Effects of slope length on runoff from alfisols in Western Nigeria

The effects of 5, 10, 15 and 20 m slope lengths were investigated on runoff for natural slope gradients of about 1, 5, 10 and 15%. These studies were conducted on field runoff plots on natural slopes and under natural rainfall conditions at Ibadan in western Nigeria. The runoff, based on individual...

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Autor principal: Lal, R.
Formato: Journal Article
Lenguaje:Inglés
Publicado: 1983
Materias:
Acceso en línea:https://hdl.handle.net/10568/177239
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author Lal, R.
author_browse Lal, R.
author_facet Lal, R.
author_sort Lal, R.
collection Repository of Agricultural Research Outputs (CGSpace)
description The effects of 5, 10, 15 and 20 m slope lengths were investigated on runoff for natural slope gradients of about 1, 5, 10 and 15%. These studies were conducted on field runoff plots on natural slopes and under natural rainfall conditions at Ibadan in western Nigeria. The runoff, based on individual rainfall events, was not significantly correlated with either of three erosivity indices (EI30, KE > 1, AIm) and only a maximum of 36% of variability in runoff could be attributed to rainfall erosivity. Runoff per unit area decreased with increase in slope length. The mean annual runoff was of the order of 100, 87, 80 and 69 for 1977 and 100, 66, 49 and 35 for 1978 for 5, 10, 15 and 20 m slope lengths, respectively. Regression analyses indicated that the annual runoff was related to slope length according to the regression equation W = 773 L−0−53, where W is annual runoff in mm and L is slope length in meters. When fitted to data from all plots on a given slope steepness, for individual years the numerical value of length exponent b ranged from 0.153 to −0.865.
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spelling CGSpace1772392025-11-11T10:31:46Z Effects of slope length on runoff from alfisols in Western Nigeria Lal, R. runoff slope soil water balance topography The effects of 5, 10, 15 and 20 m slope lengths were investigated on runoff for natural slope gradients of about 1, 5, 10 and 15%. These studies were conducted on field runoff plots on natural slopes and under natural rainfall conditions at Ibadan in western Nigeria. The runoff, based on individual rainfall events, was not significantly correlated with either of three erosivity indices (EI30, KE > 1, AIm) and only a maximum of 36% of variability in runoff could be attributed to rainfall erosivity. Runoff per unit area decreased with increase in slope length. The mean annual runoff was of the order of 100, 87, 80 and 69 for 1977 and 100, 66, 49 and 35 for 1978 for 5, 10, 15 and 20 m slope lengths, respectively. Regression analyses indicated that the annual runoff was related to slope length according to the regression equation W = 773 L−0−53, where W is annual runoff in mm and L is slope length in meters. When fitted to data from all plots on a given slope steepness, for individual years the numerical value of length exponent b ranged from 0.153 to −0.865. 1983 2025-10-21T12:07:12Z 2025-10-21T12:07:12Z Journal Article https://hdl.handle.net/10568/177239 en Open Access application/pdf Lal, R. (1983). Effects of slope length on runoff from Alfisols in Western Nigeria. Geoderma, 31(3), 185-193.
spellingShingle runoff
slope
soil water balance
topography
Lal, R.
Effects of slope length on runoff from alfisols in Western Nigeria
title Effects of slope length on runoff from alfisols in Western Nigeria
title_full Effects of slope length on runoff from alfisols in Western Nigeria
title_fullStr Effects of slope length on runoff from alfisols in Western Nigeria
title_full_unstemmed Effects of slope length on runoff from alfisols in Western Nigeria
title_short Effects of slope length on runoff from alfisols in Western Nigeria
title_sort effects of slope length on runoff from alfisols in western nigeria
topic runoff
slope
soil water balance
topography
url https://hdl.handle.net/10568/177239
work_keys_str_mv AT lalr effectsofslopelengthonrunofffromalfisolsinwesternnigeria