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Water Budget Analysis of Agulu Lake in Anambra State, Nigeria

机译:尼日利亚阿南布拉州特工湖水预算分析

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摘要

The elements of water budget equation were analyzed for the Agulu lake area and underlying aquifers. The water budget implications for soil and gully erosion were evaluated in relation to the geological formations and hydrogeotechnics. Results show that rainfall constitutes the main source of precipitation. It ranges from 1714.04mm to 1995.53mm annually. The potential groundwater aquifer volume is 1.5 X 10~7m~3. Discharge from aquifers contributes 7.4 X 10~7m~3 water annually. The amount of 1.72 X 10~5m~3 that is 60% of precipitation is lost to evaporation; 17 to 21% to infiltration. The quasi steady state of the lake water level and volume shows surface and groundwater continuity as explained by the small difference between total input and output values of the computed water budget of the lake and the aquifer. Flood studies indicate that 19.5% of the annual precipitation constitutes runoff, the main agent of gully and soil erosion, flooding and landslides. The other factors that control the distribution and location of gullies arc tithologic and strati graphical, while topography/gcomorphology controls gully distribution within various geologic units. A typical gully is about 500m X 50m X 30m long, wide and deep respectively. The destruction to life and property by runoffs/floods demands joint and sustained efforts by the community dwellers. NGOs, Local Government Areas, State governments. Federal Government and the International Communities.
机译:分析了阿古鲁湖区和下伏含水层的水预算方程的要素。评估了水预算对土壤和沟壑侵蚀的影响,并结合了地质构造和水文地质技术。结果表明,降雨是降水的主要来源。每年范围从1714.04mm到1995.53mm。潜在的地下水含水量为1.5 X 10〜7m〜3。含水层的排水每年贡献7.4 X 10〜7m〜3水。 1.72 X 10〜5m〜3的量占降水量的60%蒸发损失。 17至21%渗透。湖泊水位和水量的准稳态显示了地表和地下水的连续性,这可以通过计算得出的湖泊和蓄水层的总水量预算的总输入和输出值之间的微小差异来解释。洪水研究表明,年降水量的19.5%构成径流,这是沟壑和土壤侵蚀,洪水和滑坡的主要动因。控制沟渠分布和位置的其他因素是滴度和地层图,而地形/地貌控制着各种地质单元内沟壑的分布。典型的沟壑分别长约500m X 50m X 30m。径流/洪水对生命和财产的破坏需要社区居民的共同持续努力。非政府组织,地方政府区域,州政府。联邦政府和国际社会。

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