基于RUSLE/RUSLE-径流模型的阿尔及利亚Wadi Saida流域潜在土壤流失评价

Kessar Cherif, Nasrallah Yahia, Blissag Bilal
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引用次数: 3

摘要

土壤退化已成为一个主要的世界范围的环境问题,特别是在干旱和半干旱气候区,由于不规律的降雨和频繁产生严重洪水的暴风雨强度。本研究的主要目的是利用地理信息系统和遥感技术,通过修订的通用土壤流失方程模型和基于地表侵蚀径流的拟议模型,量化和绘制Wadi Saida流域(624 km2)的土壤流失量。结果分析表明,流域土壤流失量在0 ~ 1000 t/km2/年之间,为中高流失量。在盆地北部的西迪布克尔地区和Daia山脉;其特点是坡度陡,可达3000 t/km2/年。两种模型的相关性较好,R = 0.95, RMSE = 0.43;利用侵蚀面径流参数对流域土壤流失率进行估算是有效的。土壤侵蚀问题需要采取严肃的干预措施,特别是在有扰动和恶劣气候参数的流域。良好农业规范和森林保护区在土壤保持中发挥着重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Potential soil loss evaluation using the RUSLE/RUSLE-runoff models in Wadi Saida watershed (N-W Algeria)
Soil degradation has become a major worldwide environmental problem, particularly in arid and semi-arid climate zones due to irregular rainfall and the intensity of storms that frequently generate heavy flooding. The main objective of this study is the use of geographic information system and remote sensing techniques to quantify and to map the soil losses in the Wadi Saida watershed (624 km2) through the revised universal soil loss equation model and a proposed model based on the surface erosive runoff. The results Analysis revealed that the Wadi Saida watershed showed moderate to moderately high soil loss, between 0 and 1000 t/km2/year. In the northern part of the basin in the region of Sidi Boubkeur and the mountains of Daia; which are characterized by steep slopes, values can reach up to 3000 t/km2/year. The two models in comparison showed a good correlation with R = 0.95 and RMSE = 0.43; the use of the erosive surface runoff parameter is effective to estimate the rate of soil loss in the watersheds. The problem of soil erosion requires serious interventions, particularly in basins with disturbances and aggressive climatic parameters. Good agricultural practices and forest preservation areas play an important role in soil conservation.
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