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Conference Paper: Nitrogen isotopes in a complex urbanized marine environment

TitleNitrogen isotopes in a complex urbanized marine environment
Authors
Issue Date2019
PublisherState Key Lab of Marine Environmental Science (MEL), Xiamen University.
Citation
The 4th Xiamen Symposium on Marine Environmental Sciences (XMAS-IV): The Changing Ocean Environment: From a Multidisciplinary Perspective, Xiamen, China, 6-9 January 2019 How to Cite?
AbstractElevated nutrient inputs have led to increased eutrophication in coastal marine ecosystems worldwide. An understanding of the relative contribution of different nutrient sources is imperative for effective water quality management. Stable isotope values of nitrate (δ15NNO3-, δ18ONO3-) can complement conventional water quality monitoring programs to help differentiate natural sources of NO3- from anthropogenic inputs and estimate the processes involved in N cycling within an ecosystem. We measured nutrient concentrations, δ15NNO3-, and δ18ONO3- in 76 locations along a salinity gradient from the lower end of the Pearl River Estuary, one of China's largest rivers discharging into the South China Sea, towards the open ocean. NO3- concentrations decreased with increasing salinity, indicative of conservative mixing of eutrophic freshwater and oligotrophic seawater. However, our data did not follow conservative mixing patterns. At salinities <20 psu, samples exhibited decreasing NO3-concentrations with almost unchanged NO3- isotope values, indicating simple dilution. At salinities >20psu, NO3- concentrations decreased, while dual NO3- isotopes increased, suggesting mixing and/or other transformation processes. Our analysis yielded mean estimates for isotope enrichment factors (15ε = -2.02‰ and 18ε = -3.37‰, Δ(15,18)=-5.5‰ and δ15NNO3- - δ15NNO2- = 12.3‰. After consideration of potential alternative sources (sewage, atmospheric deposition and groundwater) we concluded that there are three plausible interpretations for deviations from conservative mixing behaviour (1) NO3- uptake by assimilation (2) in situ NO3- production (from fixation-derived nitrogen and nitrification of sewage-derived effluents) and (3) input of groundwater nitrate carrying a denitrification signal. Through this study, we propose a simple workflow that incorporates a synthesis of numerous isotope-based studies to constrain sources and behaviour of NO3- in urbanized marine environments.
DescriptionSpecial poster session: Ocean Circulation, Ecosystem and Hypoxia around Hong Kong Waters - no. P-SPS4-04
Organizer: The State Key Lab of Marine Environmental Science (MEL), Xiamen University
Persistent Identifierhttp://hdl.handle.net/10722/271147

 

DC FieldValueLanguage
dc.contributor.authorAnand, A-
dc.contributor.authorThibodeau, B-
dc.contributor.authorGeeraert, NAA-
dc.contributor.authorBaker, DM-
dc.date.accessioned2019-06-24T01:04:14Z-
dc.date.available2019-06-24T01:04:14Z-
dc.date.issued2019-
dc.identifier.citationThe 4th Xiamen Symposium on Marine Environmental Sciences (XMAS-IV): The Changing Ocean Environment: From a Multidisciplinary Perspective, Xiamen, China, 6-9 January 2019-
dc.identifier.urihttp://hdl.handle.net/10722/271147-
dc.descriptionSpecial poster session: Ocean Circulation, Ecosystem and Hypoxia around Hong Kong Waters - no. P-SPS4-04-
dc.descriptionOrganizer: The State Key Lab of Marine Environmental Science (MEL), Xiamen University-
dc.description.abstractElevated nutrient inputs have led to increased eutrophication in coastal marine ecosystems worldwide. An understanding of the relative contribution of different nutrient sources is imperative for effective water quality management. Stable isotope values of nitrate (δ15NNO3-, δ18ONO3-) can complement conventional water quality monitoring programs to help differentiate natural sources of NO3- from anthropogenic inputs and estimate the processes involved in N cycling within an ecosystem. We measured nutrient concentrations, δ15NNO3-, and δ18ONO3- in 76 locations along a salinity gradient from the lower end of the Pearl River Estuary, one of China's largest rivers discharging into the South China Sea, towards the open ocean. NO3- concentrations decreased with increasing salinity, indicative of conservative mixing of eutrophic freshwater and oligotrophic seawater. However, our data did not follow conservative mixing patterns. At salinities <20 psu, samples exhibited decreasing NO3-concentrations with almost unchanged NO3- isotope values, indicating simple dilution. At salinities >20psu, NO3- concentrations decreased, while dual NO3- isotopes increased, suggesting mixing and/or other transformation processes. Our analysis yielded mean estimates for isotope enrichment factors (15ε = -2.02‰ and 18ε = -3.37‰, Δ(15,18)=-5.5‰ and δ15NNO3- - δ15NNO2- = 12.3‰. After consideration of potential alternative sources (sewage, atmospheric deposition and groundwater) we concluded that there are three plausible interpretations for deviations from conservative mixing behaviour (1) NO3- uptake by assimilation (2) in situ NO3- production (from fixation-derived nitrogen and nitrification of sewage-derived effluents) and (3) input of groundwater nitrate carrying a denitrification signal. Through this study, we propose a simple workflow that incorporates a synthesis of numerous isotope-based studies to constrain sources and behaviour of NO3- in urbanized marine environments.-
dc.languageeng-
dc.publisherState Key Lab of Marine Environmental Science (MEL), Xiamen University.-
dc.relation.ispartofFourth Xiamen Symposium on Marine Environmental Sciences (XMAS-IV)-
dc.titleNitrogen isotopes in a complex urbanized marine environment-
dc.typeConference_Paper-
dc.identifier.emailThibodeau, B: bthib@hku.hk-
dc.identifier.emailGeeraert, NAA: geeraert@hku.hk-
dc.identifier.emailBaker, DM: dmbaker@hku.hk-
dc.identifier.authorityThibodeau, B=rp02033-
dc.identifier.authorityBaker, DM=rp01712-
dc.identifier.hkuros298030-
dc.publisher.placeChina-

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