A considerable fraction of the methane that is produced by landfills is oxidized by its covering soil before it can reach the atmosphere. This process was studied in soil columns that simulate landfill cover soil environments. The methane uptakewas followed as a function of time. In soils of agricultural origin, a maximum value of 10.7 mol m{sup}-2{sub}(column) d{sup}-1 was observed. Mixing sugar beet leaves with the soil led to a temporary stimulation of the methane oxidation rate, whereas awheat straw amendment led to permanent stimulation. Soil originating from a real landfill cover oxidized on the order of 15 mol m{sup}-2{sub}(column) d{sup}-1, the highest value found in the literature to date. The soil gas composition was studied as afunction of depth. With a new batch incubation technique, methane oxidation kinetics were determined in samples taken from the soil column. By combining this kinetic data with the soil gas composition data, the actively methane oxidizing zone in the soilcolumn could be determined and an in situ assessment of oxygen limitation could be performed. Methane oxidation takes place mainly in the top 30 cm of the covering soil.
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