Variations in dissolved CO2 and CH4 in a first-order stream and catchment: an investigation of soil-stream linkages

• Published in: Hydrological processes Vol. 18; no. 17; pp. 3255 - 3275
• Main Authors: Hope, Diane, Palmer, Sheila M., Billett, Michael F., Dawson, Julian J. C.
• Format: Journal Article
• Language: English
• Published: Chichester, UK John Wiley & Sons, Ltd 15.12.2004; Wiley
• Subjects: autoregression modelling; Brocky Burn; dissolved CO2; downstream changes; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Hydrology; Hydrology. Hydrogeology; land-atmosphere C exchange; Marine and continental quaternary; Pollution, environment geology; soil atmosphere; soil-respired inputs; stream flow; Surficial geology; United Kingdom; Scotland; Great Britain; Western Europe; atmosphere; soil atmosphere; dissolved CO2; atmospheric emission; stream order; respiration; air; soil-respired inputs; stream flow; saturation; drainage basins; hydrochemistry; peat bogs; temperature; autoregression modelling; dissolved materials; spatial variations; soils; peat; correlation coefficient; Brocky Burn; carbon dioxide; models; Europe; streams; sampling; concentration; land-atmosphere C exchange; methane; autoregression; seasonal variations; downstream changes
• ISSN: 0885-6087; 1099-1085
• DOI: 10.1002/hyp.5657

Spatial and seasonal variations in CO2 and CH4 concentrations in streamwater and adjacent soils were studied at three sites on Brocky Burn, a headwater stream draining a peatland catchment in upland Britain. Concentrations of both gases in the soil atmosphere were significantly higher in peat and riparian soils than in mineral soils. Peat and riparian soil CO2 concentrations varied seasonally, showing a positive correlation with air and soil temperature. Streamwater CO2 concentrations at the upper sampling site, which mostly drained deep peats, varied from 2·8 to 9·8 mg l−1 (2·5 to 11·9 times atmospheric saturation) and decreased markedly downstream. Temperature‐related seasonal variations in peat and riparian soil CO2 were reflected in the stream at the upper site, where 77% of biweekly variation was explained by an autoregressive model based on: (i) a negative log‐linear relationship with stream flow; (ii) a positive linear relationship with soil CO2 concentrations in the shallow riparian wells; and (iii) a negative linear relationship with soil CO2 concentrations in the shallow peat wells, with a significant 2‐week lag term. These relationships changed markedly downstream, with an apparent decrease in the soil–stream linkage and a switch to a positive relationship between stream flow and stream CO2. Streamwater CH4 concentrations also declined sharply downstream, but were much lower (<0·01 to 0·12 mg l−1) than those of CO2 and showed no seasonal variation, nor any relationship with soil atmospheric CH4 concentrations. However, stream CH4 was significantly correlated with stream flow at the upper site, which explained 57% of biweekly variations in dissolved concentrations. We conclude that stream CO2 can be a useful integrative measure of whole catchment respiration, but only at sites where the soil–stream linkage is strong. Copyright © 2004 John Wiley & Sons, Ltd.