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Analysis of flow behavior in a landfill with cover soil of low hydraulic conductivity.

Authors :
Jang, Y. -S
Source :
Environmental Geology; Jan2000, Vol. 39 Issue 3/4, p292-298, 7p
Publication Year :
2000

Abstract

This paper presents the results of field tests of hydrologic parameters in a landfill and the results of numerical simulation to find the efficiency of the pumping method to reduce leachate levels in the landfill. The field hydraulic conductivity and storativity of waste and buried cover soils in the landfill are measured by pumping and slug tests. The hydrologic condition inside the landfill is first calibrated using the drawdown-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 simulation of flow. The results of the field investigation show that the buried cover soil of low hydraulic conductivity forms an impermeable layer preventing the downward flow of leachate and upward flow of landfill gas. The hydraulic 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 close to the hydrologic property obtained from the field tests. The numerical flow analysis showed that pumping was possible up to 120 tons/day for a single well without a drain, while the pumping rate could be increased to 300 tons/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 the water contents of the disposed cover soil and waste in the field. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
09430105
Volume :
39
Issue :
3/4
Database :
Complementary Index
Journal :
Environmental Geology
Publication Type :
Academic Journal
Accession number :
16565943
Full Text :
https://doi.org/10.1007/s002540050008