Headwater gas exchange quantified from O-2 mass balances at the reach scale

Show full item record



Permalink

http://hdl.handle.net/10138/256033

Citation

Rovelli , L , Attard , K M , Heppell , C M , Binley , A , Trimmer , M & Glud , R N 2018 , ' Headwater gas exchange quantified from O-2 mass balances at the reach scale ' , Limnology and Oceanography: Methods , vol. 16 , no. 10 , pp. 696-709 . https://doi.org/10.1002/lom3.10281

Title: Headwater gas exchange quantified from O-2 mass balances at the reach scale
Author: Rovelli, L.; Attard, K. M.; Heppell, C. M.; Binley, A.; Trimmer, M.; Glud, R. N.
Contributor: University of Helsinki, Ecosystems and Environment Research Programme
Date: 2018-10
Language: eng
Number of pages: 14
Belongs to series: Limnology and Oceanography: Methods
ISSN: 1541-5856
URI: http://hdl.handle.net/10138/256033
Abstract: Headwater streams are important in the carbon cycle and there is a need to better parametrize and quantify exchange of carbon-relevant gases. Thus, we characterized variability in the gas exchange coefficient (k(2)) and dissolved oxygen (O-2) gas transfer velocity (k) in two lowland headwaters of the River Avon (UK). The traditional one-station open-water method was complemented by in situ quantification of riverine sources and sinks of O-2 (i.e., groundwater inflow, photosynthesis, and respiration in both the water column and benthic compartment) enabling direct hourly estimates of k(2) at the reach-scale (similar to 150 m) without relying on the nighttime regression method. Obtained k(2) values ranged from 0.001 h(-1) to 0.600 h(-1). Average daytime k(2) were a factor two higher than values at night, likely due to diel changes in water temperature and wind. Temperature contributed up to 46% of the variability in k on an hourly scale, but clustering temperature incrementally strengthened the statistical relationship. Our analysis suggested that k variability is aligned with dominant temperature trends rather than with short-term changes. Similarly, wind correlation with k increased when clustering wind speeds in increments correspondent with dominant variations (1 m s(-1)). Time scale is thus an important consideration when resolving physical drivers of gas exchange. Mean estimates of k(600) from recent parametrizations proposed for upscaling, when applied to the settings of this study, were found to be in agreement with our independent O-2 budget assessment (within <10%), adding further support to the validity of upscaling efforts aiming at quantifying large-scale riverine gas emissions.
Subject: WHOLE-STREAM METABOLISM
AQUATIC EDDY-CORRELATION
DISSOLVED-OXYGEN
REAERATION RATES
ATMOSPHERIC REAERATION
TEMPERATURE-DEPENDENCE
CARBON-DIOXIDE
INLAND WATERS
DELTA METHOD
WIND-SPEED
1172 Environmental sciences
Rights:


Files in this item

Total number of downloads: Loading...

Files Size Format View
Rovelli_et_al_2 ... ceanography_3A_Methods.pdf 533.8Kb PDF View/Open

This item appears in the following Collection(s)

Show full item record