4.6 Article

Sub-basin prioritisation using RUSLE in a Mountainous River Basin of Uttarakhand (India)

Journal

Publisher

SPRINGER
DOI: 10.1007/s10668-023-02989-5

Keywords

Flash floods; Soil erosion; RUSLE; GIS; Sub-basin prioritisation; Qualitative analysis

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This study assesses the soil erosion rate in various sub-basins of the Alaknanda using the revised universal soil-loss equation (RUSLE) in the GIS framework. The results show that out of the twelve sub-basins, two fall in the high erosional class, nine fall in the moderate erosional class, and one basin in the low erosional class. This study can assist decision-makers in prioritizing actions for water and soil conservation.
In a mountainous basin, flash-flood-induced soil erosion and its assessment are of major concern to the researchers. Cloudburst-induced extreme rainfall, undulating terrain, and inadequate water and soil conservation practices aggravate the problem of soil erosion. Alaknanda, a major basin of the upper Ganges in India, has experienced several incidents of flash floods. These have resulted in heavy soil loss, water siltation, and pollution in the basin. This study uses the revised universal soil-loss equation (RUSLE) in the GIS framework to assess the soil loss rate in various sub-basins of the Alaknanda. Further, the study suggests sub-basin prioritisation based on high soil erosion rate and past vulnerability that need attention of the decision-makers. RUSLE, an empirical soil erosion model, is easy to comprehend physically, involves minimum resources, and works on readily available inputs. The parameters used in the assessment include R-Rainfall Erosivity, Cover Management-C, Topographic-LS, Conservation Practice-P, and Soil Erodibility-K. The average R, K, LS, C & P factors for the Alaknanda basis are estimated as 437 MJ mm/ha/yr., 0.07 t ha h MJ-1 ha-1 mm-1, 1.4, 0.7, and 0.62, respectively. The mean annual soil erosion rate in the sub-basins varies from 6 to 27.9 t /ha/year with a mean rate of 13.4 t/ha/year and total erosion of 13.7 Mt/year. The results show that out of the twelve sub-basins, two (WS7 and WS5) fall in the high erosional class (18-30 t/ha/year), nine fall in the moderate erosional class (7-18 t /ha /year) and one basin in the low erosional class (1.0-7.0 t /ha/year). It is hoped that the present study will be helpful to the decision-makers while prioritising the actions to be taken for the water and soil conservation purposes.

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