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Assessing the effects of land use change on soil physical properties and hydrological processes in the sub-humid tropical environment of West Africa

机译:评估西非半湿热带环境中土地利用变化对土壤物理特性和水文过程的影响

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Land use is a key parameter in the hydrologic cycle. Tropical Africa is affected by intense land use change since decades, particularly deforestation and conversion to agricultural land. The aim of this study is to analyse the effects of land use change on the hydrologic processes and soil physical properties in a small catchment (Aguima catchment) in central Benin. Results from ped-ological, pedobiological and hydrological investigations within the Aguima catchment were taken into account. The effects of land use change on hydrologic processes were analysed by comparing two sub-catchments of the Aguima catchment with different land use (savannah/forest and agricultural land use). The study is part of the GLOWA IMPETUS project, which examines the effects of global change on the water cycle and water availability on a regional scale in Morocco and Benin. The investigations of this study revealed that due to reduced activity of the macrofauna the infiltration capacity is significantly lower in cultivated soils than in savannah and forest. This causes higher surface runoff and soil loss rates, which was also determined on erosion plots. The increased soil loss on fields has effects on soil physical properties like increase of gravel content and reduction of field capacity. The impact of reduced vegetation cover on the soil water dynamics was examined with soil moisture measurements on different land use. Due to higher evapotranspiration and water withdrawal the soil water content on forest and savannah plots was lower than on agricultural fields. The difference in the water yield of the forested and cultivated catchments was over 120 mm in the dry year 2001 and about 70 mm in the wetter year 2002.
机译:土地利用是水文循环中的关键参数。自几十年来以来,热带非洲一直受到土地用途的剧烈变化的影响,特别是森林砍伐和向农田转化。这项研究的目的是分析贝宁中部小流域(阿吉马流域)土地利用变化对水文过程和土壤物理特性的影响。考虑了阿吉马流域内的生态学,生态学和水文调查的结果。通过比较阿吉玛流域的两个子流域与不同土地利用(大草原/森林和农业土地利用)的关系,分析了土地利用变化对水文过程的影响。这项研究是GLOWA IMPETUS项目的一部分,该项目研究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。这项研究的调查表明,由于大型动物的活动减少,在耕种土壤中的渗透能力明显低于在大草原和森林中。这会导致更高的地表径流和土壤流失率,这也是在侵蚀图上确定的。田间土壤流失量的增加会影响土壤物理性质,例如增加砾石含量和降低田间持水量。通过不同土地利用下的土壤湿度测量,研究了植被减少对土壤水分动力学的影响。由于较高的蒸散量和取水量,森林和大草原地块的土壤含水量低于农田。在干旱的2001年,森林和耕作流域的水产量差异超过120毫米,而在潮湿的2002年,差异约为70毫米。

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