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首页> 外文期刊>Engineering >Assessing the Impacts of Land Use and Land Cover Changes on Hydrology of the Mbarali River Sub-Catchment. The Case of Upper Great Ruaha Sub-Basin, Tanzania
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Assessing the Impacts of Land Use and Land Cover Changes on Hydrology of the Mbarali River Sub-Catchment. The Case of Upper Great Ruaha Sub-Basin, Tanzania

机译:评估土地利用和土地覆盖变化对曼巴里河子流域水文的影响。坦桑尼亚上部伟大Ruaha Sub-Basin的案例

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Intensification of agricultural land use and population growth from 1990-2017 has caused changes in land cover and land use of the Mbarali River sub-catchment which is located in the Upper Great Ruaha Sub basin, Tanzania. This has affected the magnitude of the surface runoff, total water yield and the groundwater flow. This study assesses the impacts of the land cover and land use changes on the stream flows and hydrological water balance components (surface runoff, water yield, percolation and actual evapotrans-piration). The land use and land cover (LULC) maps for three window period snapshots, 1990, 2006 and 2017 were created from Landsat TM and OLI_TIRS with the help of QGIS version 2.6. Supervised classification was used to generate LULC maps using the Maximum Likelihood Algorithm and Kappa statistics for assessment of accuracy. SWAT was set up and run to simulate stream flows and hydrological water balance components. The assessment of the impacts of land use and land cover changes on stream flows and hydrological water balance component was performed by comparing hydrological parameters simulated by SWAT using land use scenarios of 2006 and 2017 against the baseline land use scenario of 1990. Accuracy of LULC classification was good with Kappa statistics ranging between 0.9 and 0.99. There was a drastic increase in areal coverage of cultivated land, for periods 1990-2006 (5.84%) and 2006-2017 (12.05%) compared to other LULC. During 2006 and 2017 surface runoff increased by 4% and 9% respectively; however, water yield increased by only 0.5% compared to 1990 baseline period. This was attributed to increased proportion of cultivated land in the sub-catchment which has a high curve number (59.60) that indicates a higher runoff response and low infiltration rate.
机译:从1990 - 2017年的农业土地利用和人口增长的加剧导致曼巴里河子集水区的土地覆盖和土地利用发生变化,位于坦桑尼亚上部伟大的Ruaha子盆地。这影响了表面径流的大小,总水产量和地下水流动。本研究评估了陆地覆盖和土地利用变化对流流量和水文水平衡成分的影响(表面径流,水产量,渗透和实际蒸发抑制)。在QGIS版本2.6的帮助下,从Landsat TM和Oli_tirs创建了三个窗口周期快照,1990,2006和2017的土地使用和陆地覆盖(LULC)地图。监督分类用于使用最大似然算法和Kappa统计来生成Lulc映射,以评估准确性。 SWAT设置并运行以模拟物流和水文水平衡组分。通过比较2006年和2017年的土地利用方案对1990年的基线土地利用场景,通过比较SWAT模拟的水文参数对流动流量和水文平衡组分对流动流量和水文平衡组分的影响进行评估。LULC分类的准确性kappa统计数据均为0.9和0.99。与其他LULC相比,1990 - 2006年(5.84%)和2006-2017(12.05%),耕地面积覆盖率急剧增加。 2006年和2017年,表面径流分别增加了4%和9%;然而,与1990年基线期间相比,水产量仅增加0.5%。这归因于子集中中的耕地比例增加,其具有高曲线数(59.60),其表示径流响应较高和低渗透率。

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