Nitrous oxide and methane in two tropical estuaries in a peat-dominated region of northwestern Borneo

Estuaries are sources of nitrous oxide (N<sub>2</sub>O) and methane (CH<sub>4</sub>) to the atmosphere. However, our present knowledge of N<sub>2</sub>O and CH<sub>4</sub> emissions from estuaries in the tropics is very limited because data are scarce....

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Main Authors: D. Müller, H. W. Bange, T. Warneke, T. Rixen, M. Müller, A. Mujahid, J. Notholt
Format: Article
Language:English
Published: Copernicus Publications 2016-04-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/13/2415/2016/bg-13-2415-2016.pdf
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author D. Müller
H. W. Bange
T. Warneke
T. Rixen
M. Müller
A. Mujahid
J. Notholt
author_facet D. Müller
H. W. Bange
T. Warneke
T. Rixen
M. Müller
A. Mujahid
J. Notholt
author_sort D. Müller
collection DOAJ
description Estuaries are sources of nitrous oxide (N<sub>2</sub>O) and methane (CH<sub>4</sub>) to the atmosphere. However, our present knowledge of N<sub>2</sub>O and CH<sub>4</sub> emissions from estuaries in the tropics is very limited because data are scarce. In this study, we present first measurements of dissolved N<sub>2</sub>O and CH<sub>4</sub> from two estuaries in a peat-dominated region of northwestern Borneo. Two campaigns (during the dry season in June 2013 and during the wet season in March 2014) were conducted in the estuaries of the Lupar and Saribas rivers. Median N<sub>2</sub>O concentrations ranged between 7.2 and 12.3 nmol L<sup>−1</sup> and were higher in the marine end-member (13.0 ± 7.0 nmol L<sup>−1</sup>). CH<sub>4</sub> concentrations were low in the coastal ocean (3.6 ± 0.2 nmol L<sup>−1</sup>) and higher in the estuaries (medians between 10.6 and 64.0 nmol L<sup>−1</sup>). The respiration of abundant organic matter and presumably anthropogenic input caused slight eutrophication, which did not lead to hypoxia or enhanced N<sub>2</sub>O concentrations, however. Generally, N<sub>2</sub>O concentrations were not related to dissolved inorganic nitrogen concentrations. Thus, the use of an emission factor for the calculation of N<sub>2</sub>O emissions from the inorganic nitrogen load leads to an overestimation of the flux from the Lupar and Saribas estuaries. N<sub>2</sub>O was negatively correlated with salinity during the dry season, which suggests a riverine source. In contrast, N<sub>2</sub>O concentrations during the wet season were not correlated with salinity but locally enhanced within the estuaries, implying that there were additional estuarine sources during the wet (i.e., monsoon) season. Estuarine CH<sub>4</sub> distributions were not driven by freshwater input but rather by tidal variations. Both N<sub>2</sub>O and CH<sub>4</sub> concentrations were more variable during the wet season. We infer that the wet season dominates the variability of the N<sub>2</sub>O and CH<sub>4</sub> concentrations and subsequent emissions from tropical estuaries. Thus, we speculate that any changes in the Southeast Asian monsoon system will lead to changes in the N<sub>2</sub>O and CH<sub>4</sub> emissions from these systems. We also suggest that the ongoing cultivation of peat soil in Borneo is likely to increase N<sub>2</sub>O emissions from these estuaries, while the effect on CH<sub>4</sub> remains uncertain.
