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Analysis of the hydrological processes in a small headwater catchment in Benin (West Africa)

机译:贝宁(西非)小源头流域的水文过程分析

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This paper analyzes the hydrological processes and the impact of soil properties and land use on these processes in tropical headwater catchment in the sub-humid part of Benin (West-Africa), the Aguima catchment. The presented study is integrated in the GLOWA IMPETUS project, which investigates the effects of global change on the water cycle and water availability on a regional scale in Morocco and Benin. The lack of field investigations concerning soil and surface hydrology in the Benin research area necessitates detailed field measurements including measurements of discharge, soil water dynamics, soil physical properties etc. on the local scale in order to understand the dominant runoff generation processes and its influencing factors. This is a pre-requisite to be able to forecast the effects which global change has on hydrological processes and water availability in the region. The paper gives an overview over the hydrologic measuring concept of the IMPETUS-Benin project focusing on measurements concerning the soil saturated conductivity ksat and discharge behaviour of two different sub-catchment of the Aguima catchment. The results of ksat measurements revealed that interflow is the dominant runoff process on the hillslopes of the investigated catchment. Concerning the impact of land use on the hydrological processes infiltration experiments showed that infiltration rates were reduced on cultivated land compared to natural land cover. This results in significant differences in runoff behaviour and runoff ratios while comparing natural and agricultural used catchments.
机译:本文分析了贝宁(西非)半湿润地区,阿吉马流域的热带水源流域的水文过程以及土壤性质和土地利用对这些过程的影响。提出的研究被整合到GLOWA IMPETUS项目中,该项目调查了摩洛哥和贝宁区域范围内全球变化对水循环和水供应的影响。贝宁研究区缺乏有关土壤和地表水文学的实地调查,因此需要详细的实地测量,包括在地方尺度上进行流量,土壤水动力学,土壤物理性质等的测量,以了解主要的径流产生过程及其影响因素。 。这是能够预测全球变化对该地区水文过程和水供应的影响的前提。本文概述了IMPETUS-Benin项目的水文测量概念,重点是有关土壤饱和电导率ksat和阿吉玛流域两个不同子流域的排水特性的测量。 ksat测量结果表明,在被调查流域的山坡上,内流是主要的径流过程。关于土地利用对水文过程的影响,入渗实验表明,与自然土地覆盖相比,耕地的入渗率降低了。在比较自然和农业用流域时,这将导致径流行为和径流比的显着差异。

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