We quantified rates of soil respiration among sites within an agricultural
landscape in central Iowa, USA. The study was conducted in riparian cool-se
ason grass buffers, in re-established multispecies (switchgrass + poplar) r
iparian buffers and in adjacent crop (maize and soybean) fields. The object
ives were to determine the variability in soil respiration among buffer typ
es and crop fields within a riparian landscape, and to identify those facto
rs correlating with the observed differences. Soil respiration was measured
approximately monthly over a two-year period using the soda-lime technique
. Mean daily soil respiration across all treatments ranged from 0.14 to 8.3
g C m(-2) d(-1). There were no significant differences between cool-season
grass buffers and re-established forest buffers, but respiration rates ben
eath switchgrass were significantly lower than those beneath cool-season gr
ass. Soil respiration was significantly greater in both buffer systems than
in the cropped fields. Seasonal changes in soil respiration were strongly
related to temperature changes. Over all sites, soil temperature and soil m
oisture together accounted for 69% of the seasonal variability in soil resp
iration. Annual soil respiration rates correlated strongly with soil organi
c carbon (R = 0.75, P < 0.001) and fine root (<2 mm) biomass (R = 0.85, P <
0.001). Annual soil respiration rates averaged 1140 g C m(-2) for poplar,
1185 g C m(-2) for cool-season grass, 1020 g C m(-2) for switchgrass, 750 g
C m(-2) for soybean and 740 g C m(-2) for corn. Overall, vegetated buffers
had significantly higher soil respiration rates than did adjacent crop fie
lds, indicating greater soil biological activity within the buffers.