{"title":"基于遥感和GIS的流域侵蚀计量分析:以埃塞俄比亚塔纳子流域盖尔达流域为例","authors":"Dessie Wubetu Melsse, Moges Animut Tegegne, Yitbarek Andualem Mekonnen, Yilak Taye Bihon","doi":"10.1007/s13201-025-02525-y","DOIUrl":null,"url":null,"abstract":"<div><p>Understanding the status of watershed erosion is essential for effective watershed management and sustainable water resources utilization. This study aimed to determine the erosion vulnerability of the Gelda entire watershed and its 26 sub-watersheds within the Tana sub-basin, Ethiopia, using hypsometric analysis. The data analysis began processing a 12.5 m by 12.5 m digital elevation model (DEM) in ArcGIS 10.5 to delineate 26 sub-watersheds from WS-1 to WS-26 and extract the DEM of each of the watersheds. Subsequently, the hypsometric curve and integral (HI) were computed for the entire Gelda watershed and its 26 sub-watersheds. The result indicates the entire watershed has an HI of 0.49, which is a mature stage, and the sub-watersheds range from 0.4 for WS-7 to .51 for WS-5 and WS-21, revealing varying degrees of erosion vulnerability. The watershed with higher HI values correlated with a youthful, erosion-prone landscape, whereas the sub-watershed (WS-7) with an HI value of 0.4 revealed that this sub-watershed is a relatively more mature and stable landscape. The coefficient of determination (R2) exceeds 0.5, confirming the robustness of the hypsometric curves in accurately representing topographic features. This is aligned with a similar study conducted by Raja Shekar (Watershed Ecol Environ 6:13–25, 2024). The study highlights the practical application of hypsometric analysis for regional watershed erosion conservation. It enables prioritizing the soil conservation measures, including tracing and check dams in high erosion watersheds like WS-5 and WS-21, and encourages groundwater recharge mechanisms for watersheds like WS-7. Moreover, this study provides essential information for planning and implementing targeted interventions such as afforestation in stable zones and structural erosion control measures in susceptible areas. These are critical in reducing erosion risks and enhancing sustainable land use planning within the Gelda watersheds. This study offers an essential outline for generating appropriate information in similar data scarcity basins and offers insights into basin dynamics and efficient management, emphasizing the necessity of targeted investments to mitigate erosion and maintain ecological balance.</p></div>","PeriodicalId":8374,"journal":{"name":"Applied Water Science","volume":"15 9","pages":""},"PeriodicalIF":5.7000,"publicationDate":"2025-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s13201-025-02525-y.pdf","citationCount":"0","resultStr":"{\"title\":\"Evaluating watershed erosion through hypsometric analysis with remote sensing and GIS: a case of gelda watershed, Tana Sub-Basin, Ethiopia\",\"authors\":\"Dessie Wubetu Melsse, Moges Animut Tegegne, Yitbarek Andualem Mekonnen, Yilak Taye Bihon\",\"doi\":\"10.1007/s13201-025-02525-y\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Understanding the status of watershed erosion is essential for effective watershed management and sustainable water resources utilization. This study aimed to determine the erosion vulnerability of the Gelda entire watershed and its 26 sub-watersheds within the Tana sub-basin, Ethiopia, using hypsometric analysis. The data analysis began processing a 12.5 m by 12.5 m digital elevation model (DEM) in ArcGIS 10.5 to delineate 26 sub-watersheds from WS-1 to WS-26 and extract the DEM of each of the watersheds. Subsequently, the hypsometric curve and integral (HI) were computed for the entire Gelda watershed and its 26 sub-watersheds. The result indicates the entire watershed has an HI of 0.49, which is a mature stage, and the sub-watersheds range from 0.4 for WS-7 to .51 for WS-5 and WS-21, revealing varying degrees of erosion vulnerability. The watershed with higher HI values correlated with a youthful, erosion-prone landscape, whereas the sub-watershed (WS-7) with an HI value of 0.4 revealed