Editing Hydrogeology of Chad
Jump to navigation
Jump to search
Your changes will be displayed to readers once an authorised user accepts them. (help) |
Warning: You are not logged in. Your IP address will be publicly visible if you make any edits. If you log in or create an account, your edits will be attributed to your username, along with other benefits.
The edit can be undone. Please check the comparison below to verify that this is what you want to do, and then save the changes below to finish undoing the edit.
This page supports semantic in-text annotations (e.g. "[[Is specified as::World Heritage Site]]") to build structured and queryable content provided by Semantic MediaWiki. For a comprehensive description on how to use annotations or the #ask parser function, please have a look at the getting started, in-text annotation, or inline queries help pages.
Latest revision | Your text | ||
Line 276: | Line 276: | ||
Groundwater is abstracted for domestic use and livestock watering through hand dug wells (in the shallow aquifer) and boreholes. | Groundwater is abstracted for domestic use and livestock watering through hand dug wells (in the shallow aquifer) and boreholes. | ||
− | ||In the Chad | + | ||In the Lake Chad basin Quaternary aquifer there are high nitrate concentrations linked to agriculture discharges and faecal contamination. High fluoride concentrations are also seen. Groundwater in parts of the northern Kanem region contains high concentrations of sodium carbonates and sodium sulphates. |
|} | |} | ||