Static floating chamber (FC) measurements of CH₄ and CO₂ fluxes from northern boreal river Kitinen
were analyzed for this thesis. Measurements were carried out in summer 2018. Spatiotemporal variability
was measured in the fluxes by comparing three chamber measuring locations: the opposite river banks and
the middle of the river. Mean CO₂ flux estimate was 0.83±0.54 μmol CO₂ m⁻² s⁻¹ (mean ± SD, n = 73),
consistent with other estimates for similar systems, with a corresponding k₆₀₀ CO₂ gas transfer velocity
estimate of 17±9 cm h⁻¹ . Nonlinear modelling of CO₂ flux was found useful for analyzing floating chamber
data from a river. The mean CH₄ flux was 0.0084±0.0047 μmol CH₄ m⁻² s⁻¹ , slightly lower than the
median for different river systems in literature. The flux estimates were compared with eddy covariance
measurements (EC). FC measurements are expected to give larger results, but additionally chambers are
known to overestimate fluxes in flowing water. The comparison yielded chamber fluxes 3.3 and 2.9 times
the EC median values for CO₂ and CH₄ respectively.
Fluxes were similar between the three locations, and they peaked in late July for both gases in all loca-
tions. Some differences over the river cross-section were observed. Discharge was significantly correlated to
fluxes in the middle of the river, which could be explained by inhomogeneous flow. On two measuring days
in early August, the mid-river CO₂ fluxes were three times those observed near the banks. The difference
was also measured in methane. No clear cause was determined, but measuring spatial variation in surface
water gas concentrations and flow could clarify the causes of similar observations in further studies.
