Githumbi Esther, Kamamia Ann, Kämpf Lucas, Mwangi Hosea, Sang Joseph, Karanja Joseph, Zech Michael, Julich Stefan, Feger Karl-Heinz
Institute of Soil Science and Site Ecology, TU Dresden, Germany.
Institute of Soil Science and Site Ecology, TU Dresden, Germany.
Sci Total Environ. 2024 Dec 1;954:176767. doi: 10.1016/j.scitotenv.2024.176767. Epub 2024 Oct 10.
Globally, siltation of water reservoirs is a major risk and cost to the provision of fresh water. Therefore, managing reservoir sedimentation is a significant task for water management agencies. In Kenya, the Ruiru water reservoir, one of four water reservoirs supplying Nairobi with drinking water has experienced a significant loss of volume since construction in 1949. However, there have been no studies characterizing the long-term catchment dynamics such as erosion, sedimentation and accumulation in the reservoir. A detailed understanding of the sediment dynamics such as identification of sediment source area; processes driving soil erosion in the catchment and accumulation in the reservoir, and identification of flood layers are necessary for the reservoir and landscape management. The accumulated sediment has not been characterized; therefore, long-term land-use and climate change impacts on the catchment on the reservoir are not documented. The study aims to identify the historical land use and climate events in the catchment impacting the reservoir through a multiproxy sediment characterization of the sediment accumulating in the Ruiru reservoir. An undisturbed 1-m sediment core retrieved in 2017 from Ruiru Reservoir was dated using Pb and Cs and particle size distribution and chemical element profiles analyzed. The accumulated sediment is a predominantly fine-grained red silt, with a particle size end-member analysis identifying four possible sources or processes of sediment accumulation. The multi-proxy analysis reveals six periods of significant accumulation, 1949, 1963/64, 1974/75, 1982/83, 1997/98 and 2013/14. The peaks coincide with high rainfall events and two are attributed to significant land-use changes in the catchment. The study identifies the catchment dynamics with a significant sediment input into the reservoir. This highlights the importance of reservoirs as environmental archives documenting 20th century land -use and climate events while providing a long-term perspective for management of critical water infrastructure.
在全球范围内,水库淤积是提供淡水的一项重大风险和成本。因此,管理水库淤积是水资源管理机构的一项重要任务。在肯尼亚,鲁伊鲁水库是为内罗毕供应饮用水的四个水库之一,自1949年建成以来,其蓄水量大幅减少。然而,尚未有研究对该水库长期的集水区动态进行描述,如侵蚀、淤积和堆积情况。详细了解沉积物动态,如确定沉积物源区;驱动集水区土壤侵蚀和水库堆积的过程,以及识别洪水层,对于水库和景观管理至关重要。目前尚未对积累的沉积物进行特征描述;因此,长期土地利用和气候变化对集水区及水库的影响尚无记录。本研究旨在通过对鲁伊鲁水库中积累的沉积物进行多指标沉积物特征分析,确定集水区内影响该水库的历史土地利用和气候事件。2017年从鲁伊鲁水库获取的一个未扰动的1米沉积物岩芯,采用铅和铯进行年代测定,并分析了粒度分布和化学元素剖面。积累的沉积物主要是细粒红色粉砂,粒度端元分析确定了沉积物积累的四个可能来源或过程。多指标分析揭示了六个显著堆积期,分别为1949年、1963/64年、1974/75年、1982/83年、1997/98年和2013/14年。这些峰值与高降雨事件相吻合,其中两个峰值归因于集水区内重大的土地利用变化。该研究确定了集水区动态以及大量沉积物输入水库的情况。这凸显了水库作为记录20世纪土地利用和气候事件的环境档案的重要性,同时为关键水利基础设施的管理提供了长期视角。