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首页> 外文期刊>Geoscience frontiers >Assessment of soil erosion in a tropical mountain river basin of the southern Western Ghats, India using RUSLE and GIS
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Assessment of soil erosion in a tropical mountain river basin of the southern Western Ghats, India using RUSLE and GIS

机译:利用RUSLE和GIS评估印度西高止山脉南部热带山区河流流域的土壤侵蚀

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Revised Universal Soil Loss Equation (RUSLE) model coupled with transport limited sediment delivery (TLSD) function was used to predict the longtime average annual soil loss, and to identify the critical erosion-/deposition-prone areas in a tropical mountain river basin, viz., Muthirapuzha River Basin (MRB;?area?=?271.75?km 2 ), in the southern Western Ghats, India. Mean gross soil erosion in MRB is 14.36?t?ha ?1 ?yr ?1 , whereas mean net soil erosion (i.e., gross erosion–deposition) is only 3.60?t?ha ?1 ?yr ?1 (i.e., roughly 25% of the gross erosion). Majority of the basin area (~86%) experiences only slight erosion (<5?t?ha ?1 ?yr ?1 ), and nearly 3% of the area functions as depositional environment for the eroded sediments (e.g., the terraces of stream reaches, the gentle plains as well as the foot slopes of the plateau scarps and the terrain with concordant summits). Although mean gross soil erosion rates in the natural vegetation belts are relatively higher, compared to agriculture, settlement/built-up areas and tea plantation, the sediment transport efficiency in agricultural areas and tea plantation is significantly high, reflecting the role of human activities on accelerated soil erosion. In MRB, on a mean basis, 0.42?t of soil organic carbon (SOC) content is being eroded per hectare annually, and SOC loss from the 4th order sub-basins shows considerable differences, mainly due to the spatial variability in the gross soil erosion rates among the sub-basins. The quantitative results, on soil erosion and deposition, modelled using RUSLE and TLSD, are expected to be beneficial while formulating comprehensive land management strategies for reducing the extent of soil degradation in tropical mountain river basins. Graphical abstract Display Omitted Highlights ? We modeled soil loss from a tropical mountain river basin in the Western Ghats. ? Used RUSLE with TLSD concept to estimate actual soil erosion and deposition. ? Net soil erosion is only 25% of the gross soil erosion. ? Highlighted the importance of topography and vegetation on soil erosion.
机译:修正后的通用土壤流失方程(RUSLE)模型与有限运输输沙量(TLSD)函数一起用于预测长期平均年土壤流失,并确定热带山区河流盆地中易发生侵蚀/沉积的关键区域,即,位于印度西高止山脉南部的Muthirapuzha流域(MRB;?area?=?271.75?km 2)。 MRB的平均土壤总侵蚀为14.36?t?ha?1?yr?1,而平均净土壤侵蚀(即总侵蚀-沉积)仅为3.60?t?ha?1?yr?1(即大约25)。总侵蚀的百分比)。流域的大部分地区(〜86%)仅遭受轻微的侵蚀(<5?t?ha?1?yr?1),并且近3%的地区作为侵蚀沉积物的沉积环境(例如,河谷阶地)。溪流到达,平缓的平原以及高原陡峭的山脚坡和地形一致的山顶)。尽管天然植被带的平均土壤总侵蚀率相对较高,但与农业,定居/集聚区和茶园相比,农业区和茶园的泥沙输送效率显着较高,这反映了人类活动对加速水土流失。在MRB中,平均而言,每年每公顷土壤侵蚀的有机碳(SOC)含量为0.42?t,四阶次流域的SOC损失显示出很大的差异,这主要是由于总土壤的空间变异性子流域之间的侵蚀率。使用RUSLE和TLSD建模的关于土壤侵蚀和沉积的定量结果有望在制定综合土地管理策略以减少热带山区河流流域土壤退化程度的过程中有所帮助。图形摘要显示省略的突出显示?我们对西高止山脉的热带山区河流流域的土壤流失进行了建模。 ?使用带有TLSD概念的RUSLE来估算实际的土壤侵蚀和沉积。 ?净土壤侵蚀仅占土壤总侵蚀的25%。 ?强调了地形和植被对土壤侵蚀的重要性。

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