Dynamics of nitrous oxide with depth in groundwater: Insights from ambient groundwater and laboratory incubation experiments (Hesbaye chalk aquifer, Belgium)

Aquifers under agricultural areas are considered to be an indirect source of nitrous oxide emission (N2O) to the atmosphere, which is the greenhouse gas (GHGs) characterized with the highest global warning potential and acts as a stratospheric ozone depletion agent. Previous investigations performed in the Cretaceous Hesbaye chalk aquifer in Eastern Belgium suggested that the dynamics of N2O in the aquifer is controlled by overlapping biochemical processes such as nitrification and denitrification. The current study aims to obtain better insight concerning the factors controlling the distribution of N2O concentration along a vertical dimension in the aquifer, and to capture and quantify the occurrence of nitrification and denitrification processes in the groundwater system. Low-flow groundwater sampling technique was undertaken at different depths in the aquifer to collect groundwater samples aiming at obtaining information about ambient aquifer hydrogeochemical conditions and their effect on the accumulation of GHGs. Afterwards, laboratory stable isotope experiments, using NO3- and NH4+ compounds labeled with heavy 15N isotope, were applied to quantify the rates of nitrification and denitrification processes. Ambient studies suggest that the occurrence of N transformation was related to denitrification while laboratory incubation experiments did not detect it. Such controversial results might be explained by the discrepancy between real aquifer conditions and lab design studies. Thus, additional in situ tracer experiments should be carried out in areas where natural groundwater fluxes do not flush the injected tracer too rapidly. In addition, it would be useful to conduct microbiological studies to obtain better insight into the nature of subsurface biofilm biotope.

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Main Authors: Nikolenko, Olha, Brouyѐre, Serge, Goderniaux, Pascal, Robert, Tanguy, Orban, Philippe, Borges, Alberto V, Jurado, Anna, Duvivier, Maxime, Morana, Cedric
Other Authors: European Commission
Format: artículo biblioteca
Language:English
Published: Elsevier 2021-08
Subjects:Nitrification, Denitrification, Greenhouse gases, Groundwater, Low-flow sampling, N stable isotope analysis,
Online Access:http://hdl.handle.net/10261/265181
http://dx.doi.org/10.13039/501100000780
https://api.elsevier.com/content/abstract/scopus_id/85104151151
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spelling dig-idaea-es-10261-2651812024-05-13T20:37:02Z Dynamics of nitrous oxide with depth in groundwater: Insights from ambient groundwater and laboratory incubation experiments (Hesbaye chalk aquifer, Belgium) Nikolenko, Olha Brouyѐre, Serge Goderniaux, Pascal Robert, Tanguy Orban, Philippe Borges, Alberto V Jurado, Anna Duvivier, Maxime Morana, Cedric European Commission Nitrification Denitrification Greenhouse gases Groundwater Low-flow sampling N stable isotope analysis Aquifers under agricultural areas are considered to be an indirect source of nitrous oxide emission (N2O) to the atmosphere, which is the greenhouse gas (GHGs) characterized with the highest global warning potential and acts as a stratospheric ozone depletion agent. Previous investigations performed in the Cretaceous Hesbaye chalk aquifer in Eastern Belgium suggested that the dynamics of N2O in the aquifer is controlled by overlapping biochemical processes such as nitrification and denitrification. The current study aims to obtain better insight concerning the factors controlling the distribution of N2O concentration along a vertical dimension in the aquifer, and to capture and quantify the occurrence of nitrification and denitrification processes in the groundwater system. Low-flow groundwater sampling technique was undertaken at different depths in the aquifer to collect groundwater samples aiming at obtaining information about ambient aquifer hydrogeochemical conditions and their effect on the accumulation of GHGs. Afterwards, laboratory stable isotope experiments, using NO3- and NH4+ compounds labeled with heavy 15N isotope, were applied to quantify the rates of nitrification and denitrification processes. Ambient studies suggest that the occurrence of N transformation was related to denitrification while laboratory incubation experiments did not detect it. Such controversial results might be explained by the discrepancy between real aquifer conditions and lab design studies. Thus, additional in situ tracer experiments should be carried out in areas where natural groundwater fluxes do not flush the injected tracer too rapidly. In addition, it would be useful to conduct microbiological studies to obtain better insight into the nature of subsurface biofilm biotope. This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No 675120. Los Gatos Research OA-ICOS was funded by the Fonds National de la Rechecherche Scientifique (FNRS) (22547486). AVB is a Research Director at the FNRS. Peer reviewed 2022-03-24T10:35:32Z 2022-03-24T10:35:32Z 2021-08 artículo http://purl.org/coar/resource_type/c_6501 Journal of Contaminant Hydrology 241: 103797 (2021) 01697722 http://hdl.handle.net/10261/265181 10.1016/j.jconhyd.2021.103797 http://dx.doi.org/10.13039/501100000780 33813144 2-s2.0-85104151151 https://api.elsevier.com/content/abstract/scopus_id/85104151151 en #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/H2020/675120. Journal of contaminant hydrology Postprint https://doi.org/10.1016/j.jconhyd.2021.103797 Sí open Elsevier
