Changes in soil susceptibility to erosion under tillage and soil fertility management practices

The degree to which soil is susceptible to erosion is measured as soil erodibility which can be influenced by different land management options. This study evaluated the dynamics of soil erodibility to tillage and soil amendments in a maize field under five consecutive cropping cycles. Tillage treat...

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Main Author: Samuel Ayodele Mesele
Format: Article
Language:English
Published: Maximum Academic Press 2024-01-01
Series:Circular Agricultural Systems
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Online Access:https://www.maxapress.com/article/doi/10.48130/cas-0024-0004
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author Samuel Ayodele Mesele
author_facet Samuel Ayodele Mesele
author_sort Samuel Ayodele Mesele
collection DOAJ
description The degree to which soil is susceptible to erosion is measured as soil erodibility which can be influenced by different land management options. This study evaluated the dynamics of soil erodibility to tillage and soil amendments in a maize field under five consecutive cropping cycles. Tillage treatments were no-till, minimum, conventional, and grassland fallow (control). The soil amendment treatments used were no amendment (control), NPK, poultry manure (PM), and ½ NPK + ½ PM and these treatments were applied to all the tillage treatments including no-till. The study showed that tillage and soil amendment interactions had significant effects on soil erodibility (p < 0.05). The mean erodibility values ranged from 13 × 10−3 to 24 × 10−3 Mg·h·MJ−1·mm−1 in the following order: control < conventional tillage < minimum tillage < no-till. For the soil amendments, erodibility varied from NPK > poultry manure = ½ NPK + ½ PM > control (undisturbed grassland). Regardless of the type of soil amendment, the soil erodibility under conventional tillage was significantly lower than that under no-till and minimum tillage systems. The relationship between erodibility and easily measured soil parameters, such as % sand greater than 100 µm, % silt plus very fine sand, clay, and saturated hydraulic conductivity, were significant at p < 0.05. The higher contribution (86%) of sand and silt to the variation in erodibility indicates that any other indices of erodibility based on particle size distribution, apart from the nomograph, could satisfactorily predict erodibility values.
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spelling doaj-art-b0d1a4f483a045ecac4ee3b183965a562025-08-20T02:27:18ZengMaximum Academic PressCircular Agricultural Systems2767-96082024-01-01411710.48130/cas-0024-0004cas-0024-0004Changes in soil susceptibility to erosion under tillage and soil fertility management practicesSamuel Ayodele Mesele0International Institute of Tropical Agriculture (IITA), Headquarters, PMB 5320, Oyo Road, Ibadan, NigeriaThe degree to which soil is susceptible to erosion is measured as soil erodibility which can be influenced by different land management options. This study evaluated the dynamics of soil erodibility to tillage and soil amendments in a maize field under five consecutive cropping cycles. Tillage treatments were no-till, minimum, conventional, and grassland fallow (control). The soil amendment treatments used were no amendment (control), NPK, poultry manure (PM), and ½ NPK + ½ PM and these treatments were applied to all the tillage treatments including no-till. The study showed that tillage and soil amendment interactions had significant effects on soil erodibility (p < 0.05). The mean erodibility values ranged from 13 × 10−3 to 24 × 10−3 Mg·h·MJ−1·mm−1 in the following order: control < conventional tillage < minimum tillage < no-till. For the soil amendments, erodibility varied from NPK > poultry manure = ½ NPK + ½ PM > control (undisturbed grassland). Regardless of the type of soil amendment, the soil erodibility under conventional tillage was significantly lower than that under no-till and minimum tillage systems. The relationship between erodibility and easily measured soil parameters, such as % sand greater than 100 µm, % silt plus very fine sand, clay, and saturated hydraulic conductivity, were significant at p < 0.05. The higher contribution (86%) of sand and silt to the variation in erodibility indicates that any other indices of erodibility based on particle size distribution, apart from the nomograph, could satisfactorily predict erodibility values.https://www.maxapress.com/article/doi/10.48130/cas-0024-0004conservation agricultureland degradationsoil erosiontillage
spellingShingle Samuel Ayodele Mesele
Changes in soil susceptibility to erosion under tillage and soil fertility management practices
Circular Agricultural Systems
conservation agriculture
land degradation
soil erosion
tillage
title Changes in soil susceptibility to erosion under tillage and soil fertility management practices
title_full Changes in soil susceptibility to erosion under tillage and soil fertility management practices
title_fullStr Changes in soil susceptibility to erosion under tillage and soil fertility management practices
title_full_unstemmed Changes in soil susceptibility to erosion under tillage and soil fertility management practices
title_short Changes in soil susceptibility to erosion under tillage and soil fertility management practices
title_sort changes in soil susceptibility to erosion under tillage and soil fertility management practices
topic conservation agriculture
land degradation
soil erosion
tillage
url https://www.maxapress.com/article/doi/10.48130/cas-0024-0004
work_keys_str_mv AT samuelayodelemesele changesinsoilsusceptibilitytoerosionundertillageandsoilfertilitymanagementpractices