As I pointed out in my last post, the groundwater recharges dependents on
the surface water inflows and the river recharges from upstream. And at the
same time it is a closed system, on that account the vulnerability for pollution
could be immense, because every contamination will accumulate over the time. In
particular, because of a growing population, there is a growing demand for
food, therefore more production and more fertilization. Which implicates a
great threat to the groundwater. While working on the project ‘Advice on
groundwater resources for the Lake Chad Basin Commission’, the BGR published
several reports on the quality of water in this area. I will give you a brief
summary on that.
In their most recent report (Nr. 4, 2012), they used data from 441 water
samples, 19 from surface water and 422 from groundwater. They looked at the
anion and cation species and trace elements by measuring temperature, pH and
electric conductivity. In general, groundwater quality depends on the paste of
infiltration. To put it simply, fast infiltration means less minerals and less
filtering than slow infiltration. The paste of infiltration depends on the flow
features and thickness of the unsaturated zone. As you can see on the figure
below the light-colour areas are characterized by direct recharge and therefore
low in minerals, whereas the dark-colour areas are marked by low flow velocity,
so the water had time to mineralize.
Figure 7: BGR Nr. 4, 2012
The danger of pollution is immense higher with a direct recharge of water
than with a long time of filtration through the ground. Therefore, hand dug
open wells are a particular threat to the groundwater. The next figure is
showing the nitrate pollution, a pollution, which is caused by agricultural
fertilizers and human or animal faeces. With more than 50mg/l nitrate (US and
WHO limit, the European limit is 25mg/l) the water can harm the health of a
human body. In 59 samples of water were the limit exceeded.
Figure 8: BGR Nr. 4, 2012
To conclude, there is a punctual pollution of nitrate in some areas.
Mainly caused by livestock and farming and open contact to the groundwater. On
that account, the BGR strongly recommend a better protection of the
groundwater, especially concerning open hand dug wells. But in general the
pollution of water is at the moment not the greatest threat for this area. More
important is a constantly water supply to save lake Chad from drying and keep a
basis of existence for all the people living there.
You consult a very interesting study by BGR here. You recognise well the increased risk of contamination posed by groundwater recharged quickly by surface infiltration that does undergo attenuation or solutes and particles by pore-matrix flow. Look out for a new paper due out in a few weeks which shows that this problem occurs throughout the tropics (Jasechko, S. and Taylor, R.G., in press. Intensive rainfall recharges tropical groundwaters. Environmental Research Letters).
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