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首页> 外文期刊>Geomorphologie >Water erosion in South-Western Niger: impacts of natural and anthropogenic factors on soil losses
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Water erosion in South-Western Niger: impacts of natural and anthropogenic factors on soil losses

机译:尼日尔西南部水土流失:自然和人为因素对土壤流失的影响

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摘要

This study was conducted in the extreme south-western of Niger, at the scale of the Kori Ouallam watershed. It proposes to assess the potential soil losses induced by water erosion in connection with natural constraints and anthropization. The methodology adopted involves field campaigns, laboratory analyses confronted with the tools composed of the Geographic Information System (GIS), remote sensing and the Revised Universal Soil Loss Equation (RUSLE). The use of these data reveals that the annual average of potential soil losses generated by water erosion is 1.54 t/ha/yr. On the scale of the watershed, the erosion risk varies from a very low erosion rate (0-0.5 t/ha/yr) largely observed in the North to an extremely severe erosion rate (> 5 t/ha/yr) with an increasing gradient towards the South. The correlation matrix shows that topographical factors related to slope length (L) and slope steepness (S) are the main erosive factors influencing soil loss. Soil erodibility and erosivity of rainfall are secondary factors. The gradual degradation of soils by water erosion is also amplified by inappropriate human activities, which undermines the resilience of ecosystems and communities. In a Sahelian context marked by climatic uncertainties and strong anthropization, the regional pattern of soil erosive dynamics deserves more adequate monitoring for a sustainable management of natural resources.
机译:这项研究是在极端的进行尼日尔的西南部,在科瑞的规模Ouallam分水岭。潜在的土壤水蚀引起的损失与自然的约束和anthropization。面对现场活动,实验室分析与地理组成的工具信息系统(GIS)、遥感和修正的通用土壤流失方程(RUSLE)。使用这些数据显示,年平均潜在的土壤水所产生的损失侵蚀是1.54吨/公顷/年。分水岭,侵蚀的风险从一个不等侵蚀率低(0 - 0.5吨/公顷/年)很大程度上观察到北方的一个非常严重的侵蚀率(> 5吨/公顷/年)越来越梯度方向南方。地形因素与边坡长度(L)和坡度(S)是主要的侵蚀影响水土流失的因素。和降雨侵蚀力是次要的因素。逐渐退化的土壤被水侵蚀也放大了不合适的人吗活动,破坏了的弹性生态系统和社区。气候不确定性和强anthropization,区域模式的土壤侵蚀动力学更值得足够了监控的可持续管理自然资源。

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