Assessment of Soil Erosion Hazards in Kambiti Subcatchment, Murang’a County, Kenya

Daniel Wachira Githinji, J. Obando, S. Murimi
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Abstract

Erosion is a global problem that destroys soil and adversely affects ecosystem productivity. Soil erosion generally involves many processes but the major activities involve particles being transported and deposited to another location. With an increasing population, soil erosion, water availability, energy production, and biodiversity loss are some of the most pressing environmental problems around the world. Erosion is a hazard associated with agriculture in tropical and semi-arid areas. Kambiti sub catchment is part of the upper Tana catchment. The upper Tana catchment includes 25% of Kenya gazette forest. A large area of land has been degraded, resulting in a drastic reduction in surface water availability during the dry season and poor-quality water during the wet season caused by high silt levels. The main objective of the study is to assess erosion hazards using RUSLE model in Kambiti sub catchment area, Murang’a County. The specific objectives of the study were to determine the effect of rainfall erosivity and soil erodibility factor in Kambiti Sub catchment area in Murang’a County, to determine  effect of slope factor to soil loss in Kambiti Sub-catchment area in Murang’a County, to determine the effect of crop protection and management factor in Kambiti Sub catchment area in Murang’a County to soil loss and to determine the strategies for management of soil and water in Kambiti Sub catchment area in Murang’a County. Data was collected from the catchment and analyzed using arc Geographical Information System to obtain the specific parameters in the revised universal soil loss equation model. Interpolation method was used to determine the mean annual precipitation. The k factor is a function of soil texture. Shape file for geological structure for Kenya was obtained from Kenya Agriculture and livestock Research Organisation and analyzed by use of arc GIS to obtain soil erodibility factor. The slope factor was analyzed using digital elevation model from arc view. Digital elevation model was gotten from STRM download. The C factor was derived from Landsat imagery from sentinel of 30metres by 30 metres. It was further analysed by unsupervised classification from Arc GIS. The sentinel clip of Kambiti sub-catchment was joined with ground trothing observations. The results were useful in estimation of soil loss therefore profiling the areas prone to soil loss. Study findings indicated rain drop impact and runoff were primarily responsible for causing erosion in Kambiti sub catchment. Anthropogenic factors played an important role in amplifying the severity of the damage, such as persistent vegetative degradation and destruction of soil structure due to organic matter depletion and routine shallow tillage. In recent years, erosion control has been hampered by the occurrence of gaps in knowledge regarding the integrated nature of erosion processes, leading to land damage caused by rill and inter-rill erosion going unaddressed. Poor people and those lacking capital to invest in reclaiming land are the main causes of abandoning degraded land. Through strategic awareness campaigns and education, soil erosion will be assessed and the knowledge gap will be closed. Participation of farmers in land use decisions is inevitable as it ensures that people who utilize land resources are recognized as equal partners in identifying problems and designing solutions. It was also recommended that Identification and operationalization of alternative off-farm income.  
肯尼亚穆郎阿县坎比蒂子流域土壤侵蚀危害评估
水土流失是一个全球性问题,它破坏土壤并对生态系统的生产力产生不利影响。土壤侵蚀通常涉及许多过程,但主要活动是将颗粒迁移并沉积到另一个地方。随着人口的不断增长,水土流失、水资源供应、能源生产和生物多样性丧失已成为全球最紧迫的环境问题。在热带和半干旱地区,水土流失是与农业相关的一种危害。坎比提子集水区是塔纳河上游集水区的一部分。塔纳河上游集水区包括 25% 的肯尼亚地名录森林。大片土地退化,导致旱季地表水供应量急剧下降,雨季因泥沙含量高而导致水质变差。本研究的主要目的是利用 RUSLE 模型评估穆朗阿县坎比蒂子集水区的侵蚀危害。研究的具体目标是确定穆朗阿县坎比蒂次级集水区降雨侵蚀性和土壤可侵蚀性因子的影响,确定坡度因子对穆朗阿县坎比蒂次级集水区土壤流失的影响,确定穆朗阿县坎比蒂次级集水区作物保护和管理因子对土壤流失的影响,并确定穆朗阿县坎比蒂次级集水区水土管理策略。从集水区收集数据,并使用弧形地理信息系统进行分析,以获得修订后的通用土壤流失方程模型中的具体参数。采用内插法确定年平均降水量。k 系数是土壤质地的函数。肯尼亚的地质结构形状文件来自肯尼亚农业和畜牧业研究组织,通过使用 arc GIS 进行分析,得出土壤侵蚀系数。坡度因子是利用弧形视图的数字高程模型进行分析的。数字高程模型从 STRM 下载。C 因子来自于 30 米乘 30 米的大地遥感卫星图像。通过 Arc GIS 的无监督分类对其进行了进一步分析。Kambiti 子流域的定点片段与地面观测数据相结合。研究结果有助于估算土壤流失量,从而确定土壤易流失的地区。研究结果表明,雨滴冲击和径流是造成坎比提子流域水土流失的主要原因。人为因素在加剧水土流失的严重程度方面发挥了重要作用,如有机质枯竭和日常浅耕造成的持续植被退化和土壤结构破坏。近年来,由于对水土流失过程的综合性质认识不足,水土流失控制工作受到了阻碍,导致垄沟和沟间侵蚀造成的土地破坏问题得不到解决。贫困人口和缺乏资金投资开垦土地的人是放弃退化土地的主要原因。通过战略性的宣传活动和教育,将对水土流失进行评估,缩小知识差距。农民参与土地使用决策是不可避免的,因为这可以确保土地资源的使用者在发现问题和制定解决方案时被视为平等的合作伙伴。还建议确定并实施替代性非农业收入。
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