The biogeochemistry of marine nitrous oxide

Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution June 2011 Atmospheric nitrous oxide N2O concentrations have been rising steadily for the past century as a result of h...

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Main Author: Frame, Caitlin H.
Format: Thesis
Language:English
Published: Massachusetts Institute of Technology and Woods Hole Oceanographic Institution 2011
Subjects:
Ida
Online Access:https://hdl.handle.net/1912/4735
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/4735 2023-05-15T18:20:58+02:00 The biogeochemistry of marine nitrous oxide Frame, Caitlin H. South Atlantic Ocean 2011-06 application/pdf https://hdl.handle.net/1912/4735 en_US eng Massachusetts Institute of Technology and Woods Hole Oceanographic Institution WHOI Theses https://hdl.handle.net/1912/4735 doi:10.1575/1912/4735 doi:10.1575/1912/4735 Nitrification Biogeochemistry Knorr (Ship : 1970-) Cruise KN192-05 Thesis 2011 ftwhoas https://doi.org/10.1575/1912/4735 2022-05-28T22:58:25Z Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution June 2011 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 (NO-2) 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. Funding for this work was provided by NSF/OCE 05-26277, the Andrew W. Mellon Founda- tion Awards for Innovative Research, the Cecil H. and Ida M. Green Technology Innovation Awards, and the W. M. Keck Foundation. Thesis South Atlantic Ocean Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Ida ENVELOPE(170.483,170.483,-83.583,-83.583) Woods Hole, MA
institution Open Polar
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
op_collection_id ftwhoas
language English
topic Nitrification
Biogeochemistry
Knorr (Ship : 1970-) Cruise KN192-05
spellingShingle Nitrification
Biogeochemistry
Knorr (Ship : 1970-) Cruise KN192-05
Frame, Caitlin H.
The biogeochemistry of marine nitrous oxide
topic_facet Nitrification
Biogeochemistry
Knorr (Ship : 1970-) Cruise KN192-05
description Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution June 2011 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 (NO-2) 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. Funding for this work was provided by NSF/OCE 05-26277, the Andrew W. Mellon Founda- tion Awards for Innovative Research, the Cecil H. and Ida M. Green Technology Innovation Awards, and the W. M. Keck Foundation.
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 and Woods Hole Oceanographic Institution
publishDate 2011
url https://hdl.handle.net/1912/4735
op_coverage South Atlantic Ocean
long_lat ENVELOPE(170.483,170.483,-83.583,-83.583)
geographic Ida
geographic_facet Ida
genre South Atlantic Ocean
genre_facet South Atlantic Ocean
op_source doi:10.1575/1912/4735
op_relation WHOI Theses
https://hdl.handle.net/1912/4735
doi:10.1575/1912/4735
op_doi https://doi.org/10.1575/1912/4735
op_publisher_place Woods Hole, MA
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