Assessment of soil erosion in a tropical mountain river basin of the southern Western Ghats, India using RUSLE and GIS

被引:136
|
作者
Thomas, Jobin [1 ,2 ]
Joseph, Sabu [2 ]
Thrivikramji, K. P. [3 ]
机构
[1] Indian Inst Technol, Dept Civil Engn, EWRE, Madras 600036, Tamil Nadu, India
[2] Univ Kerala, Dept Environm Sci, Thiruvananthapuram 695581, Kerala, India
[3] Ctr Environm & Dev, Thiruvananthapuram 695013, Kerala, India
关键词
Soil erosion; RUSLE; Transport limited sediment delivery; Muthirapuzha river basin; Western Ghats; Kerala; LOSS EQUATION RUSLE; SEDIMENT YIELD; PRECIPITATION DATA; CATCHMENT-SCALE; MODEL; RISK; DEPOSITION; VEGETATION; PATTERNS; IMPACT;
D O I
10.1016/j.gsf.2017.05.011
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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 erosionedeposition) is only 3.60 t ha(-1) yr(-1) (i.e., roughly 25% of the gross erosion). Majority of the basin area (similar to 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. (C) 2018, China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license.
引用
收藏
页码:893 / 906
页数:14
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