2014Journal of environment and earth scienceRequires access

Determination of Soil Erosion Runoff using a Developed Laboratory Rainfall Simulator

O M Unuigbe, C I Ayilaran, Ikhazuagbe Ohiwere, Thomas Bosede

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Abstract

Using a developed rainfall simulator, soil erosion was studied in three representative soils in Auchi, Southern part of Nigeria. The runoff water and the quantities of the eroded sediments were measured with respect to soil type, slope and vegetal cover. Erosion from the simulated storm was greatly reduced by vegetative cover, declining from (3.32 - 4.48)*10 -3 m 3 for the exposed soil to (1.05 - 1.21)*10 -3 m 3 , for the one covered with vegetation due to interception of raindrop by the leaves. However, increase in slope from 5 o through 15 o increased the runoff and quantities of eroded sediments slightly from (4.82)*10 -3 m 3 and 0.850 kg to (3.98)*10 -3 m 3 and 1.439kg respectively. The quantity of runoff for the three types of soil considered was more in sample C (sandy loam) with a value of (3.32)*10 -3 m 3 than the other soil types, sample A (silty clay) and sample B (clay soil) with runoff values of 4.48 and 4.38*(10 -3 m 3 respectively. K eywords : soil erosion; slope; soil type; vegetation; rainfall simulator

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What this paper is about

Using a developed rainfall simulator, soil erosion was studied in three representative soils in Auchi, Southern part of Nigeria. The runoff water and the quantities of the eroded sediments were measured with respect to soil type, slope and vegetal cover. Erosion from the simulated storm was greatly reduced by vegetative cover, declining from (3.32 - 4.48)*10 -3 m 3 for the exposed soil to (1.05 - 1.21)*10 -3 m 3 , for the one covered with vegetation due to interception of raindrop by the leaves. However, increase in slope from 5 o through 15 o increased the runoff and quantities of eroded sediments slightly from (4.82)*10 -3 m 3 and 0.850 kg to (3.98)*10 -3 m 3 and 1.439kg respectively. The quantity of runoff for the three types of soil considered was more in sample C (sandy loam) with a value of (3.32)*10 -3 m 3 than the other soil types, sample A (silty clay) and sample B (clay soil) with runoff values of 4.48 and 4.38*(10 -3 m 3 respectively. K eywords : soil erosion; slope; soil type; vegetation; rainfall simulator

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Available abstract

Using a developed rainfall simulator, soil erosion was studied in three representative soils in Auchi, Southern part of Nigeria. The runoff water and the quantities of the eroded sediments were measured with respect to soil type, slope and vegetal cover. Erosion from the simulated storm was greatly reduced by vegetative cover, declining from (3.32 - 4.48)*10 -3 m 3 for the exposed soil to (1.05 - 1.21)*10 -3 m 3 , for the one covered with vegetation due to interception of raindrop by the leaves. However, increase in slope from 5 o through 15 o increased the runoff and quantities of eroded sediments slightly from (4.82)*10 -3 m 3 and 0.850 kg to (3.98)*10 -3 m 3 and 1.439kg respectively. The quantity of runoff for the three types of soil considered was more in sample C (sandy loam) with a value of (3.32)*10 -3 m 3 than the other soil types, sample A (silty clay) and sample B (clay soil) with runoff values of 4.48 and 4.38*(10 -3 m 3 respectively. K eywords : soil erosion; slope; soil type; vegetation; rainfall simulator

Key concepts: Surface runoff, Loam, Hydrology (agriculture), Environmental science, Erosion, Interception, Vegetation (pathology), Soil water

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