nerc.ac.uk

The influence of flow and bed slope on gas transfer in steep streams and their implications for evasion of CO2

Maurice, L.; Rawlins, B.G.; Farr, G.; Bell, R.; Gooddy, D.C.. 2017 The influence of flow and bed slope on gas transfer in steep streams and their implications for evasion of CO2. Journal of Geophysical Research: Biogeosciences. 27, pp. 10.1002/2017JG004045

Before downloading, please read NORA policies.
[img] Text
Maurice et al 2017 gas transfer paper for NORA_V2.pdf - Accepted Version
Restricted to NERC registered users only until 22 March 2018.

Download (1MB) | Request a copy

Abstract/Summary

The evasion of greenhouse gases (including CO2, CH4 and N2O) from streams and rivers to the atmosphere is an important process in global biogeochemical cycles, but our understanding of gas transfer in steep (> 10%) streams, and under varying flows is limited. We investigated gas transfer using combined tracer injections of SF6 and salt. We used a novel experimental design in which we compared four very steep (18.4-29.4%) and four moderately steep (3.7-7.6%) streams, and conducted tests in each stream under low flow conditions and during a high discharge event. Most dissolved gas evaded over short distances (~100 and ~200-400 m respectively), so accurate estimates of evasion fluxes will require sampling of dissolved gases at these scales to account for local sources. We calculated CO2 gas transfer coefficients (KCO2) and found statistically significant differences between larger KCO2 values for steeper (mean 0.465 min-1) streams compared to those with shallower slopes (mean 0.109 min-1). Variations in flow had an even greater influence. KCO2 was substantially larger under high (mean 0.497 min-1) compared to low flow conditions (mean 0.077 min-1). We developed a statistical model to predict KCO2 using values of streambed slope x discharge which accounted for 94 % of the variation. We show that two models using slope and velocity developed by Raymond et al. [2012] for streams and rivers with shallower slopes, also provide reasonable estimates of our CO2 gas transfer velocities (kCO2; m d-1). We developed a robust field protocol which could be applied in future studies.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1002/2017JG004045
Additional Keywords: GroundwaterBGS, Groundwater, Surface water interaction, Catchment processes, Climate change
Date made live: 26 Oct 2017 13:53 +0 (UTC)
URI: http://nora.nerc.ac.uk/id/eprint/517989

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...