Salinity–pH Relationships in Calcareous Soils

Soil pH is the most commonly requested analysis undertaken during farm advisory work. Determination of pH assists in understanding many reactions that occur in soil. Variations in pH between soils have been related to a number of other soil parameters. In this study thirty different soils were colle...

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Main Authors: A.S. Al-Busaidi, P. Cookson
Format: Article
Language:English
Published: Sultan Qaboos University 2003-01-01
Series:Journal of Agricultural and Marine Sciences
Subjects:
Online Access:https://journals.squ.edu.om/index.php/jams/article/view/615
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author A.S. Al-Busaidi
P. Cookson
author_facet A.S. Al-Busaidi
P. Cookson
author_sort A.S. Al-Busaidi
collection DOAJ
description Soil pH is the most commonly requested analysis undertaken during farm advisory work. Determination of pH assists in understanding many reactions that occur in soil. Variations in pH between soils have been related to a number of other soil parameters. In this study thirty different soils were collected from agricultural areas to have a wide range of pH, salinity, and texture. The objective was to study the relationship between soil pH and salinity. A negative relationship was found between soil salinity and pH. The main factor contributing to this relationship was probably the presence of soluble Ca2+ ion in soil. Variations in soluble Ca2+ ion concentrations between soils were negatively related to soil pH and positively related to soil salinity. Other soil properties that may affect pH, including CEC, CaCO3, clay content, gypsum and sodium adsorption ratio (SAR), were also determined.
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spelling doaj.art-52cd39b2962d48cdab5057be0a2c804b2022-12-21T19:22:02ZengSultan Qaboos UniversityJournal of Agricultural and Marine Sciences2410-10602410-10792003-01-0181414610.24200/jams.vol8iss1pp41-46599Salinity–pH Relationships in Calcareous SoilsA.S. Al-Busaidi0P. Cookson1Department of Soil and Water Sciences, College of Agricultural and Marine Sciences, Sultan Qaboos University, P.O. Box 34 Al-Khod 123, Sultanate of OmanDepartment of Soil and Water Sciences, College of Agricultural and Marine Sciences, Sultan Qaboos University, P.O. Box 34 Al-Khod 123, Sultanate of OmanSoil pH is the most commonly requested analysis undertaken during farm advisory work. Determination of pH assists in understanding many reactions that occur in soil. Variations in pH between soils have been related to a number of other soil parameters. In this study thirty different soils were collected from agricultural areas to have a wide range of pH, salinity, and texture. The objective was to study the relationship between soil pH and salinity. A negative relationship was found between soil salinity and pH. The main factor contributing to this relationship was probably the presence of soluble Ca2+ ion in soil. Variations in soluble Ca2+ ion concentrations between soils were negatively related to soil pH and positively related to soil salinity. Other soil properties that may affect pH, including CEC, CaCO3, clay content, gypsum and sodium adsorption ratio (SAR), were also determined.https://journals.squ.edu.om/index.php/jams/article/view/615electrical conductivity, sodicity, ph, alkaline soil, caco3.
spellingShingle A.S. Al-Busaidi
P. Cookson
Salinity–pH Relationships in Calcareous Soils
Journal of Agricultural and Marine Sciences
electrical conductivity, sodicity, ph, alkaline soil, caco3.
title Salinity–pH Relationships in Calcareous Soils
title_full Salinity–pH Relationships in Calcareous Soils
title_fullStr Salinity–pH Relationships in Calcareous Soils
title_full_unstemmed Salinity–pH Relationships in Calcareous Soils
title_short Salinity–pH Relationships in Calcareous Soils
title_sort salinity ph relationships in calcareous soils
topic electrical conductivity, sodicity, ph, alkaline soil, caco3.
url https://journals.squ.edu.om/index.php/jams/article/view/615
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