...
首页> 外文期刊>Environmental Geology >Relating soil erosion and sediment yield to geomorphic features and erosion processes at the catchment scale in the Spanish Pre-Pyrenees
【24h】

Relating soil erosion and sediment yield to geomorphic features and erosion processes at the catchment scale in the Spanish Pre-Pyrenees

机译:在西班牙比利牛斯山脉流域尺度上将土壤侵蚀和沉积物产量与地貌特征和侵蚀过程联系起来

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Erosion and sediment redistribution are important processes in landscape changes in the short and long term. In this study, the RMMF model of soil erosion and the SEDD model of sediment delivery were used to estimate annual soil loss and sediment yield in an ungauged catchment of the Spanish Pre-Pyrenees and results were interpreted in the context of the geomorphic features. The Estafia Catchment is divided into 15 endorheic sub-catchments and there are 17 dolines. Gullies and slopes were the main erosive geomorphic elements, whereas the colluvial, alluvial, valley floor, and doline deposits were depositional elements. Spatially distributed maps of gross soil erosion, sediment delivery ratio (SDR), and sediment yield (SY) were generated in a GIS. Severe erosion rates (>100 Mg ha"1 year"1) were found in gullies, whereas mean and maximum erosion rates were very high on slopes developed on Keuper Fades and high in soils on Muschelkalk Facies. Where crops are grown, the depositional-type geoforms were predicted by the models to have an erosive dynamic. Those results were consistent with the rates of erosion quantified by ~(137)Cs which reflects the significant role of human activities in triggering soil erosion. Catchment area was positively correlated with erosion rate, but negatively correlated with SDR and SY. The latter were negatively correlated with the proportion of the surface catchment covered with forests and scrublands. The topography of the area influenced the high SDR and SY in the dolines and valley floors near the sinks. Intra-basin stored sediment was 59.2% of the total annualrneroded soil in the catchment. The combination of the RMMF and SEDD models was an appropriate means of assessing the effects of land uses on soil erosion and obtaining a better understanding of the processes that underlie the geomorphic changes occurring in mountainous environments of the Mediterranean region.
机译:侵蚀和沉积物的重新分配是短期和长期景观变化的重要过程。在这项研究中,使用土壤侵蚀的RMMF模型和沉积物输送的SEDD模型来估算西班牙比利牛斯山脉未集水区的年土壤流失和沉积物产量,并根据地貌特征来解释结果。 Estafia集水区分为15个内分泌子集水区,共有17条do水线。沟壑和斜坡是主要的侵蚀性地貌元素,而冲积,冲积,谷底和floor石沉积物是沉积元素。在GIS中生成了土壤总侵蚀,沉积物输送比(SDR)和沉积物产量(SY)的空间分布图。在沟壑中发现了严重的侵蚀速率(> 100 Mg ha“ 1年” 1),而在库珀法德地区形成的斜坡上和穆斯克列克相地区的土壤中,平均和最大侵蚀速率非常高。在农作物生长的地方,模型预测的沉积型地貌具有侵蚀性。这些结果与〜(137)Cs定量的侵蚀速率相一致,后者反映了人类活动在引发土壤侵蚀中的重要作用。流域面积与侵蚀率呈正相关,与SDR和SY呈负相关。后者与被森林和灌木丛覆盖的表层集水区的比例负相关。该区域的地形影响了水槽附近的do线和谷底中的高SDR和SY。流域内流域内沉积的泥沙占每年被侵蚀土壤总量的59.2%。 RMMF模型和SEDD模型的组合是评估土地利用对土壤侵蚀的影响并更好地理解构成地中海地区山区环境中发生的地貌变化的过程的一种合适方法。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号