Investigation of Soil Physiochemical Properties Effects on Soil Compaction for a Long Year Tilled Farmland

In many parts of the world, the earth has been heavily compacted as a result of large farm equipment. For soil compaction, the main constituent factors were soil physiochemical properties such as soil texture, moisture content, electrical conductivity, cation exchange capacity, total organic carbon,...

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Main Authors: Yared Seifu Woldeyohannis, Someshakher S Hiremath, Simie Tola, Amana Wako
Format: Article
Language:English
Published: Wiley 2022-01-01
Series:Applied and Environmental Soil Science
Online Access:http://dx.doi.org/10.1155/2022/8626200
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author Yared Seifu Woldeyohannis
Someshakher S Hiremath
Simie Tola
Amana Wako
author_facet Yared Seifu Woldeyohannis
Someshakher S Hiremath
Simie Tola
Amana Wako
author_sort Yared Seifu Woldeyohannis
collection DOAJ
description In many parts of the world, the earth has been heavily compacted as a result of large farm equipment. For soil compaction, the main constituent factors were soil physiochemical properties such as soil texture, moisture content, electrical conductivity, cation exchange capacity, total organic carbon, organic matter, total nitrogen, and soil pH directly and indirectly. This article addressed the causes and effects of soil compaction, operating parameters, and soil physicochemical properties in the Bishoftu long year tilled farmland of Ethiopia. For the experimental test, 5 different depths (5, 10, 15, 20, and 25 cm) and fifteen sample points were selected in 0.6 ha of 60 m by 100 m farmland for taking soil compaction data. Soil samples are taken from three depth ranges (0–10, 10–20, and 20–30 cm) from farmlands for investigation of soil physicochemical properties. The maximum and minimum values of the cone index of this study were 1918.133 kPa and 864.733 kPa, respectively, by taking the average of all sample points. The soil laboratory result shows that Bishoftu farmland soil is a mixture of loam, clay loam, and sandy clay loam with 47.33% of sand, 25.67% of clay, and 27% of silt. The maximum and minimum percentages of soil moisture values were 27.02 and 21.46 at 0–10 cm and 20–30 cm depth, respectively. Total organic carbon, organic matter, and total nitrogen exhibit positive relationships with depth and soil compaction. The correlation analysis indicates soil pH, electric conductivity, percentage of sand, cation exchange capacity, organic matter, and total nitrogen were among soil physiochemical parameters that are positively correlated with soil compaction. Furthermore, the percentage of clay, percentage of silt, and total organic carbon (p≤0.05) are negatively correlated with soil compaction in soil samples.
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spelling doaj-art-524e00e5fb3249139f3a623a29b4464d2025-02-03T06:13:02ZengWileyApplied and Environmental Soil Science1687-76752022-01-01202210.1155/2022/8626200Investigation of Soil Physiochemical Properties Effects on Soil Compaction for a Long Year Tilled FarmlandYared Seifu Woldeyohannis0Someshakher S Hiremath1Simie Tola2Amana Wako3Department of Mechanical EngineeringDepartment of Mechanical Engineering (Precision and Instrumentation Laboratory Engineering)Department of Mechanical EngineeringDepartment of Mechanical EngineeringIn many parts of the world, the earth has been heavily compacted as a result of large farm equipment. For soil compaction, the main constituent factors were soil physiochemical properties such as soil texture, moisture content, electrical conductivity, cation exchange capacity, total organic carbon, organic matter, total nitrogen, and soil pH directly and indirectly. This article addressed the causes and effects of soil compaction, operating parameters, and soil physicochemical properties in the Bishoftu long year tilled farmland of Ethiopia. For the experimental test, 5 different depths (5, 10, 15, 20, and 25 cm) and fifteen sample points were selected in 0.6 ha of 60 m by 100 m farmland for taking soil compaction data. Soil samples are taken from three depth ranges (0–10, 10–20, and 20–30 cm) from farmlands for investigation of soil physicochemical properties. The maximum and minimum values of the cone index of this study were 1918.133 kPa and 864.733 kPa, respectively, by taking the average of all sample points. The soil laboratory result shows that Bishoftu farmland soil is a mixture of loam, clay loam, and sandy clay loam with 47.33% of sand, 25.67% of clay, and 27% of silt. The maximum and minimum percentages of soil moisture values were 27.02 and 21.46 at 0–10 cm and 20–30 cm depth, respectively. Total organic carbon, organic matter, and total nitrogen exhibit positive relationships with depth and soil compaction. The correlation analysis indicates soil pH, electric conductivity, percentage of sand, cation exchange capacity, organic matter, and total nitrogen were among soil physiochemical parameters that are positively correlated with soil compaction. Furthermore, the percentage of clay, percentage of silt, and total organic carbon (p≤0.05) are negatively correlated with soil compaction in soil samples.http://dx.doi.org/10.1155/2022/8626200
spellingShingle Yared Seifu Woldeyohannis
Someshakher S Hiremath
Simie Tola
Amana Wako
Investigation of Soil Physiochemical Properties Effects on Soil Compaction for a Long Year Tilled Farmland
Applied and Environmental Soil Science
title Investigation of Soil Physiochemical Properties Effects on Soil Compaction for a Long Year Tilled Farmland
title_full Investigation of Soil Physiochemical Properties Effects on Soil Compaction for a Long Year Tilled Farmland
title_fullStr Investigation of Soil Physiochemical Properties Effects on Soil Compaction for a Long Year Tilled Farmland
title_full_unstemmed Investigation of Soil Physiochemical Properties Effects on Soil Compaction for a Long Year Tilled Farmland
title_short Investigation of Soil Physiochemical Properties Effects on Soil Compaction for a Long Year Tilled Farmland
title_sort investigation of soil physiochemical properties effects on soil compaction for a long year tilled farmland
url http://dx.doi.org/10.1155/2022/8626200
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