Abstract
Spatial and seasonal variations in CO~2~ and CH~4~ 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 CO~2~ concentrations varied seasonally, showing a positive correlation with air and soil temperature. Streamwater CO~2~ 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 CO~2~ 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 CO~2~ concentrations in the shallow riparian wells; and (iii) a negative linear relationship with soil CO~2~ 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 CO~2~. Streamwater CH~4~ concentrations also declined sharply downstream, but were much lower (<0·01 to 0·12 mg l^−1^) than those of CO~2~ and showed no seasonal variation, nor any relationship with soil atmospheric CH~4~ concentrations. However, stream CH~4~ was significantly correlated with stream flow at the upper site, which explained 57% of biweekly variations in dissolved concentrations. We conclude that stream CO~2~ 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.