Abstract

Due to uninterrupted erosion and transportation, huge volume of sediments carried away by streams and rivers are finally deposited on the meanders, lakes, and reservoirs when the velocity of the surface water flow decreases. Kulfo River in the southern part of Ethiopia faces a challenge due to massive deposit of sediments. Hydrometeorological and spatial data of Kulfo watershed from the observed stream flow data series near Kulfo bridge and four meteorological station data were used to assess the depositional environment of Kulfo watershed. The data length covers the period from 2000 to 2019. Geomorphic parameters of the watershed were developed by using a 30m × 30m digital elevation model (DEM). The spatial distribution of sediment yield of the study area was estimated using SWAT, the soil and water assessment tool. Scenarios were developed to assess the effectiveness of watershed management interventions provided at the watershed and critical subwatershed level. The model genuinely replicated the observed discharge and sediment with an overall performance of 0.75 as measured by NSE. Twenty-one subbasins were created, and the observed average sediment yield was calculated as 11.9 ton/ha/y. The observed average sediment yield reduction at the hotspot subwatershed level postapplication of contouring, filter strip, terracing, and strip cropping were 40.79%, 57.94%, 66.02%, and 62.93%, respectively. By intricately analyzing, it can be referred that terracing is the best conservation measure to be incorporated into the affected subbasins.

Highlights

  • Loss of soil is a natural geological denudation practice of detachment of upper soil by natural agencies like water, wind, glacier, and tidal effects though some anthropogenic interference cannot be ruled out

  • To get the spatial distribution of average sediment yield annually at the subbasin level, the soil and water assessment tools (SWAT) model was run by using twenty-four years (2000–2019) hydrometeorological data. e spatial distribution of sediment yield of Kulfo watershed was acknowledged from the simulated annual sediment yield, and the result shows that they lie in between 3.38 ton/ha/y and 38.55 ton/ha/y with an annual mean of 11.9 ton/ha/y for the subbasins (Table 3)

  • Spatial distribution of sediment yield from Kulfo watershed was projected from the simulated sediment outputs for each of the subbasins. e soil erosion levels in the basin were classified as very high (>20 t/ha/y), high (15–20 t/ha/y), moderate (10–15 t/ha/y), low (5–10 t/ha/y), and very low (0–5 t/ha/y)

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Summary

Introduction

Loss of soil is a natural geological denudation practice of detachment of upper soil by natural agencies like water, wind, glacier, and tidal effects though some anthropogenic interference cannot be ruled out. It reduces the fertility of land and eases the productivity of agricultural land [1, 2], [3]. Over grazing and indecorously managed land use/ land cover (LULC) may contribute to soil loss, changing the existence of the basins in large extent. Over grazing and indecorously managed land use/ land cover (LULC) may contribute to soil loss, changing the existence of the basins in large extent. is hampers in aggravating the climate change augmenting soil degradation

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