首页> 外文会议>International Soil Conservation Organization Conference vol.2; 20020526-31; Beijing(CN) >Simultaneous Quantification of Wind and Water Erosions within Small Grazing Sahelian Catchments (Burkina Faso - West Africa)
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Simultaneous Quantification of Wind and Water Erosions within Small Grazing Sahelian Catchments (Burkina Faso - West Africa)

机译:萨赫勒小牧区(布基纳法索-西非)内风蚀和水蚀的同时定量

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Wind and water erosions were measured simultaneously during the 2001 rainy season in northern Burkina Faso where the climate is typically Sahelian. In order to obtain measurement on exactly the same surface area, two small catchments fitting together were chosen (BV1 = 1.4 and BV2 = 0.3 ha). They are part of the grazing area of the village land and differ by their soil types and surface features. Wind blown sediment budget was obtained by using 35 masts equipped with BSNE sand traps placed on the boundaries of the catchments. Water erosion was estimated at the outlets of the two catchments by discrete sampling for suspension and by sediment trap for bedload. Wind blown sediment balance appeared to be highly positive (+32 Mg ha~(-1) yr~(-1)) for the upstream catchment (BV2) and negative (-12 Mg ha~(-1) yr~(-1)) for the downstream part of BV1 (BV1-BV2). These differences are attributed to the differences in surface features. Quantities of soil lost by water erosion are quite the same for the 2 catchments (about 5 Mg ha~(-1) yr~(-1)), but differ in sediment size distribution and type of transportation: coarse sediments transported mainly in bedload for BV2 and fine sediments transported in suspension for BV1. As for wind erosion, such differences are related to the soil surface type. These results point out at the same time the importance of spatial variability in erosion for naturally grazed area of Sahel and the need to consider both wind and water erosions to study land degradation in this region.
机译:在布基纳法索北部的2001年雨季期间,同时测量了风蚀和水蚀,那里的气候通常为萨赫勒地区。为了在完全相同的表面积上获得测量值,选择了两个小流域,它们相互配合(BV1 = 1.4和BV2 = 0.3 ha)。它们是村庄土地的放牧区域的一部分,其土壤类型和表面特征也不同。风吹沉积物的预算是通过使用35个配有BSNE捕沙器的桅杆获得的,该桅杆位于集水区的边界。通过离散采样的悬浮液和沉积物的沉降量估算了两个流域出口的水蚀。风吹沉积物平衡对于上游集水区(BV2)表现为高度正(+32 Mg ha〜(-1)yr〜(-1)),而负值(-12 Mg ha〜(-1)yr〜(-1) ))用于BV1(BV1-BV2)的下游部分。这些差异归因于表面特征的差异。两个集水区因水蚀而流失的土壤数量基本相同(约5 Mg ha〜(-1)yr〜(-1)),但沉积物的大小分布和运输类型不同:粗颗粒沉积物主要在床荷中运输BV2和悬浮在BV1中的精细沉积物。至于风蚀,这种差异与土壤表面类型有关。这些结果同时指出了萨赫勒地区自然放牧区侵蚀空间变异性的重要性,并需要考虑风蚀和水蚀研究该地区的土地退化。

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