The vertical profiles of methane and oxygen concentrations were measur
ed in the cover soil at four sites in a restored and covered landfill.
At sites 2 and 3 within the landfill area methane was detectable even
to the soil surface and emission of methane occurred at these two sit
es. Measured methane emission rates varied seasonally and appeared to
be most influenced by soil water content. On an annual basis methane e
missions at these two sites were 495 and 909 mol methane m-2 y-1, resp
ectively. At sites 1 and 4 methane was detected in the cover soil but
was not present in the immediate subsurface layer, and emission of met
hane did not occur. Oxidation of methane by bacteria within the soil p
rofile at these two sites appeared to prevent methane emission from th
e surface.A methane-oxidising microflora had been enriched in the soil
s of all four landfill sites, as shown by counts of methanotrophs and
methylotrophs which were greater than in controls of garden soil not s
ubjected to elevated methane. Counts of methanotrophs and methylotroph
s were generally higher in those soil strata where methane concentrati
ons were greatest. Methane oxidation rates were maximum at soil depths
where gradients of methane and oxygen overlapped, usually 10-30 cm de
pth. The depth integrated rates of methane oxidation were very high at
sites 2 and 3, the sites also where methane was emitted from the soil
surface. A maximum oxidation rate of 450 mmol CH4 m-2 d-1 was measure
d at site 3. The data suggested that the microflora in the soil above
landfill adapted to the presence of elevated methane concentrations by
selection of a more methanotrophic community which was able to rapidl
y oxidise methane. Optimisation of microbial oxidation of methane by b
acteria in landfill cover soil may provide a cheap management strategy
to minimise the emissions of methane to the atmosphere from landfill.