Nitrate pollution in groundwater in two selected areas from Cameroon and Chad in the Lake Chad basin

Water Policy ◽  
2010 ◽  
Vol 12 (5) ◽  
pp. 722-733 ◽  
Author(s):  
Benjamin Ngounou Ngatcha ◽  
Djoret Daira

The shallow aquifer in the Lake Chad basin is highly vulnerable to pollution. Analysis carried out on 316 wells and boreholes have showed a tendency towards an increase of nitrate values, exceeding 50 mg l−1. Nitrate concentrations ranged between about 1 and 300 mg l−1. Large variation in concentration was observed in wells and boreholes that are only short distances apart. High concentrations of nitrate in wells, especially in a recharge area along the sand dunes, or via infiltration from river banks, irrigation channels, and infiltration of urban wastewater into groundwater from septic tanks, pose a serious problem for drinking water supply. In Cameroon and Chad, the results of the investigation indicate a variation of nitrate concentration in groundwater between the two areas. The primary origin of this pollution is agricultural proliferation activities that are developed and stressed by socio-economic needs outside the urban area, and by urban expansion within the area served by a decrepit network of urban area sewers. Substancial differences in values of nitrate concentrations were observed in groundwater from adjacent wells and boreholes, indicating local rather than regional contamination.

Earth ◽  
2021 ◽  
Vol 2 (2) ◽  
pp. 340-356
Author(s):  
Forrest W. Black ◽  
Jejung Lee ◽  
Charles M. Ichoku ◽  
Luke Ellison ◽  
Charles K. Gatebe ◽  
...  

The present study investigated the effect of biomass burning on the water cycle using a case study of the Chari–Logone Catchment of the Lake Chad Basin (LCB). The Chari–Logone catchment was selected because it supplies over 90% of the water input to the lake, which is the largest basin in central Africa. Two water balance simulations, one considering burning and one without, were compared from the years 2003 to 2011. For a more comprehensive assessment of the effects of burning, albedo change, which has been shown to have a significant impact on a number of environmental factors, was used as a model input for calculating potential evapotranspiration (ET). Analysis of the burning scenario showed that burning grassland, which comprises almost 75% of the total Chari–Logone land cover, causes increased ET and runoff during the dry season (November–March). Recent studies have demonstrated that there is an increasing trend in the LCB of converting shrubland, grassland, and wetlands to cropland. This change from grassland to cropland has the potential to decrease the amount of water available to water bodies during the winter. All vegetative classes in a burning scenario showed a decrease in ET during the wet season. Although a decrease in annual precipitation in global circulation processes such as the El Niño Southern Oscillation would cause droughts and induce wildfires in the Sahel, the present study shows that a decrease in ET by the human-induced burning would cause a severe decrease in precipitation as well.


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