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土地利用/土地覆被变化对埃塞俄比亚奥莫河吉贝流域威尼凯流域土壤侵蚀和泥沙输送的影响。

Land use/land cover change effect on soil erosion and sediment delivery in the Winike watershed, Omo Gibe Basin, Ethiopia.

机构信息

Center for Environmental Science, College of Natural and Computational Science, Addis Ababa University, P.O. Box 1176, Addis Ababa, Ethiopia; Department of Natural Resource Management, College of Agriculture and Natural Resource, Wolkite University, P.O. Box 07, Wolkite, Ethiopia.

Center for Environmental Science, College of Natural and Computational Science, Addis Ababa University, P.O. Box 1176, Addis Ababa, Ethiopia.

出版信息

Sci Total Environ. 2020 Aug 1;728:138776. doi: 10.1016/j.scitotenv.2020.138776. Epub 2020 Apr 19.

Abstract

Information on soil loss and sediment export is essential to identify hotspots of soil erosion to inform conservation interventions in a given watershed. This study investigates the dynamics of soil loss and sediment export associated with land-use/land cover changes and identifying soil loss hotspot areas in the Winike watershed of the Omo-Gibe Basin of Ethiopia. Spatial data collected from satellite images, topographic maps, meteorological and soil data were analyzed. The land-use types in the study area were categorized into six: cultivated land, woodland, forest, grazing, shrubland, and bare land. The Integrated Valuation of Ecosystem Services and Tradeoffs (InVEST) of the sediment delivery ratio (SDR) model was used based on the analysis of land use/land cover and RUSLE factors. The results show that total soil loss increased from 774.86 thousand tons in 1988 to 951.21 thousand tons in 2018 while the corresponding sediment export increased by 3.85 thousand tons for the same period. These were subsequently investigated in each land-use type. Cultivated fields generated the highest soil erosion rate, increasing from 10.02 t/ha/year in 1988 to 43.48 t/ha/year in 2018 when compared with the grazing, shrub, forest, wood land and bare land-use types. This corresponds with the expansion of the cultivated area. This is logical as the correlation between soil loss and sediment delivery and expansion of cultivated area is highly significant (p < 0.001). Sub-watershed six (SW-6) showed the highest soil loss (23.17 t/ha/year) while sub-watershed two (SW- 2) has the lowest soil loss (5.54 t/ha/year). This is because SW-2 is situated in the lower reaches of the watershed under dense vegetation cover experiencing less erosion. The findings on the erosion hotspots presented in this study allow prioritizing the segments of the watershed that need immediate application of improved management interventions and informed decision-making processes.

摘要

土壤流失和泥沙输出信息对于确定特定流域的水土流失热点至关重要,以便为保护干预措施提供信息。本研究调查了与土地利用/土地覆被变化相关的土壤流失和泥沙输出动态,并确定了埃塞俄比亚奥莫-吉贝流域威尼克流域的土壤流失热点地区。从卫星图像、地形地图、气象和土壤数据中收集了空间数据。研究区域的土地利用类型分为六种:耕地、林地、森林、放牧、灌木林和裸地。基于土地利用/土地覆被和 RUSLE 因子分析,使用了综合生态系统服务和权衡评估(InVEST)的泥沙输送比(SDR)模型。结果表明,总土壤流失量从 1988 年的 774.86 万吨增加到 2018 年的 951.21 万吨,同期相应的泥沙输出量增加了 3.85 万吨。随后对每种土地利用类型进行了调查。耕地产生的土壤侵蚀率最高,从 1988 年的 10.02 吨/公顷/年增加到 2018 年的 43.48 吨/公顷/年,与放牧、灌木、森林、林地和裸地利用类型相比。这与耕地面积的扩大相对应。这是合乎逻辑的,因为土壤流失和泥沙输送与耕地面积的扩大之间的相关性具有高度显著性(p<0.001)。第六个子流域(SW-6)的土壤流失量最高(23.17 吨/公顷/年),而第二个子流域(SW-2)的土壤流失量最低(5.54 吨/公顷/年)。这是因为 SW-2 位于流域下游,植被茂密,受到的侵蚀较少。本研究中提出的侵蚀热点的发现,可以优先考虑流域的各个部分,需要立即应用改进的管理干预措施,并为决策过程提供信息。

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