2022
DOI: 10.3390/environments9020019
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Characterization of the Dynamics of Leachate Contamination Plumes in the Surroundings of the Hulene-B Waste Dump in Maputo, Mozambique

Abstract: The contamination of areas around solid urban waste dumps is a global challenge for the maintenance of environmental quality in large urban centres in developing countries. This study applied a geophysical method (electrical resistivity) to identify leachate contamination plumes in the subsoil and groundwater, as well as to describe their temporal dynamics (2020 and 2021) in the surroundings of the Hulene-B waste dump, Maputo, Mozambique. Eight 400 m electrical resistivity profiles were performed, four profile… Show more

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Cited by 6 publications
(4 citation statements)
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“…Waste deposition in the Hulene-B dump is mostly located in QMa, spreading to the East (TPv). Geologically, the Hulene-B waste dump is in the Mesocenozoic sedimentary basin, in southern Mozambique [36] in a contact zone of two lithologies (Ponta Vermelha TPv, and Malhazine QMa Formations) [27] (Figure 2). The Ponta Vermelha Formation dates from the upper Pliocene to the lower Pleistocene, being composed in the upper part of ferruginous sandstones and red silty sands, which gradually change to yellow and whitish sands [37].…”
Section: Study Areamentioning
confidence: 99%
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“…Waste deposition in the Hulene-B dump is mostly located in QMa, spreading to the East (TPv). Geologically, the Hulene-B waste dump is in the Mesocenozoic sedimentary basin, in southern Mozambique [36] in a contact zone of two lithologies (Ponta Vermelha TPv, and Malhazine QMa Formations) [27] (Figure 2). The Ponta Vermelha Formation dates from the upper Pliocene to the lower Pleistocene, being composed in the upper part of ferruginous sandstones and red silty sands, which gradually change to yellow and whitish sands [37].…”
Section: Study Areamentioning
confidence: 99%
“…Momade et al [38] performed drillings L16 and L125 (Figure 2a) in two geological formations around the dump, showing that TPv formation underlain QMa, and TSa (Miocene-Pliocene) is composed of clayey, calcareous sandstone with Ostrea cullata in its upper part. Geologically, the Hulene-B waste dump is in the Mesocenozoic sedimentary bas in southern Mozambique [36] in a contact zone of two lithologies (Ponta Vermelha TP and Malhazine QMa Formations) [27] (Figure 2). The Ponta Vermelha Formation dat from the upper Pliocene to the lower Pleistocene, being composed in the upper part ferruginous sandstones and red silty sands, which gradually change to yellow an whitish sands [37].…”
Section: Study Areamentioning
confidence: 99%
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