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Title: Gas pressure and concentration gradients at the top of a landfill

Conference ·
OSTI ID:6353714

Vertical gas pressure and concentration gradients are being investigated at the Mallard North Landfill (DuPage County, Illinois) using nests of probes installed in the top of refuse and at two depths in the clay cover materials. Soil gas pressures and atmospheric pressure are monitored continuously using electronic pressure transducers linked to a microcomputer. Concentrations of methane, carbon dioxide, nitrogen, and oxygen in the soil gas are determined using a field gas chromatograph. Supporting meteorological, soil temperature, and soil moisture data also are obtained. Based on data from the fall of 1985 and the spring, summer, and fall of 1986, soil gas pressures at all depths responded to changes in barometric pressure; however, the type of response varied, depending on soil moisture and temperature. During warm, dry weather, for example, soil gas pressures in the cover and the top of the refuse equilibrate rapidly with barometric pressure, indicating that diffusion is the major mechanism for gas transport at that time (no pressure gradients). The rate of diffusional flow depends on the properties of the cover materials, as well as the concentration gradients. Increases in soil moisture, in particular, decrease the gas-filled porosity of the cover materials and retard gas movement. Our results suggest that design and maintenance of tighter landfill covers should be considered at sites where gas recovery is anticipated, to prevent loss of methane and influx of oxygen.

Research Organization:
Argonne National Lab., IL (USA); Geotechnics, Inc., Columbus, OH (USA)
DOE Contract Number:
W-31109-ENG-38
OSTI ID:
6353714
Report Number(s):
CONF-870297-1; ON: DE87011490
Resource Relation:
Conference: 10. international landfill gas symposium, West Palm Beach, FL, USA, 9 Feb 1987; Other Information: Portions of this document are illegible in microfiche products
Country of Publication:
United States
Language:
English