Chasia Stanley, Olang Luke O, Bess Claudia, Kimuyu Jacinta, Sitoki Lewis
Department of Geosciences and the Environment, Technical University of Kenya (TU-K), Nairobi, Kenya; Department of Civil Engineering, Technical University of Kenya (TU-K), Nairobi, Kenya.
School of Chemical and Biological Systems Engineering, Technical University of Kenya (TU-K), Nairobi, Kenya; Centre for Integrated Water Resource Management, Technical University of Kenya (TU-K), Nairobi, Kenya.
J Environ Manage. 2024 Nov;370:122916. doi: 10.1016/j.jenvman.2024.122916. Epub 2024 Oct 15.
Persistent soil erosion poses a significant threat to water quality, ecosystem viability and soil health in many regions of the world. Addressing this challenge requires a comprehensive understanding of local soil erosion rates, including the identification of vulnerable areas, to facilitate effective and integrated environmental management. In East Africa, however, many affected regions are data poor and lack measured hydrological data from which soil erosion estimates can be derived. This study used the physically based Revised Universal Soil Loss Equation (RUSLE) model to estimate the annual rate of soil erosion in the transboundary Sio-Malaba-Malakisi catchment, straddling Kenya and Uganda. Soil erosion events were quantified by integrating input factors derived from physical datasets using a Geographical Information System (GIS). The Analytical Hierarchy Process (AHP) technique was then used to assess the importance of selected physical factors influencing the soil erosion process in order to identify regions of increasing environmental vulnerability. The results obtained indicate a wide range of soil erosion rates across the region, with an estimated mean annual rate of 250 t ha yr for the whole catchment. Upstream areas characterized by intensive agricultural activity had erosion rates of up to 2000 t ha yr, while downstream areas recorded erosion rates below 600 t ha yr. Areas with intensive agriculture, unprotected soils, and a soil loss tolerance value above 12 t ha yr were found to be most vulnerable. Rainfall and vegetation cover were identified as key factors influencing erosion susceptibility. Regions with soil erosion rates above 50 t ha yr were identified as high priority regions for targeted soil and water conservation measures. The identification of vulnerability zones, including the classification of their severity, provides an opportunity to prioritize sustainable environmental management interventions; a process that can be replicated for such affected regions elsewhere.
持续的土壤侵蚀对世界许多地区的水质、生态系统活力和土壤健康构成了重大威胁。应对这一挑战需要全面了解当地的土壤侵蚀速率,包括确定脆弱地区,以促进有效的综合环境管理。然而,在东非,许多受影响地区数据匮乏,缺乏可用于估算土壤侵蚀的实测水文数据。本研究使用基于物理过程的修正通用土壤流失方程(RUSLE)模型,估算了跨越肯尼亚和乌干达的跨境西奥-马拉巴-马拉基西集水区的年土壤侵蚀速率。通过使用地理信息系统(GIS)整合从物理数据集得出的输入因子,对土壤侵蚀事件进行了量化。然后使用层次分析法(AHP)评估影响土壤侵蚀过程的选定物理因子的重要性,以确定环境脆弱性增加的区域。所得结果表明,该地区的土壤侵蚀速率范围很广,整个集水区的年平均侵蚀速率估计为250吨/公顷·年。以集约农业活动为特征的上游地区侵蚀速率高达2000吨/公顷·年,而下游地区的侵蚀速率低于600吨/公顷·年。发现集约农业、无保护土壤且土壤流失容忍值高于12吨/公顷·年的地区最为脆弱。降雨和植被覆盖被确定为影响侵蚀敏感性的关键因素。土壤侵蚀速率高于50吨/公顷·年的地区被确定为有针对性的水土保持措施的高优先区域。确定脆弱区域,包括对其严重程度进行分类,为优先开展可持续环境管理干预措施提供了机会;这一过程可在其他此类受影响地区复制。