This paper presents the results of field tests of hydrologic parameters in
a landfill and the cy of the pumping method to reduce leachate levels in th
e landfill. The field hydraulic conductivity and storativity of waste and b
uried cover soils in the landfill are measured by pumping and slug tests. T
he hydrologic condition inside the landfill is first calibrated using the d
rawdown-time curve obtained from the pumping test, and the flow behavior of
leachate during pumping in the landfill, when various layers of waste and
buried cover soil exist, is analyzed through three-dimensional numerical si
mulation of flow. The results of the field investigation show that the buri
ed cover soil of low hydraulic conductivity forms an impermeable layer prev
enting the downward flow of leachate and upward flow of landfill gas. The h
ydraulic conductivities of the pumping test and slug tests were quite close
on the same order of magnitude. It was also possible to match the drawdown
-time data of the field tests with those of the model using input data clos
e to the hydrologic property obtained from the field tests. The numerical f
low analysis showed that pumping was possible up to 120 tons/day for a sing
le well without a drain, while the pumping rate could be increased to 300 t
ons/day for the same well with the drain. From the vertical section of the
flow vector with a horizontal drain, the barrier role of buried cover soil
is identified, which was proposed by examining thp water contents of the di
sposed cover soil and waste in the field.