Abstract. Nitrous oxide (N2O) and methane (CH4) are atmospheric trace gases
which play important roles in the climate and atmospheric chemistry of the
Earth. However, little is known about their emissions from rivers and
estuaries, which seem to contribute significantly to the atmospheric budget
of both gases. To this end concentrations of N2O and CH4 were
measured in the Rajang, Maludam, Sebuyau and Simunjan rivers draining
peatland in northwestern (NW) Borneo during two campaigns in March and
September 2017. The Rajang River was additionally sampled in August 2016 and
the Samunsam and Sematan rivers were additionally sampled in March 2017. The
Maludam, Sebuyau, and Simunjan rivers are typical “blackwater” rivers with
very low pH (3.7–7.8), very high dissolved organic carbon (DOC)
concentrations (235–4387 mmol L−1) and very low O2
concentrations (31–246 µmol L−1; i.e. 13 %–116 % O2
saturation). The spatial and temporal variability of N2O and CH4
concentrations (saturations) in the six rivers or estuaries was large and
ranged from 2.0 nmol L−1 (28 %) to 41.4 nmol L−1 (570 %) and
from 2.5 nmol L−1 (106 %) to 1372 nmol L−1 (57 459 %),
respectively. We found no overall trends of N2O with O2 or
NO3-, NO2- or NH4+, and there were no trends of
CH4 with O2 or dissolved nutrients or DOC. N2O concentrations
showed a positive linear correlation with rainfall. We conclude, therefore,
that rainfall is the main factor determining the riverine N2O
concentrations since N2O production or consumption in the blackwater rivers themselves seems to be low because of the low pH. CH4
concentrations were highest at salinity = 0 and most probably result from
methanogenesis as part of the decomposition of organic matter under anoxic
conditions. CH4 in the concentrations in the blackwater rivers showed
an inverse relationship with rainfall. We suggest that CH4 oxidation in
combination with an enhanced river flow after the rainfall events might be
responsible for the decrease in the CH4 concentrations. The rivers and
estuaries studied here were an overall net source of N2O and CH4
to the atmosphere. The total annual N2O and CH4 emissions were
1.09 Gg N2O yr−1 (0.7 Gg N yr−1) and 23.8 Gg CH4 yr−1, respectively. This represents about 0.3 %–0.7 % of the global
annual riverine and estuarine N2O emissions and about 0.1 %–1 % of
the global riverine and estuarine CH4 emissions. Therefore, we conclude
that rivers and estuaries in NW Borneo – despite the fact their water area
covers only 0.05 % of the global river/estuarine area – contribute
significantly to global riverine and estuarine emissions of N2O and
CH4.