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埃塞俄比亚梅格奇大坝流域土地利用动态对水文和泥沙淤积影响的建模

Modeling Impact of Land Use Dynamics on Hydrology and Sedimentation of Megech Dam Watershed, Ethiopia.

作者信息

Assfaw Abebe Tarko

机构信息

Civil Engineering Department, College of Engineering, Debre Berhan University, P.O. Box 445, Debre Berhan, Ethiopia.

出版信息

ScientificWorldJournal. 2020 Oct 24;2020:6530278. doi: 10.1155/2020/6530278. eCollection 2020.

Abstract

Land use/land cover dynamics change the hydrology and sediment yield of the watershed. This research on how land use dynamics alters catchment hydrology and reservoir sedimentation aids the government to implement appropriate response strategies to minimize undesirable future impacts on the upper Megech dam reservoir. For this study, the impacts were quantified and analyzed through hydrological modeling (SWAT). The overall analysis was performed by using 1998 historical and 2016 recent land use satellite images. The analysis has shown that the cultivated land has increased from 60.69% to 67.17% and urban land from 2.3% to 3.36% between 1998 and 2016. Whereas the grassland area has decreased from 11.42% to 5.33%, plantation forest from 1.84% to 0.9%, and bareland from 3.58% to 2.56%. A comparison of the simulated outputs of the model shows that the mean annual surface runoff for 1998 land use was 251.3 mm and had changed to 316.7 mm in 2016 land use. The mean annual streamflow changed from 150.3 m/sec to 165.6 m/sec for 1998 and 2016 land uses, respectively. Similarly, 10.23 t/ha mean annual sediment load gets into Megech dam reservoir in 1998 LULC and was changed to 13.61 t/ha in 2016 LULC. This shows that streamflow, surface runoff, and sediment yield increases by 10.2%, 26.03%, and 33.3% in 2016 land use as compared with 1998 land use. Finally, the most dynamic subbasins that have a significant impact on streamflow and sediment yield were identified. Based on this, subbasins 13, 17, 19, 20, 23, 24, and 25 were found to be the most dynamic and change sensitive subbasins that have a significant contribution to the increment of runoff and sediment yield in Megech dam watershed.

摘要

土地利用/土地覆盖动态变化改变了流域的水文状况和产沙量。这项关于土地利用动态如何改变集水区水文状况和水库淤积情况的研究,有助于政府实施适当的应对策略,以尽量减少未来对上梅格赫大坝水库产生的不良影响。在本研究中,通过水文模型(SWAT)对这些影响进行了量化和分析。总体分析使用了1998年的历史土地利用卫星图像和2016年的近期土地利用卫星图像。分析表明,1998年至2016年期间,耕地面积从60.69%增加到67.17%,城市用地从2.3%增加到3.36%。而草地面积从11.42%减少到5.33%,人工林从1.84%减少到0.9%,裸地从3.58%减少到2.56%。模型模拟输出结果的对比显示,1998年土地利用情况下的年均地表径流量为251.3毫米,在2016年土地利用情况下变为316.7毫米。1998年和2016年土地利用情况下的年均河川径流量分别从150.3立方米/秒变为165.6立方米/秒。同样,1998年土地利用/土地覆被情况下,年均输沙量为10.23吨/公顷,在2016年土地利用/土地覆被情况下变为13.61吨/公顷。这表明,与1998年土地利用情况相比,2016年土地利用情况下的河川径流量、地表径流量和产沙量分别增加了10.2%、26.03%和33.3%。最后,确定了对河川径流量和产沙量有重大影响的最活跃子流域。基于此,发现子流域13、17、19、20、23、24和25是最活跃且对变化敏感的子流域,它们对上梅格赫大坝流域径流量和产沙量的增加有重大贡献。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/acc4/7604611/4e39f7c52f09/TSWJ2020-6530278.001.jpg

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