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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Sediment production in large gullies of the Mediterranean area (NE Spain) from high-resolution digital elevation models and geographical information systems analysis
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Sediment production in large gullies of the Mediterranean area (NE Spain) from high-resolution digital elevation models and geographical information systems analysis

机译:通过高分辨率数字高程模型和地理信息系统分析,在地中海地区(西班牙东北部)的大型沟壑中产生泥沙

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Recent studies in the Mediterranean area have shown gully erosion to have a very significant contribution to total soil loss. In the Penedes vineyard region (NE Spain), between 15 and 27% of the land is affected by large gullies and gully-wall retreat seems to be an ongoing process. Multi-date digital elevation model (DEM) analysis has allowed computation of sediment production by gully erosion, showing that the sediment production rates are very high by the, up-to-date, usual global standards. Here, we present a study carried out using large-scale multi-date (1975 and 1995) aerial photographs (1:5000 and 1:7000) to monitor sediment yield caused by large gullies in the Penedes region (NE Spain). High-resolution DEMs (1 m grid) were derived and analysed by means of geographical information systems techniques to determine the gully erosion rates. Rainfall characteristics within the same study period were also analysed in order to correlate with the soil loss produced. Mass movement was the main process contributing to total sediment production. This process could have been favoured by rainfalls recorded during the period: 58% of the events were of an erosive character and showed high kinetic energy and erosivity. A sediment production rate of 846 ± 40 Mg ha~(-1) year~(-1), a sediment deposition rate of 270 ± 18 Mg ha~(-1) year~(-1) and a sediment delivery ratio of 68.1% were computed for a gully area of 0.10 km~2. The average net erosion within the study period (1975-95) was 576 ± 58 Mg ha~(-1) year~(-1). In comparison with other methods, the proposed method also includes sediment produced by processes other than only overland flow, i.e. downcutting, headcutting, and mass movements and bank erosion.
机译:地中海地区最近的研究表明,沟壑侵蚀对土壤的总流失具有非常重要的作用。在Penedes葡萄园地区(西班牙东北部),有15%到27%的土地受到大型沟渠的影响,沟壁撤退似乎是一个持续的过程。多日期数字高程模型(DEM)分析已允许通过沟壑侵蚀来计算沉积物产量,表明按最新的通用全球标准,沉积物的生产率非常高。在这里,我们提出一项使用大型多日期(1975年和1995年)航空照片(1:5000和1:7000)进行的研究,以监测Penedes地区(西班牙东北部)由大型沟壑引起的沉积物产量。通过地理信息系统技术,导出并分析了高分辨率DEM(1 m网格),以确定沟壑侵蚀率。还对同一研究期间的降雨特征进行了分析,以与产生的土壤流失相关。群众运动是造成沉积物总产量的主要过程。该过程可能受到这段时期记录的降雨的支持:58%的事件具有侵蚀性,并显示出很高的动能和侵蚀性。沉积物产生速率为846±40 Mg ha〜(-1)年〜(-1),沉积物沉积速率为270±18 Mg ha〜(-1)年〜(-1)和沉积物输送率为68.1对于0.10 km〜2的沟壑面积,计算出%。研究期间(1975-95年)的平均净侵蚀量为576±58 Mg ha〜(-1)年〜(-1)。与其他方法相比,所提出的方法还包括除陆上流动以外的其他过程所产生的沉积物,即下切,head割,土石运动和河岸侵蚀。

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