The biogeochemistry of marine nitrous oxide
Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), June 2011. "June 2011." Cataloged from PDF version of thesis. Inc...
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ftmit:oai:dspace.mit.edu:1721.1/68887 2023-06-11T04:16:42+02:00 The biogeochemistry of marine nitrous oxide Frame, Caitlin H Karen Casciotti. Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering. Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences. 2011 149 p. application/pdf http://hdl.handle.net/1721.1/68887 eng eng Massachusetts Institute of Technology http://hdl.handle.net/1721.1/68887 773364560 M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 Joint Program in Oceanography/Applied Ocean Science and Engineering Earth Atmospheric and Planetary Sciences Woods Hole Oceanographic Institution Nitrification Biogeochemistry Thesis 2011 ftmit 2023-05-29T08:52:13Z Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), June 2011. "June 2011." Cataloged from PDF version of thesis. Includes bibliographical references. Atmospheric nitrous oxide N₂O concentrations have been rising steadily for the past century as a result of human activities. In particular, human perturbation of the nitrogen cycle has increased the N₂O production rates of the two major sources of this greenhouse gas, soil and the ocean. Nitrification, and particularly ammonia oxidation, is one of the major processes that produces N₂O in the ocean. In this thesis, a series of stable isotopic methods have been used to characterize the biogeochemical controls on N₂O production by marine nitrification as well as the natural abundance stable isotopic signatures of N₂O produced by marine nitrifiers. This thesis shows that in addition to chemical controls on N₂O production rates such as oxygen (O₂) and nitrite (NO₂- ) concentrations, there are also biological controls such as nitrifier cell abundances and coastal phytoplankton blooms that may influence N₂O production by ammonia oxidizers as well. Ammonia oxidizers can produce N₂O through two separate biochemical mechanisms that have unique isotopic signatures. Using culture-based measurements of these signatures, we conclude that one of these pathways, nitrifier-denitrification, may be a significant source of N₂O produced in the South Atlantic Ocean and possibly the global ocean. by Caitlin Frame. Ph.D. Thesis South Atlantic Ocean DSpace@MIT (Massachusetts Institute of Technology) |
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English |
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Joint Program in Oceanography/Applied Ocean Science and Engineering Earth Atmospheric and Planetary Sciences Woods Hole Oceanographic Institution Nitrification Biogeochemistry |
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Joint Program in Oceanography/Applied Ocean Science and Engineering Earth Atmospheric and Planetary Sciences Woods Hole Oceanographic Institution Nitrification Biogeochemistry Frame, Caitlin H The biogeochemistry of marine nitrous oxide |
topic_facet |
Joint Program in Oceanography/Applied Ocean Science and Engineering Earth Atmospheric and Planetary Sciences Woods Hole Oceanographic Institution Nitrification Biogeochemistry |
description |
Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), June 2011. "June 2011." Cataloged from PDF version of thesis. Includes bibliographical references. Atmospheric nitrous oxide N₂O concentrations have been rising steadily for the past century as a result of human activities. In particular, human perturbation of the nitrogen cycle has increased the N₂O production rates of the two major sources of this greenhouse gas, soil and the ocean. Nitrification, and particularly ammonia oxidation, is one of the major processes that produces N₂O in the ocean. In this thesis, a series of stable isotopic methods have been used to characterize the biogeochemical controls on N₂O production by marine nitrification as well as the natural abundance stable isotopic signatures of N₂O produced by marine nitrifiers. This thesis shows that in addition to chemical controls on N₂O production rates such as oxygen (O₂) and nitrite (NO₂- ) concentrations, there are also biological controls such as nitrifier cell abundances and coastal phytoplankton blooms that may influence N₂O production by ammonia oxidizers as well. Ammonia oxidizers can produce N₂O through two separate biochemical mechanisms that have unique isotopic signatures. Using culture-based measurements of these signatures, we conclude that one of these pathways, nitrifier-denitrification, may be a significant source of N₂O produced in the South Atlantic Ocean and possibly the global ocean. by Caitlin Frame. Ph.D. |
author2 |
Karen Casciotti. Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering. Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences. |
format |
Thesis |
author |
Frame, Caitlin H |
author_facet |
Frame, Caitlin H |
author_sort |
Frame, Caitlin H |
title |
The biogeochemistry of marine nitrous oxide |
title_short |
The biogeochemistry of marine nitrous oxide |
title_full |
The biogeochemistry of marine nitrous oxide |
title_fullStr |
The biogeochemistry of marine nitrous oxide |
title_full_unstemmed |
The biogeochemistry of marine nitrous oxide |
title_sort |
biogeochemistry of marine nitrous oxide |
publisher |
Massachusetts Institute of Technology |
publishDate |
2011 |
url |
http://hdl.handle.net/1721.1/68887 |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_relation |
http://hdl.handle.net/1721.1/68887 773364560 |
op_rights |
M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 |
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1768375204002660352 |