Evolution of the Physico-Chemical Quality of the Water in the Manantali Dam Reservoir from 1989 (One Year after Impoundment) to 2022

Joseph Mbeur Faye, Saïdou Ndao, Louis Eugène Victor Sambou
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Abstract

The Manantali dam is located on the Bafing River in the Kayes region of Mali. It is the main tributary of the Senegal River. The water released from the dam provides year-round access to water for drinking, irrigation and livestock watering. The Manantali dam regulates the river’s flow, generates energy and supports agricultural development in all three countries (Mali, Mauritania, and Senegal). The aim of this article is to monitor changes in the physico-chemical quality of the water in the dam’s reservoir from 1989 (one year after the dam was impounded) to 2022. In order to carry out this work, we analysed the evolution of physico-chemical parameters in Stations 1 and 3 of the dam, on the basis of fluctuating water levels in the reservoir. The results obtained show a similarity in the parameters measured at the two stations, except for iron content, which is higher at Station 3. The average pH is weakly basic (7.44 at Station 1 and 7.29 at Station 3) and the average water temperature is between 26.5°C at Station 1 and 26.2°C at Station 3. The average conductivity of the water at Station 1 is 38.8 μS/cm and 39.8 μS/cm at Station 3, attesting to low mineralization of the water. The oxygen content of 5.75 mg/L at Station 1 and 5.00 mg/L at Station 3 shows good oxygenation of the water, which is favorable for the development of most fish and aquatic plant species. Ammonium levels of 0.02 mg/L at Station 1 and 0.06 mg/L at Station 3 show that the water is not contaminated. In addition, the Water Quality Index (WQI) was calculated, showing excellent water quality at Station 1 and good quality at Station 3. Overall, the results obtained show that the water is of good quality, enabling the authorities of the Organization for the Development of the Senegal River (OMVS) to achieve their development objectives.
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1989年(蓄水后1年)至2022年马南塔里水库水理化质量演变
Manantali大坝位于马里Kayes地区的Bafing河上。它是塞内加尔河的主要支流。从大坝释放的水提供了全年的饮用水、灌溉和牲畜用水。马南塔利大坝调节河流流量,产生能源,并支持这三个国家(马里、毛里塔尼亚和塞内加尔)的农业发展。本文的目的是监测1989年(大坝被扣押后一年)至2022年大坝水库水的理化质量变化。为了开展这项工作,我们根据水库水位的波动,分析了大坝1站和3站的理化参数的演变。得到的结果表明,除了3号站铁含量较高外,两个站点测量的参数相似。平均pH值为弱碱性(站1为7.44,站3为7.29),平均水温在站1的26.5℃至站3的26.2℃之间。1站位水的平均电导率为38.8 μS/cm, 3站位水的平均电导率为39.8 μS/cm,表明水的矿化程度较低。1号站和3号站的氧含量分别为5.75 mg/L和5.00 mg/L,表明水体氧合良好,有利于大多数鱼类和水生植物的发育。1号站的铵含量为0.02 mg/L, 3号站的铵含量为0.06 mg/L,这表明水没有受到污染。此外,计算了水质指数(WQI),结果表明1号站水质优良,3号站水质良好。总体而言,获得的结果表明,水质良好,使塞内加尔河发展组织(OMVS)当局能够实现其发展目标。
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