institution IDAEA ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-idaea-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IDAEA España
language English
topic Nitrification
Denitrification
Greenhouse gases
Groundwater
Low-flow sampling
N stable isotope analysis
Nitrification
Denitrification
Greenhouse gases
Groundwater
Low-flow sampling
N stable isotope analysis
spellingShingle Nitrification
Denitrification
Greenhouse gases
Groundwater
Low-flow sampling
N stable isotope analysis
Nitrification
Denitrification
Greenhouse gases
Groundwater
Low-flow sampling
N stable isotope analysis
Nikolenko, Olha
Brouyѐre, Serge
Goderniaux, Pascal
Robert, Tanguy
Orban, Philippe
Borges, Alberto V
Jurado, Anna
Duvivier, Maxime
Morana, Cedric
Dynamics of nitrous oxide with depth in groundwater: Insights from ambient groundwater and laboratory incubation experiments (Hesbaye chalk aquifer, Belgium)
description Aquifers under agricultural areas are considered to be an indirect source of nitrous oxide emission (N2O) to the atmosphere, which is the greenhouse gas (GHGs) characterized with the highest global warning potential and acts as a stratospheric ozone depletion agent. Previous investigations performed in the Cretaceous Hesbaye chalk aquifer in Eastern Belgium suggested that the dynamics of N2O in the aquifer is controlled by overlapping biochemical processes such as nitrification and denitrification. The current study aims to obtain better insight concerning the factors controlling the distribution of N2O concentration along a vertical dimension in the aquifer, and to capture and quantify the occurrence of nitrification and denitrification processes in the groundwater system. Low-flow groundwater sampling technique was undertaken at different depths in the aquifer to collect groundwater samples aiming at obtaining information about ambient aquifer hydrogeochemical conditions and their effect on the accumulation of GHGs. Afterwards, laboratory stable isotope experiments, using NO3- and NH4+ compounds labeled with heavy 15N isotope, were applied to quantify the rates of nitrification and denitrification processes. Ambient studies suggest that the occurrence of N transformation was related to denitrification while laboratory incubation experiments did not detect it. Such controversial results might be explained by the discrepancy between real aquifer conditions and lab design studies. Thus, additional in situ tracer experiments should be carried out in areas where natural groundwater fluxes do not flush the injected tracer too rapidly. In addition, it would be useful to conduct microbiological studies to obtain better insight into the nature of subsurface biofilm biotope.
author2 European Commission
author_facet European Commission
Nikolenko, Olha
Brouyѐre, Serge
Goderniaux, Pascal
Robert, Tanguy
Orban, Philippe
Borges, Alberto V
Jurado, Anna
Duvivier, Maxime
Morana, Cedric
format artículo
topic_facet Nitrification
Denitrification
Greenhouse gases
Groundwater
Low-flow sampling
N stable isotope analysis
author Nikolenko, Olha
Brouyѐre, Serge
Goderniaux, Pascal
Robert, Tanguy
Orban, Philippe
Borges, Alberto V
Jurado, Anna
Duvivier, Maxime
Morana, Cedric
author_sort Nikolenko, Olha
title Dynamics of nitrous oxide with depth in groundwater: Insights from ambient groundwater and laboratory incubation experiments (Hesbaye chalk aquifer, Belgium)
title_short Dynamics of nitrous oxide with depth in groundwater: Insights from ambient groundwater and laboratory incubation experiments (Hesbaye chalk aquifer, Belgium)
title_full Dynamics of nitrous oxide with depth in groundwater: Insights from ambient groundwater and laboratory incubation experiments (Hesbaye chalk aquifer, Belgium)
title_fullStr Dynamics of nitrous oxide with depth in groundwater: Insights from ambient groundwater and laboratory incubation experiments (Hesbaye chalk aquifer, Belgium)
title_full_unstemmed Dynamics of nitrous oxide with depth in groundwater: Insights from ambient groundwater and laboratory incubation experiments (Hesbaye chalk aquifer, Belgium)
title_sort dynamics of nitrous oxide with depth in groundwater: insights from ambient groundwater and laboratory incubation experiments (hesbaye chalk aquifer, belgium)
publisher Elsevier
publishDate 2021-08
url http://hdl.handle.net/10261/265181
http://dx.doi.org/10.13039/501100000780
https://api.elsevier.com/content/abstract/scopus_id/85104151151
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