that this sub-watershed is a relatively more mature and stable landscape. The coefficient of determination (R2) exceeds 0.5, confirming the robustness of the hypsometric curves in accurately representing topographic features. This is aligned with a similar study conducted by Raja Shekar (Watershed Ecol Environ 6:13–25, 2024). The study highlights the practical application of hypsometric analysis for regional watershed erosion conservation. It enables prioritizing the soil conservation measures, including tracing and check dams in high erosion watersheds like WS-5 and WS-21, and encourages groundwater recharge mechanisms for watersheds like WS-7. Moreover, this study provides essential information for planning and implementing targeted interventions such as afforestation in stable zones and structural erosion control measures in susceptible areas. These are critical in reducing erosion risks and enhancing sustainable land use planning within the Gelda watersheds. 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引用次数: 0
摘要
了解流域侵蚀现状对流域有效管理和水资源可持续利用至关重要。本研究旨在利用半计量分析方法确定埃塞俄比亚塔纳子流域内盖尔达整个流域及其26个子流域的侵蚀脆弱性。数据分析开始在ArcGIS 10.5中处理一个12.5 m × 12.5 m的数字高程模型(DEM),从WS-1到WS-26划分出26个子流域,并提取每个流域的DEM。随后,计算了整个Gelda流域及其26个子流域的等高曲线和积分(HI)。结果表明,整个流域的HI为0.49,处于成熟阶段,子流域的WS-7至WS-7为0.4。51的WS-5和WS-21,揭示不同程度的侵蚀脆弱性。高HI值的流域为年轻的易侵蚀景观,而高HI值为0.4的WS-7子流域为相对成熟稳定的景观。决定系数(R2)超过0.5,证实了等高曲线在准确表征地形特征方面的稳健性。这与Raja Shekar进行的类似研究(Watershed Ecol Environ 6:13 - 25,2024)相一致。本研究强调了假设分析在区域流域侵蚀保护中的实际应用。它可以优先考虑土壤保持措施,包括在WS-5和WS-21等高侵蚀流域追踪和检查水坝,并鼓励WS-7等流域的地下水补给机制。此外,该研究还为规划和实施有针对性的干预措施(如稳定区造林和易感区结构侵蚀控制措施)提供了重要信息。这对于减少侵蚀风险和加强盖尔达流域的可持续土地利用规划至关重要。该研究为在类似的数据稀缺盆地中产生适当的信息提供了基本的轮廓,并为流域动态和有效管理提供了见解,强调了有针对性的投资以减轻侵蚀和维持生态平衡的必要性。
Evaluating watershed erosion through hypsometric analysis with remote sensing and GIS: a case of gelda watershed, Tana Sub-Basin, Ethiopia
Understanding the status of watershed erosion is essential for effective watershed management and sustainable water resources utilization. This study aimed to determine the erosion vulnerability of the Gelda entire watershed and its 26 sub-watersheds within the Tana sub-basin, Ethiopia, using hypsometric analysis. The data analysis began processing a 12.5 m by 12.5 m digital elevation model (DEM) in ArcGIS 10.5 to delineate 26 sub-watersheds from WS-1 to WS-26 and extract the DEM of each of the watersheds. Subsequently, the hypsometric curve and integral (HI) were computed for the entire Gelda watershed and its 26 sub-watersheds. The result indicates the entire watershed has an HI of 0.49, which is a mature stage, and the sub-watersheds range from 0.4 for WS-7 to .51 for WS-5 and WS-21, revealing varying degrees of erosion vulnerability. The watershed with higher HI values correlated with a youthful, erosion-prone landscape, whereas the sub-watershed (WS-7) with an HI value of 0.4 revealed that this sub-watershed is a relatively more mature and stable landscape. The coefficient of determination (R2) exceeds 0.5, confirming the robustness of the hypsometric curves in accurately representing topographic features. This is aligned with a similar study conducted by Raja Shekar (Watershed Ecol Environ 6:13–25, 2024). The study highlights the practical application of hypsometric analysis for regional watershed erosion conservation. It enables prioritizing the soil conservation measures, including tracing and check dams in high erosion watersheds like WS-5 and WS-21, and encourages groundwater recharge mechanisms for watersheds like WS-7. Moreover, this study provides essential information for planning and implementing targeted interventions such as afforestation in stable zones and structural erosion control measures in susceptible areas. These are critical in reducing erosion risks and enhancing sustainable land use planning within the Gelda watersheds. This study offers an essential outline for generating appropriate information in similar data scarcity basins and offers insights into basin dynamics and efficient management, emphasizing the necessity of targeted investments to mitigate erosion and maintain ecological balance.