Wet and gassy zones in a municipal landfill from P- and S-wave velocity fields

Journal Article (2016)
Author(s)

L.A. Konstantaki (TU Delft - Geo-engineering)

R. Ghose (TU Delft - Applied Geophysics and Petrophysics)

D.S. Draganov (TU Delft - Applied Geophysics and Petrophysics)

Timo Heimovaara (TU Delft - Geo-engineering)

Research Group
Applied Geophysics and Petrophysics
Copyright
© 2016 L.A. Konstantaki, R. Ghose, D.S. Draganov, T.J. Heimovaara
DOI related publication
https://doi.org/10.1190/GEO2015-0581.1
More Info
expand_more
Publication Year
2016
Language
English
Copyright
© 2016 L.A. Konstantaki, R. Ghose, D.S. Draganov, T.J. Heimovaara
Research Group
Applied Geophysics and Petrophysics
Issue number
6
Volume number
81
Pages (from-to)
75-86
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

The knowledge of the distribution of leachate and gas in a municipal landfill is of vital importance to the landfill operators performing improved landfill treatments and for environmental protection and efficient biogas extraction. We have explored the potential of using the velocity fields of seismic S- and P-waves to delineate the wet and gassy (relatively dry, gas/air-filled) zones inside a landfill.We have analyzed shallow S- and P-wave reflection data and seismic surface-wave data acquired at a very heterogeneous landfill site, where biogas was extracted. A joint interpretation of the independently estimated velocity fields from these various approaches has allowed us to localize anomalously low- and high-velocity zones in the landfill. From the complementary information provided by P- and S-wave velocity fields, we have inferred the leachate-bearing wet zones and the gassy zones inside the landfill. Independent measurements of gas flow and mechanical tip resistance to waste deformation validate our seismic interpretations.