Aquifer Depletion in the Arlit Mining Area (Tim Mersoï Basin, North Niger)
Farida Boubé Dobi,
Eugène Koffi Kouakou,
Yahaya Nazoumou,
Boubacar Abdou Boko,
Sophie Ngomune Edimo,
Fadji Zaouna Maina,
Moussa Konaté
Affiliations
Farida Boubé Dobi
Laboratoire de Génie Civil, Géosciences et Sciences Géographiques (UMRI 68), Institut National Polytechnique Houphouët-Boigny (INPH-B), Yamoussoukro BP 1093, Côte d’Ivoire
Eugène Koffi Kouakou
Laboratoire de Génie Civil, Géosciences et Sciences Géographiques (UMRI 68), Institut National Polytechnique Houphouët-Boigny (INPH-B), Yamoussoukro BP 1093, Côte d’Ivoire
Yahaya Nazoumou
Laboratoire des Eaux Souterraines et Géo-Ressources, Département de Géologie, Faculté des Sciences, Université Abdou Moumouni (UAM), BP 10 662, Niamey 8000, Niger
Boubacar Abdou Boko
Laboratoire des Eaux Souterraines et Géo-Ressources, Département de Géologie, Faculté des Sciences, Université Abdou Moumouni (UAM), BP 10 662, Niamey 8000, Niger
Sophie Ngomune Edimo
Laboratoire de Génie Civil, Géosciences et Sciences Géographiques (UMRI 68), Institut National Polytechnique Houphouët-Boigny (INPH-B), Yamoussoukro BP 1093, Côte d’Ivoire
Fadji Zaouna Maina
NASA Goddard Space Flight Center, Hydrological Sciences Laboratory, Code 617, Greenbelt, MD 20771, USA
Moussa Konaté
Laboratoire des Eaux Souterraines et Géo-Ressources, Département de Géologie, Faculté des Sciences, Université Abdou Moumouni (UAM), BP 10 662, Niamey 8000, Niger
Located in northwestern Niger, the Tim Mersoï Basin (TMB) is an important mining region in the scale of West Africa. Groundwater is considered the main source of fresh water in the basin, especially for mining activities. It, therefore, appears essential to monitor their responses to these activities. However, no study has been carried out in the Tim Mersoï Basin. This study aims to evaluate the groundwater storage changes (GWSC) of the TMB and to analyze the spatio-temporal evolution of the Tarat aquifer under the effect of mining activities in the Arlit region. For this purpose, Gravity Recovery And Climate Experiment (GRACE), Global Land Data Assimilation System (GLDAS), and in-situ data were used. The results show a variation of the GWS from 2002 to 2019 of about −0.1310 cm/year on the scale of the basin and −0.0109 cm/year in the Arlit mining area. The GWSC at the basin scale and the one at the Arlit region scale were shown to be linked with an RMSE between the two datasets of 0.79. This shows the potential of GRACE for contextualizing studies in small areas. The study also highlighted that the groundwater flow direction was highly modified; the drawdown of the Tarat water table was more than 50 m in the areas heavily impacted by mining activities, with an increasing intensity from the northwest to the southeast of Arlit.
