Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters

Nitrogen (N) transport from land to water is a dominant contributor of N in estuarine waters leading to eutrophication, harmful algal blooms, and hypoxia. Our objectives were to (1) investigate the composition of inorganic and organic N forms, (2) distinguish the sources and biogeochemical mechanism...

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Main Authors: Jani, Jariani, Toor, Gurpal S.
Format: Article
Published: Elsevier 2018
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Online Access:http://eprints.um.edu.my/21754/
https://doi.org/10.1016/j.watres.2018.02.042
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spelling my.um.eprints.217542019-08-02T03:37:22Z http://eprints.um.edu.my/21754/ Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters Jani, Jariani Toor, Gurpal S. Q Science (General) QD Chemistry Nitrogen (N) transport from land to water is a dominant contributor of N in estuarine waters leading to eutrophication, harmful algal blooms, and hypoxia. Our objectives were to (1) investigate the composition of inorganic and organic N forms, (2) distinguish the sources and biogeochemical mechanisms of nitrate–N (NO3–N) transport using stable isotopes of NO3 − and Bayesian mixing model, and (3) determine the dissolved organic N (DON) bioavailability using bioassays in a longitudinal gradient from freshwater to estuarine ecosystem located in the Tampa Bay, Florida, United States. We found that DON was the most dominant N form (mean: 64%, range: 46–83%) followed by particulate organic N (PON, mean: 22%, range: 14–37%), whereas inorganic N forms (NOx–N: 7%, NH4–N: 7%) were 14% of total N in freshwater and estuarine waters. Stable isotope data of NO3 − revealed that nitrification was the main contributor (36.4%), followed by soil and organic N sources (25.5%), NO3 − fertilizers (22.4%), and NH4 + fertilizers (15.7%). Bioassays showed that 14 to 65% of DON concentrations decreased after 5-days of incubation indicating utilization of DON by microbes in freshwater and estuarine waters. These results suggest that despite low proportion of inorganic N forms, the higher concentrations and bioavailability of DON can be a potential source of N for algae and bacteria leading to water quality degradation in the estuarine waters. Elsevier 2018 Article PeerReviewed Jani, Jariani and Toor, Gurpal S. (2018) Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters. Water Research, 137. pp. 344-354. ISSN 0043-1354 https://doi.org/10.1016/j.watres.2018.02.042 doi:10.1016/j.watres.2018.02.042
institution Universiti Malaya
building UM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaya
content_source UM Research Repository
url_provider http://eprints.um.edu.my/
topic Q Science (General)
QD Chemistry
spellingShingle Q Science (General)
QD Chemistry
Jani, Jariani
Toor, Gurpal S.
Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters
description Nitrogen (N) transport from land to water is a dominant contributor of N in estuarine waters leading to eutrophication, harmful algal blooms, and hypoxia. Our objectives were to (1) investigate the composition of inorganic and organic N forms, (2) distinguish the sources and biogeochemical mechanisms of nitrate–N (NO3–N) transport using stable isotopes of NO3 − and Bayesian mixing model, and (3) determine the dissolved organic N (DON) bioavailability using bioassays in a longitudinal gradient from freshwater to estuarine ecosystem located in the Tampa Bay, Florida, United States. We found that DON was the most dominant N form (mean: 64%, range: 46–83%) followed by particulate organic N (PON, mean: 22%, range: 14–37%), whereas inorganic N forms (NOx–N: 7%, NH4–N: 7%) were 14% of total N in freshwater and estuarine waters. Stable isotope data of NO3 − revealed that nitrification was the main contributor (36.4%), followed by soil and organic N sources (25.5%), NO3 − fertilizers (22.4%), and NH4 + fertilizers (15.7%). Bioassays showed that 14 to 65% of DON concentrations decreased after 5-days of incubation indicating utilization of DON by microbes in freshwater and estuarine waters. These results suggest that despite low proportion of inorganic N forms, the higher concentrations and bioavailability of DON can be a potential source of N for algae and bacteria leading to water quality degradation in the estuarine waters.
format Article
author Jani, Jariani
Toor, Gurpal S.
author_facet Jani, Jariani
Toor, Gurpal S.
author_sort Jani, Jariani
title Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters
title_short Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters
title_full Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters
title_fullStr Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters
title_full_unstemmed Composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters
title_sort composition, sources, and bioavailability of nitrogen in a longitudinal gradient from freshwater to estuarine waters
publisher Elsevier
publishDate 2018
url http://eprints.um.edu.my/21754/
https://doi.org/10.1016/j.watres.2018.02.042
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