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Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/12451

Title: Spectral time-domain induced polarisation and magnetic surveying − an efficient tool for characterisation of solid waste deposits in developing countries
Authors: Wemegah, David Dotse
Fiandaca, Gianluca
Auken, Esben
Menyeh, Aboagye
Danuor, Sylvester Kojo
Issue Date: 1-Jun-2017
Publisher: European Association of Geoscientists & Engineers
Citation: Near Surface Geophysics, 2017, 15, 75-84., doi: 10.3997/1873-0604.2016048
Abstract: Time-domain induced polarisation and magnetic data were acquired to map and characterise the decommissioned and un-engineered municipal solid waste disposal site of the Kwame Nkrumah University of Science and Technology, located in the Kumasi Metropolis of Ghana. In this survey, 13 induced polarisation profiles 500–800 m long and 26 magnetic profiles 400–800 m long were acquired. In addition, two boreholes were drilled to help in the interpretation of the geophysical data. The study was carried out with the aim of determining the risk posed by the waste deposit to the quality of the soil and the ground water system, which is the main potable water supply for the Secondary School, the University Teaching Hospital and the Veterinary School, situated within the catchment area of the site. Full-decay 2-D time-domain induced polarisation inversions in terms of Cole–Cole parameters were used for interpreting the induced polarisation data. The chargeability, resistivity and normalised chargeability distributions, together with the magnetic results, aided in a full characterisation of the site geology, the waste and the associated pollution plume. In particular, clear contrasts in resistivity and the polarisation parameters were found between the saprolite layer and the granitic bedrock, which are the main lithological units of the area. Furthermore, it was found that the Kwame Nkrumah University of Science and Technology waste deposit is characterised by a low-chargeability and low-resistivity signature and that the low-resistivity area spreads out from the waste deposit into the permeable saprolite layer, indicating the presence of a leachate plume. A fracture zone in the granitic bedrock beneath the waste deposit, which is a potential conduit for leachate contamination of the ground water system, was also identified. The study thus provides the information needed for assessing the future impact of the waste on the water quality in the area and for designing risk-mitigation actions.
Description: An article published by European Association of Geoscientists & Engineers and also available at doi: 10.3997/1873-0604.2016048
URI: http://hdl.handle.net/123456789/12451
Appears in Collections:College of Science

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