...
首页> 外文期刊>Geomorphology >Effects of soil surface components on soil hydrological behaviour in a dry Mediterranean environment (Southern Spain)
【24h】

Effects of soil surface components on soil hydrological behaviour in a dry Mediterranean environment (Southern Spain)

机译:地中海干燥环境中土壤表面成分对土壤水文行为的影响(西班牙南部)

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

Various researchers have studied the spatial pattern of soil surface components such as vegetation, rock fragments, bare soil, litter and surface crusts, as a key factor of hydrological behaviour in Mediterranean settings with heterogeneous patches of vegetation cover and strong human impact. The studies indicate that there is a mosaic of patches that generate run-off or infiltrate overland flow, distributed in various ways along hillslopes. Few of these studies, however, have looked at areas underlain by metamorphic rocks such as phyllites or schists. This study analysed the temporal and spatial variability of the effects of soil surface components on hydrological processes in a small dry Mediterranean catchment underlain by metamorphic rocks. A systematic sampling of multiple sites throughout a hydrological year was carried out. We related the hydrological behaviour of soil surface components to 1) their position along the hillslope, 2) the distance of existing vegetation tussocks from the line of run-off, 3) rainfall intensity and 4) the main physical/chemical soil properties affecting infiltration processes. Statistical analysis was used to check the validity of the relationships. The results show that soil surface components have highly variable effects, in both space and time, on soil hydrologica! behaviour. These effects particularly depend on the location along the line of maximum slope and the intensity of preceding rainfall, whose interaction defines soil hydrological status. These results are similar to those for other Mediterranean settings with different lithology, in that the succession of contributing patches are hydrologically interconnected along a hillslope. The variables used and the grouping of explanatory variables through principal component analyses were found to be suitable for discussing the spatial distribution of soil surface components in the hydrologically dynamic environment of the study area.
机译:各种各样的研究人员已经研究了土壤表面成分的空间格局,例如植被,岩石碎片,裸露的土壤,垃圾和地壳,这是地中海环境中水文行为的关键因素,植被覆盖的异质性和人类的强烈影响。研究表明,沿山坡分布着各种斑块的马赛克会产生径流或渗入的陆上水流。但是,这些研究中很少有人研究变质岩(如千枚石或片岩)下垫的区域。这项研究分析了在变质岩层下的地中海小干燥流域中,土壤表面成分对水文过程的影响的时空变化。在整个水文年中对多个站点进行了系统采样。我们将土壤表面成分的水文行为与1)它们在山坡上的位置,2)现有植被丛距径流线的距离,3)降雨强度和4)影响入渗的主要物理/化学土壤特性相关联流程。使用统计分析来检查关系的有效性。结果表明,土壤表层成分在时空上对土壤水文状况具有高度可变的影响!行为。这些影响尤其取决于沿最大坡度线的位置和先前降雨的强度,前者的相互作用决定了土壤水文状况。这些结果与其他具有不同岩性的地中海环境的结果相似,因为一系列贡献斑块沿山坡在水文上相互联系。通过主成分分析发现所使用的变量和解释变量的分组适合于讨论研究区域水文动态环境中土壤表面成分的空间分布。

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