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Integration of geospatial technologies with RUSLE for analysis of land use/cover change impact on soil erosion: case study in Rib watershed, north-western highland Ethiopia

机译:地理空间技术与RUSLE的集成,用于分析土地利用/覆盖变化对土壤侵蚀的影响:埃塞俄比亚西北高地Rib流域的案例研究

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In recent times, soil erosion interlocked with land use and land cover (LULC) changes has become one of the most important environmental issues in developing countries. Evaluation of this complex interaction between LULC change and soil erosion is indispensable in land use planning and conservation works. This paper analysed the impact of LULC change on soil erosion in the north-western highland Ethiopia over the period 1986-2016. Rib watershed, the area with dynamic LULC change and severe soil erosion problem, was selected as a case study site. Integrated approach that combined geospatial technologies with revised universal soil loss equation model was utilized to evaluate the spatio-temporal dynamics of soil loss over the study period. Pixel-based overlay of soil erosion intensity maps with LULC maps was carried out to understand the change in soil loss due to LULC change. Results showed that the annual soil loss in the study area varied from 0 to 236.5 t ha(-1) year(-1) (tons per hectare per year) in 1986 and 0-807 t ha(-1) year(-1) in 2016. The average annual soil loss for the entire watershed was estimated about 40 t ha(-1) year(-1) in 1986 comparing with 68 t ha(-1) year(-1) in 2016, a formidable increase. Soil erosion potential that was estimated to exceed the average soil loss tolerance level increased from 34.5% in 1986 to 66.8% in 2016. Expansion of agricultural land at the expense of grassland and shrubland was the most detrimental factor for severe soil erosion in the watershed. The most noticeable change in soil erosion intensity was observed from cropland with mean annual soil loss amount increased to 41.38 t ha(-1) year(-1) in 2016 from 26.60 in 1986. Moreover, the most successive erosion problems were detected in eastern, south-eastern and northern parts of the watershed. Therefore, the results of this study can help identify the soil erosion hot spots and conservation priority areas at local and regional levels.
机译:近年来,水土流失与土地利用和土地覆被(LULC)的变化联系在一起,已成为发展中国家最重要的环境问题之一。在土地利用规划和保护工作中,对土地利用变化和土地利用变化与土壤侵蚀之间这种复杂相互作用的评估是必不可少的。本文分析了1986-2016年期间埃塞俄比亚西北高地土地利用,土地利用变化对土壤侵蚀的影响。肋骨流域,LULC动态变化和严重的土壤侵蚀问题,被选为案例研究地点。利用地理空间技术与修正的通用土壤流失方程模型相结合的综合方法来评估研究期间土壤流失的时空动态。进行了基于像素的土壤侵蚀强度图与LULC叠加图,以了解由于LULC变化导致的土壤流失变化。结果表明,研究区的年土壤流失量从1986年的0到236.5 t ha(-1)年(-1)(吨每公顷每年)和0-807 t ha(-1)年(-1)不等。 )在2016年。整个流域的年均土壤流失量估计在1986年约为40 t ha(-1)年(-1),而2016年为68 t ha(-1)年(-1),这是一个巨大的增长。估计超过平均水土流失耐受水平的土壤侵蚀潜力从1986年的34.5%增加到2016年的66.8%。以流失草地和灌木丛为代价的农业用地扩张是流域严重土壤侵蚀的最不利因素。在农田中,土壤侵蚀强度变化最为明显,年平均土壤流失量从1986年的26.60增加到2016年的41.38 t ha(-1)year(-1)。此外,东部地区发现了最连续的侵蚀问题,分水岭的东南和北部。因此,这项研究的结果可以帮助确定地方和区域层面的水土流失热点和保护重点地区。

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