Groundwater Pollution in Africa 2006
DOI: 10.1201/9780203963548.ch13
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Statistical assessment of groundwater quality in Bamako City, Mali

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Cited by 6 publications
(7 citation statements)
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“…Thus, during the dry season there is an accumulation of substances from atmospheric deposition and anthropogenic inputs in the soil, whereas during the rainy season, these substances dissolve and are washed by recharging rain water. A similar observation was made around the Bamako-Mali urban settlement (Traore et al 2006). However, the bore wells tapping deeper aquifers are not affected by this process, probably due to selective removal of ions during long periods of contact with the soil.…”
Section: Shallow Aquifer Quality Characteristicssupporting
confidence: 55%
“…Thus, during the dry season there is an accumulation of substances from atmospheric deposition and anthropogenic inputs in the soil, whereas during the rainy season, these substances dissolve and are washed by recharging rain water. A similar observation was made around the Bamako-Mali urban settlement (Traore et al 2006). However, the bore wells tapping deeper aquifers are not affected by this process, probably due to selective removal of ions during long periods of contact with the soil.…”
Section: Shallow Aquifer Quality Characteristicssupporting
confidence: 55%
“…By the early 1980s, several nations had reintroduced strict fire suppression policies. Mali, Burkina Faso, and Guinea all passed laws forbidding any form of savanna fire (Traoré 1980; Government of Haute Volta 1981; Fairhead and Leach 1995). The laws often carried harsh penalties 6 .…”
Section: The Burning Experimentsmentioning
confidence: 99%
“…Monitoring the long-term change in groundwater quality is generally focused on deep aquifers, where typically there is a lag of years or decades between the ingress of contaminants from surface hazards and its impact on groundwater quality. For example, examination of long-term data for a drilled well field in Mochudi, Botswana suggest nitrate levels rose from <1 mg/L in the 1960s to over 30 mg/L in the 1980s [ 8 ], whilst borehole data for Bamako, Mali suggest median nitrate as total N rose from 5 mg/L in 1990 to over 20 mg/L by 2002 [ 9 ]. However, whilst deep aquifers are an important potential source of domestic water, boreholes and deep wells are expensive to construct and are only affordable by wealthy individuals or accessible to the urban poor through donor funded projects.…”
Section: Introductionmentioning
confidence: 99%