SOIL-MOISTURE AS A PREDICTOR OF METHANE UPTAKE BY TEMPERATE FOREST SOILS

We conducted soil moisture manipulation experiments in a red pine (Pin us resinosa Ait.) plantation at the Harvard Forest (Petersham, Mass.) in August 1992 and May 1993. To manipulate soil moisture, we added 10 cm of groundwater to 1-m(2) plots and allowed the soils to dry down to their pretreatment moisture contents. We measured methane (CH4) flux, soil moisture, and temperature prior to and after the water addition. Soils in both the control and watered plots were usually sinks for at mospheric CH4. Average consumption rates by control soils ranged from 0.12 to 0.17 mg CH4-C.m(-2) h(-1). Methane consumption rates by watere d soils ranged from 0 to 0.12 mg CH4-C m(-2)h(-1) and were inversely r elated to the moisture content of the upper 10 cm of mineral soil. Lin ear regression between soil moisture and CH4 consumption explained 78% of the variability (CH4 consumption = 0.001 75 (percent water filled pore space) - 0.1957). Using this empirical relationship, we predicted CH4 consumption by soils at three other locations in the Harvard Fore st, which agreed closely (r(2) = 0.7574) with rates measured in the sp ring, summer, and fall of 1988-1992. Results from our study suggest th at soil moisture is a good predictor of methane uptake by these forest soils and may be used to predict how future changes in soil moisture resulting from alterations in regional precipitation patterns will aff ect the strength of this terrestrial CH4 sink.