摘要
Water resources, although renewable, are limited and threatened by climate <span>change and anthropic activities. Assessment and forecasting of these resources</span> can provide valuable information for water resource planners. This study aims to quantify the surface water resources used for sugarcane production in sugar complexes of Ferkessedougou. This is based on the morphological characterization of the river Morrison and Lopkoho dams and on <span>extreme daily flow probability of occurrence estimation using frequency analysis</span> method. The bathymetric survey showed that the Morrison Dam im<span>poundment had a maximum depth of 11.98 m;a water capacity of 11,656,735.5</span> m<sup>3</sup>. For the Lokpoho dam, the reservoir had a maximum depth of 8.82 m, which corresponds to a water volume of 4,354,531.5 m<sup>3</sup>. Nevertheless, the water capacity of these reservoirs is greatly reduced by a large volume of sediment estimated at 1,013,058.96 m<sup>3</sup> for Morrison and 599,740 m<sup>3</sup> for Lokpoho. Statistical analysis of maximum daily flows shows that flows between 73.9 and 100 m<sup>3</sup>/s have the potential to occur every five years at the Route Korhogo Badikaha hydrometric station. The recurrence of the decennial (298 m<sup>3</sup>) and quinquenal (248 m<sup>3</sup>) flows shows the importance of the flood flows of the Bandama River. It also shows that the low water levels of the Bandama are very pronounced. The minimum flow that SUCAF-CI water managers should expect every five years is 1.36 m<sup>3</sup>/s and the ten-year low flow is 2.10 m<sup>3</sup>/s. These results are indicators of water scarcity risks and could guide decision making in the Ferkessedougou sugar complexes.
Water resources, although renewable, are limited and threatened by climate <span>change and anthropic activities. Assessment and forecasting of these resources</span> can provide valuable information for water resource planners. This study aims to quantify the surface water resources used for sugarcane production in sugar complexes of Ferkessedougou. This is based on the morphological characterization of the river Morrison and Lopkoho dams and on <span>extreme daily flow probability of occurrence estimation using frequency analysis</span> method. The bathymetric survey showed that the Morrison Dam im<span>poundment had a maximum depth of 11.98 m;a water capacity of 11,656,735.5</span> m<sup>3</sup>. For the Lokpoho dam, the reservoir had a maximum depth of 8.82 m, which corresponds to a water volume of 4,354,531.5 m<sup>3</sup>. Nevertheless, the water capacity of these reservoirs is greatly reduced by a large volume of sediment estimated at 1,013,058.96 m<sup>3</sup> for Morrison and 599,740 m<sup>3</sup> for Lokpoho. Statistical analysis of maximum daily flows shows that flows between 73.9 and 100 m<sup>3</sup>/s have the potential to occur every five years at the Route Korhogo Badikaha hydrometric station. The recurrence of the decennial (298 m<sup>3</sup>) and quinquenal (248 m<sup>3</sup>) flows shows the importance of the flood flows of the Bandama River. It also shows that the low water levels of the Bandama are very pronounced. The minimum flow that SUCAF-CI water managers should expect every five years is 1.36 m<sup>3</sup>/s and the ten-year low flow is 2.10 m<sup>3</sup>/s. These results are indicators of water scarcity risks and could guide decision making in the Ferkessedougou sugar complexes.
作者
Affoué Berthe Yao
Sampah Georges Eblin
Gla Blaise Ouedé
Kouakou Lazare Kouassi
Do Ange Désiré Soro
Arona Diedhiou
Bi Crépin Péné
Affoué Berthe Yao;Sampah Georges Eblin;Gla Blaise Ouedé;Kouakou Lazare Kouassi;Do Ange Désiré Soro;Arona Diedhiou;Bi Crépin Péné(Laboratory of Environmental Sciences and Technologies, UFR Environment, Jean Lorougnon Guédé University, Daloa, Côte d’Ivoire;Laboratory NEXUS “Climate, Water, Agriculture, Energy Nexus and Climate Services” Research and Development Institute, Felix Houphouët Boigny University, Abidjan, Côte d’Ivoire;Research and Development Department, SUCAF-CI, Ferkessedougou, Côte d’Ivoire)
