An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska

Iron in seawater is biologically significant for its contribution to primary productivity. This study showed a high livel of iron in Glacier Bay, as well as higher values for the metal in water beneath the mixed layer. This suggests that sediments are the source for iron in the bay.

Bibliographic Details
Main Author: Peterson, Marcus
Format: Other/Unknown Material
Language:English
Published: School of Oceanography, University of Washington 2008
Subjects:
Carbon cycle (biogeochemistry) > Alaska > Glacier Bay
Trace elements
Seawater > Iron content > analysis
Glacier Bay
glacier
Alaska
Online Access:http://hdl.handle.net/1773/3767
id ftunivwashington:oai:digital.lib.washington.edu:1773/3767
record_format openpolar
spelling ftunivwashington:oai:digital.lib.washington.edu:1773/3767 2024-06-02T08:07:00+00:00 An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska Peterson, Marcus 2008-06-19 http://hdl.handle.net/1773/3767 en_US eng School of Oceanography, University of Washington Keil R., Kelley D., D'Asaro E., Krembs C., and Collins R.E. [Eds.] 2008. Proceedings from the University of Washington School of Oceanography Undergraduate Thesis Research Expedition to Glacier Bay Alaska, March 2008. 296pp. http://hdl.handle.net/1773/3767 Carbon cycle (biogeochemistry)--Alaska--Glacier Bay Trace elements Seawater--Iron content--analysis Other 2008 ftunivwashington 2024-05-06T11:36:59Z Iron in seawater is biologically significant for its contribution to primary productivity. This study showed a high livel of iron in Glacier Bay, as well as higher values for the metal in water beneath the mixed layer. This suggests that sediments are the source for iron in the bay. Other/Unknown Material glacier Alaska University of Washington, Seattle: ResearchWorks Glacier Bay
institution Open Polar
collection University of Washington, Seattle: ResearchWorks
op_collection_id ftunivwashington
language English
topic Carbon cycle (biogeochemistry)--Alaska--Glacier Bay
Trace elements
Seawater--Iron content--analysis
spellingShingle Carbon cycle (biogeochemistry)--Alaska--Glacier Bay
Trace elements
Seawater--Iron content--analysis
Peterson, Marcus
An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska
topic_facet Carbon cycle (biogeochemistry)--Alaska--Glacier Bay
Trace elements
Seawater--Iron content--analysis
description Iron in seawater is biologically significant for its contribution to primary productivity. This study showed a high livel of iron in Glacier Bay, as well as higher values for the metal in water beneath the mixed layer. This suggests that sediments are the source for iron in the bay.
format Other/Unknown Material
author Peterson, Marcus
author_facet Peterson, Marcus
author_sort Peterson, Marcus
title An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska
title_short An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska
title_full An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska
title_fullStr An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska
title_full_unstemmed An investigation into sources and distributions of iron, aluminum, and nutrients in Glacier Bay, Alaska
title_sort investigation into sources and distributions of iron, aluminum, and nutrients in glacier bay, alaska
publisher School of Oceanography, University of Washington
publishDate 2008
url http://hdl.handle.net/1773/3767
geographic Glacier Bay
geographic_facet Glacier Bay
genre glacier
Alaska
genre_facet glacier
Alaska
op_relation Keil R., Kelley D., D'Asaro E., Krembs C., and Collins R.E. [Eds.] 2008. Proceedings from the University of Washington School of Oceanography Undergraduate Thesis Research Expedition to Glacier Bay Alaska, March 2008. 296pp.
http://hdl.handle.net/1773/3767
_version_ 1800752012398166016

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