Groundwater from the keta-Anlo artesian basin / Akiti, T. T.

Public ISBD Titre : Groundwater from the keta-Anlo artesian basin Type de document : texte imprimé Auteurs : Akiti, T. T. Mention d'édition : Water Resources Research Unit Editeur : Water Resources Research Unit Année de publication : 1977 ISBN/ISSN/EAN : CI-04499 Note générale : The extensive limestone aquifer underlying the Ketaq-anlo basin in Ghana has been discussed with particular reference to the flowing well at Anyako. A hypothesis has been advanced that the recharge source of this aquifer is on the river Mono in the republic of Togo. The quality of the groundwater from the limestone es good, however, salt water instrusion poses a threat to overdevelopment of the aquifer. Since the quality of the water is very good, methods have been proposed for the development of the artesian basin so that salt water intrusion does not occur. Mots-clés : Eau souterraine  Hydrogéologie  Alimentation en eau Index. décimale : 644.6 Alimentation en eau Résumé : The extensive limestone aquifer underlying the Ketaq-anlo basin in Ghana has been discussed with particular reference to the flowing well at Anyako. A hypothesis has been advanced that the recharge source of this aquifer is on the river Mono in the republic of Togo. The quality of the groundwater from the limestone es good, however, salt water instrusion poses a threat to overdevelopment of the aquifer. Since the quality of the water is very good, methods have been proposed for the development of the artesian basin so that salt water intrusion does not occur. Note de contenu : The extensive limestone aquifer underlying the Ketaq-anlo basin in Ghana has been discussed with particular reference to the flowing well at Anyako. A hypothesis has been advanced that the recharge source of this aquifer is on the river Mono in the republic of Togo. The quality of the groundwater from the limestone es good, however, salt water instrusion poses a threat to overdevelopment of the aquifer. Since the quality of the water is very good, methods have been proposed for the development of the artesian basin so that salt water intrusion does not occur. Groundwater from the keta-Anlo artesian basin [texte imprimé] / Akiti, T. T.  . -  Water Resources Research Unit . - Water Resources Research Unit, 1977. ISSN : CI-04499 The extensive limestone aquifer underlying the Ketaq-anlo basin in Ghana has been discussed with particular reference to the flowing well at Anyako. A hypothesis has been advanced that the recharge source of this aquifer is on the river Mono in the republic of Togo. The quality of the groundwater from the limestone es good, however, salt water instrusion poses a threat to overdevelopment of the aquifer. Since the quality of the water is very good, methods have been proposed for the development of the artesian basin so that salt water intrusion does not occur. Mots-clés : Eau souterraine  Hydrogéologie  Alimentation en eau Index. décimale : 644.6 Alimentation en eau Résumé : The extensive limestone aquifer underlying the Ketaq-anlo basin in Ghana has been discussed with particular reference to the flowing well at Anyako. A hypothesis has been advanced that the recharge source of this aquifer is on the river Mono in the republic of Togo. The quality of the groundwater from the limestone es good, however, salt water instrusion poses a threat to overdevelopment of the aquifer. Since the quality of the water is very good, methods have been proposed for the development of the artesian basin so that salt water intrusion does not occur. Note de contenu : The extensive limestone aquifer underlying the Ketaq-anlo basin in Ghana has been discussed with particular reference to the flowing well at Anyako. A hypothesis has been advanced that the recharge source of this aquifer is on the river Mono in the republic of Togo. The quality of the groundwater from the limestone es good, however, salt water instrusion poses a threat to overdevelopment of the aquifer. Since the quality of the water is very good, methods have been proposed for the development of the artesian basin so that salt water intrusion does not occur.

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