Methane exchange with the atmosphere was measured during three seasons at the Rooney Road landfill in Jefferson County, CO. Substantial spatial and temporal variability in exchange rates were observed. Mean fluxes to the atmosphere were 534, 1290, and 538 mg CH 4 /m 2 /day, respectively, in the fall of 1994, winter of 1994-1995, and summer of 1995. Median fluxes were 12.42, 8.62, and 5.65 mg CH 4 /m 2 /day, respectively, during those seasons. Forty-three of 177 measurements had small negative fluxes, suggesting methanotrophic activity in the landfill cover soils. Despite probable methanotrophic activity in cover soils, landfills without gas collection systems may emit substantial CH 4 to the atmosphere, with large spatial and seasonal variability.
INTRODUCTIONLandfills have been cited as a major anthropogenic source of CH 4 in the atmosphere. [1][2][3][4] As such, landfills contributed a portion of the total increase in the atmospheric concentration of CH 4 by nearly 1% per year for the period of 1984-1992, but this rate of increase has subsequently slowed.5 Municipal solid waste (MSW) landfills have an estimated source strength of 20-60 Tg CH 4 /yr.