Distribution of humic substances in sieved aggregates of soil under contrasting land use

Soil quality indicators that control aggregate stability need o be extensively investigated so as to maintain our soils. Humified carbon (HC), humified acid carbon (HAC), and aggregate-associated fulvic acid carbon (FAC) in forest soils, cocoa plantations, five-year fallow, and five-year continuous...

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Main Authors: Bassey Udom, Achimota Dickson, Gogo Arthur, Miebaka Ikiriko, Babatunde Nuga
Format: Article
Language:English
Published: Sebelas Maret University 2025-01-01
Series:Sains Tanah: Journal of Soil Science and Agroclimatology
Subjects:
Online Access:https://jurnal.uns.ac.id/tanah/article/view/85938
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author Bassey Udom
Achimota Dickson
Gogo Arthur
Miebaka Ikiriko
Babatunde Nuga
author_facet Bassey Udom
Achimota Dickson
Gogo Arthur
Miebaka Ikiriko
Babatunde Nuga
author_sort Bassey Udom
collection DOAJ
description Soil quality indicators that control aggregate stability need o be extensively investigated so as to maintain our soils. Humified carbon (HC), humified acid carbon (HAC), and aggregate-associated fulvic acid carbon (FAC) in forest soils, cocoa plantations, five-year fallow, and five-year continuous cultivated soils were studied. Samples of soil were collected at 0-15 cm topsoil in order to measure the amount of humic materials in both the wet sieved and dry sieved aggregates. Findings revealed a significant input of land use on values of HC, HAC, and FAC occluded in sieved soil aggregates. The HC and FAC were preferentially stored in micro aggregate fractions less than 0.25 mm, while the HAC was greater in macro aggregates 2-1 mm and 1-0.5 mm. Concentration of HC was 18.8 g kg-1 in dry sieved and 17.2 g kg-1 in wet sieved micro aggregates less than 0.25 mm. The HC increased significantly (p<0.05) under a 5-year fallow. The HAC was stored in macro aggregates larger than 1 mm, whereas the HC and FAC fractions were occluded in micro aggregates > 1.0 mm. Continuous cropping decreased MWD of water-stable aggregates by 55%, while bulk density increased by 18%. The correlation coefficient between HC and MWD was significant (r = 0.811, p < 0.01), revealing the positive role of HC in aggregate stability. This study will help in understanding soil management strategies that will raise the accumulation of HC and HAC in macro-aggregates, thereby protecting the soil mass from structural degradation.
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institution Kabale University
issn 1412-3606
2356-1424
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publishDate 2025-01-01
publisher Sebelas Maret University
record_format Article
series Sains Tanah: Journal of Soil Science and Agroclimatology
spelling doaj-art-92b2bf7f24c34f29892fa268cce5fa7c2025-01-13T01:07:41ZengSebelas Maret UniversitySains Tanah: Journal of Soil Science and Agroclimatology1412-36062356-14242025-01-0121220320910.20961/stjssa.v21i2.8593844455Distribution of humic substances in sieved aggregates of soil under contrasting land useBassey Udom0Achimota Dickson1Gogo Arthur2Miebaka Ikiriko3Babatunde Nuga4Department of Crop and Soil Science, University of Port Harcourt, Port HarcourtDepartment of Crop and Soil Science, Niger Delta University, Wilberforce IslandDepartment of Crop and Soil Science, University of Port Harcourt, Port HarcourtDepartment of Crop and Soil Science, University of Port Harcourt, Port HarcourtNukot Consulting Services Inc., Winnipeg, ManitobaSoil quality indicators that control aggregate stability need o be extensively investigated so as to maintain our soils. Humified carbon (HC), humified acid carbon (HAC), and aggregate-associated fulvic acid carbon (FAC) in forest soils, cocoa plantations, five-year fallow, and five-year continuous cultivated soils were studied. Samples of soil were collected at 0-15 cm topsoil in order to measure the amount of humic materials in both the wet sieved and dry sieved aggregates. Findings revealed a significant input of land use on values of HC, HAC, and FAC occluded in sieved soil aggregates. The HC and FAC were preferentially stored in micro aggregate fractions less than 0.25 mm, while the HAC was greater in macro aggregates 2-1 mm and 1-0.5 mm. Concentration of HC was 18.8 g kg-1 in dry sieved and 17.2 g kg-1 in wet sieved micro aggregates less than 0.25 mm. The HC increased significantly (p<0.05) under a 5-year fallow. The HAC was stored in macro aggregates larger than 1 mm, whereas the HC and FAC fractions were occluded in micro aggregates > 1.0 mm. Continuous cropping decreased MWD of water-stable aggregates by 55%, while bulk density increased by 18%. The correlation coefficient between HC and MWD was significant (r = 0.811, p < 0.01), revealing the positive role of HC in aggregate stability. This study will help in understanding soil management strategies that will raise the accumulation of HC and HAC in macro-aggregates, thereby protecting the soil mass from structural degradation.https://jurnal.uns.ac.id/tanah/article/view/85938aggregate stabilityhumified acid carbonhumified carbonsoil organic matterwater stable aggregates
spellingShingle Bassey Udom
Achimota Dickson
Gogo Arthur
Miebaka Ikiriko
Babatunde Nuga
Distribution of humic substances in sieved aggregates of soil under contrasting land use
Sains Tanah: Journal of Soil Science and Agroclimatology
aggregate stability
humified acid carbon
humified carbon
soil organic matter
water stable aggregates
title Distribution of humic substances in sieved aggregates of soil under contrasting land use
title_full Distribution of humic substances in sieved aggregates of soil under contrasting land use
title_fullStr Distribution of humic substances in sieved aggregates of soil under contrasting land use
title_full_unstemmed Distribution of humic substances in sieved aggregates of soil under contrasting land use
title_short Distribution of humic substances in sieved aggregates of soil under contrasting land use
title_sort distribution of humic substances in sieved aggregates of soil under contrasting land use
topic aggregate stability
humified acid carbon
humified carbon
soil organic matter
water stable aggregates
url https://jurnal.uns.ac.id/tanah/article/view/85938
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AT achimotadickson distributionofhumicsubstancesinsievedaggregatesofsoilundercontrastinglanduse
AT gogoarthur distributionofhumicsubstancesinsievedaggregatesofsoilundercontrastinglanduse
AT miebakaikiriko distributionofhumicsubstancesinsievedaggregatesofsoilundercontrastinglanduse
AT babatundenuga distributionofhumicsubstancesinsievedaggregatesofsoilundercontrastinglanduse