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作 者:Omer Kawende Kalonda Ivon Ndala Tshiwis Boniface Mumbimb Atalatala Clement N’Zau Umba-Di-Mbudi Omer Kawende Kalonda;Ivon Ndala Tshiwis;Boniface Mumbimb Atalatala;Clement N’Zau Umba-Di-Mbudi(Geo-Hydro-Energy Research Group, University of Kinshasa, Kinshasa, Democratic Republic of the Congo;Department of Geosciences, Faculty of Science and Technology, University of Kinshasa, Kinshasa, Democratic Republic of the Congo;Polytechnic Faculty, President Joseph Kasa-Vubu State University, Boma, Democratic Republic of the Congo)
机构地区:[1]Geo-Hydro-Energy Research Group, University of Kinshasa, Kinshasa, Democratic Republic of the Congo [2]Department of Geosciences, Faculty of Science and Technology, University of Kinshasa, Kinshasa, Democratic Republic of the Congo [3]Polytechnic Faculty, President Joseph Kasa-Vubu State University, Boma, Democratic Republic of the Congo
出 处:《Journal of Geoscience and Environment Protection》2023年第5期404-426,共23页地球科学和环境保护期刊(英文)
摘 要:The headrace of the Inga hydropower complex is experiencing siltation problems, reducing the exploitable draft and limiting the production capacity of the two main Inga hydropower plants during the low water period. During the 2019 low water period, several sediment slumps occurred in the Shongo basin, disrupting the production of hydroelectric power generated by the Inga 1 & 2 power plant, resulting in massive load shedding of power supply to downstream customers. The cardinal aim of this study is to determine the quantities of sediments deposited and those eroded, in order to know the evolution of sedimentation in the Shongo basin from February 2020 to May 2021. The results obtained show that the running index of the generating units is determinant and influences the sedimentation process in the Shongo basin. The cleaning of the Shongo basin in terms of the spatial distribution of sedimentation from February 2020 to May 2021 is plausible.The headrace of the Inga hydropower complex is experiencing siltation problems, reducing the exploitable draft and limiting the production capacity of the two main Inga hydropower plants during the low water period. During the 2019 low water period, several sediment slumps occurred in the Shongo basin, disrupting the production of hydroelectric power generated by the Inga 1 & 2 power plant, resulting in massive load shedding of power supply to downstream customers. The cardinal aim of this study is to determine the quantities of sediments deposited and those eroded, in order to know the evolution of sedimentation in the Shongo basin from February 2020 to May 2021. The results obtained show that the running index of the generating units is determinant and influences the sedimentation process in the Shongo basin. The cleaning of the Shongo basin in terms of the spatial distribution of sedimentation from February 2020 to May 2021 is plausible.
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