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Abstract
The effect of soil warming on CO
2 and CH
4 flux from a spruce-fir forest soil was evaluated at the Howland Integrated Forest Study site in Maine, USA from 1993 to 1995. Elevated soil temperatures (~5 °C) were maintained during the snow-free season (May-November) in replicated 15 × 15-m plots using electric cables buried 1-2 cm below the soil surface; replicated unheated plots served as the control. CO
2 evolution from the soil surface and soil air CO
2 concentrations both showed clear seasonal trends and significant (
P < 0.0001) positive exponential relationships with soil temperature. Soil warming caused a 25-40% increase in CO
2 flux from the heated plots compared to the controls. No significant differences were observed between heated and control plot soil air CO
2 concentrations which we attribute to rapid equilibration with the atmosphere in the O horizon and minimal treatment effects in the B horizon. Methand fluxes were highly variable and showed no consistent trends with treatment.
Citation
Rustad, Lindsey E.; Fernandez, Ivan J. 1998. Experimental soil warming effects on CO
2 and CH
4 flux from a low elevation spruce-fir forest soil in Maine, USA. Global Change Biology. 4(6): 597-605. https://doi.org/10.1046/j.1365-2486.1998.00169.x.