protected by copyright. They may be viewed, downloaded, or printed from this source but further reproduction or distribution in any format is prohibited without written permission. http://dspace.mit.edu/handle/1721.1/7582 27 pages application/pdf n-us-ak Massachusetts Institute of Technology
spellingShingle Earth, Atmospheric, and Planetary Sciences.
Frazer, Breton B
Lability of dissolved organic carbon in Arctic rivers on the North Slope of Alaska
title Lability of dissolved organic carbon in Arctic rivers on the North Slope of Alaska
title_full Lability of dissolved organic carbon in Arctic rivers on the North Slope of Alaska
title_fullStr Lability of dissolved organic carbon in Arctic rivers on the North Slope of Alaska
title_full_unstemmed Lability of dissolved organic carbon in Arctic rivers on the North Slope of Alaska
title_short Lability of dissolved organic carbon in Arctic rivers on the North Slope of Alaska
title_sort lability of dissolved organic carbon in arctic rivers on the north slope of alaska
topic Earth, Atmospheric, and Planetary Sciences.
url http://hdl.handle.net/1721.1/114329
work_keys_str_mv AT frazerbretonb labilityofdissolvedorganiccarboninarcticriversonthenorthslopeofalaska