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spelling doaj.art-d1fe3e678485461e922e650ed8f10ec82022-12-21T18:26:27ZengCopernicus PublicationsBiogeosciences1726-41701726-41892016-04-011382415242810.5194/bg-13-2415-2016Nitrous oxide and methane in two tropical estuaries in a peat-dominated region of northwestern BorneoD. Müller0H. W. Bange1T. Warneke2T. Rixen3M. Müller4A. Mujahid5J. Notholt6Institute of Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, GermanyGEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker Weg 20, 24105 Kiel, GermanyInstitute of Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, GermanyLeibniz Center for Tropical Marine Ecology, Fahrenheitstr. 6, 28359 Bremen, GermanySwinburne University of Technology, Faculty of Engineering, Computing and Science, Jalan Simpang Tiga, 93350 Kuching, Sarawak, MalaysiaDepartment of Aquatic Science, Faculty of Resource Science & Technology, University Malaysia Sarawak, 94300 Kota Samarahan, Sarawak, MalaysiaInstitute of Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, GermanyEstuaries are sources of nitrous oxide (N<sub>2</sub>O) and methane (CH<sub>4</sub>) to the atmosphere. However, our present knowledge of N<sub>2</sub>O and CH<sub>4</sub> emissions from estuaries in the tropics is very limited because data are scarce. In this study, we present first measurements of dissolved N<sub>2</sub>O and CH<sub>4</sub> from two estuaries in a peat-dominated region of northwestern Borneo. Two campaigns (during the dry season in June 2013 and during the wet season in March 2014) were conducted in the estuaries of the Lupar and Saribas rivers. Median N<sub>2</sub>O concentrations ranged between 7.2 and 12.3 nmol L<sup>−1</sup> and were higher in the marine end-member (13.0 ± 7.0 nmol L<sup>−1</sup>). CH<sub>4</sub> concentrations were low in the coastal ocean (3.6 ± 0.2 nmol L<sup>−1</sup>) and higher in the estuaries (medians between 10.6 and 64.0 nmol L<sup>−1</sup>). The respiration of abundant organic matter and presumably anthropogenic input caused slight eutrophication, which did not lead to hypoxia or enhanced N<sub>2</sub>O concentrations, however. Generally, N<sub>2</sub>O concentrations were not related to dissolved inorganic nitrogen concentrations. Thus, the use of an emission factor for the calculation of N<sub>2</sub>O emissions from the inorganic nitrogen load leads to an overestimation of the flux from the Lupar and Saribas estuaries. N<sub>2</sub>O was negatively correlated with salinity during the dry season, which suggests a riverine source. In contrast, N<sub>2</sub>O concentrations during the wet season were not correlated with salinity but locally enhanced within the estuaries, implying that there were additional estuarine sources during the wet (i.e., monsoon) season. Estuarine CH<sub>4</sub> distributions were not driven by freshwater input but rather by tidal variations. Both N<sub>2</sub>O and CH<sub>4</sub> concentrations were more variable during the wet season. We infer that the wet season dominates the variability of the N<sub>2</sub>O and CH<sub>4</sub> concentrations and subsequent emissions from tropical estuaries. Thus, we speculate that any changes in the Southeast Asian monsoon system will lead to changes in the N<sub>2</sub>O and CH<sub>4</sub> emissions from these systems. We also suggest that the ongoing cultivation of peat soil in Borneo is likely to increase N<sub>2</sub>O emissions from these estuaries, while the effect on CH<sub>4</sub> remains uncertain.http://www.biogeosciences.net/13/2415/2016/bg-13-2415-2016.pdf
spellingShingle D. Müller
H. W. Bange
T. Warneke
T. Rixen
M. Müller
A. Mujahid
J. Notholt
Nitrous oxide and methane in two tropical estuaries in a peat-dominated region of northwestern Borneo
Biogeosciences
title Nitrous oxide and methane in two tropical estuaries in a peat-dominated region of northwestern Borneo
title_full Nitrous oxide and methane in two tropical estuaries in a peat-dominated region of northwestern Borneo
title_fullStr Nitrous oxide and methane in two tropical estuaries in a peat-dominated region of northwestern Borneo
title_full_unstemmed Nitrous oxide and methane in two tropical estuaries in a peat-dominated region of northwestern Borneo
title_short Nitrous oxide and methane in two tropical estuaries in a peat-dominated region of northwestern Borneo
title_sort nitrous oxide and methane in two tropical estuaries in a peat dominated region of northwestern borneo
url http://www.biogeosciences.net/13/2415/2016/bg-13-2415-2016.pdf
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