期刊
BIOGEOCHEMISTRY
卷 89, 期 3, 页码 367-377出版社
SPRINGER
DOI: 10.1007/s10533-008-9225-4
关键词
denitrification; ebullition; nitrogen; bubbles; South Platte River
资金
- Teagasc Ireland
Rates of ebullition and composition of bubbles were measured along a nutrient-enriched segment of the South Platte River below Denver, Colorado. Ebullition was widespread in the South Platte up to 81 km downstream from Denver. Ebullitive fluxes of 0.44 and 0.29 g N m(-2) d(-1) were recorded at two sites downstream of Denver and represented 6-16% of the diffusive N-2 efflux from this region. These data indicate that not accounting for ebullitive N-2 losses can, at some locations, lead to a considerable underestimation of dentrification rates using the open-channel (gas exchange) method. Gas bubbles often were > 98% N-2; methane dominated in a few organic-rich areas. Rates of ebullition related significantly to variations in temperature and dissolved organic carbon. Ebullition was not observed in four tributaries of the South Platte River, despite their moderate to high concentrations of nitrate and dissolved organic carbon. The data demonstrate that ebullition can contribute significantly to N-2 effluxes in running waters exhibiting high rates of denitrification.
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