Temporal variations in greenhouse gas emissions at a midlatitude landfill

A field study encompassing a parallel time series of CH4, N2O, and CO2 emis sions measurements was completed by using static enclosure techniques at a midlatitude landfill (northeastern Illinois) during the period of July thro ugh December 1995. The site had a pumped gas recovery system and thus a hig h level of engineered gas control. No net CH4 emissions to the atmosphere w ere measured during this study; rather, the landfill cover soils were funct ioning as a sink for atmospheric CH4. The net measured emissions of CO2 (da rk respiration) and N2O were in ranges characteristic of natural soils and were dependent on similar controls, including temperature, moisture, and ae ration status. A comparison of proximal (near gas recovery well) and distal (between wells) emissions with soil gas profiles permitted development of a conceptual biogeochemical model for gas transport and reaction through th e landfill cover. This model includes a modified reduction sequence where t he major zones (from ground surface downward) were a near-surface zone of o ptimum CH4 oxidation; a zone of optimum CO2 production (predominantly from root zone respiration); a zone of optimum N2O production; and a deep zone d ominated by transport of landfill gas (CH4 and CO2) from methanogenic produ ction zones in the underlying refuse.