BEHAVIOR OF MAGNESIUM IN SALINE SOILS 1- IT'S EFFECT ON CATION EXCHANGE CHARACTERTICS

To study the effect of magnesium on cation exchange characteristics, soil samples were collected from salt-affected soils of five locations from Al-Jazeera northern irrigation project of Nenava province-Iraq. Cation exchange experiment between Ca and Mg in the presence of sodium was carried out to q...

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Main Author: A.W. Abdul-Kareem
Format: Article
Language:Arabic
Published: College of Agriculture 2009-03-01
Series:Mesopotamia Journal of Agriculture
Online Access:https://magrj.mosuljournals.com/article_27390_072405040afed409316380adcf404ca6.pdf
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spelling doaj-591961adb5804abf8d6e126cef6516bd2020-11-25T02:15:58ZaraCollege of AgricultureMesopotamia Journal of Agriculture1815-316X2224-97962009-03-0137110311010.33899/magrj.2009.2739027390BEHAVIOR OF MAGNESIUM IN SALINE SOILS 1- IT'S EFFECT ON CATION EXCHANGE CHARACTERTICSA.W. Abdul-KareemTo study the effect of magnesium on cation exchange characteristics, soil samples were collected from salt-affected soils of five locations from Al-Jazeera northern irrigation project of Nenava province-Iraq. Cation exchange experiment between Ca and Mg in the presence of sodium was carried out to quantify the Mg on the accumulation samples with ten electrolyte solutions using chloride salts of NaCl, MgCl2.6H2O and CaCl2.2H2O with ratio of Na: Ca + Mg ranging from 1: 9 to 9: 1. the SAR ranging from (0-40) and the total concentration of the chloride solutions was 100 mmolcl-1. Revealing soils preference for calcium and magnesium was conducted by using electrolyte solutions with different Mg/Ca ratios. The results showed that the selectivity coefficient values of Mg-Ca ranged between (0.466-0.810) with an average 0.622 which reflect that Ca and Mg are not identical in their exchange behavior and the studied soils showed a preference for Ca in comparison with Mg. The examined soils had a tendency to accumulate exchangeable Na when Mg rather than Ca was the complementary cation, the Na-Mg systems had between 11.5-23.7% more exchangeable Na with an average of 19%.https://magrj.mosuljournals.com/article_27390_072405040afed409316380adcf404ca6.pdf
collection DOAJ
language Arabic
format Article
sources DOAJ
author A.W. Abdul-Kareem
spellingShingle A.W. Abdul-Kareem
BEHAVIOR OF MAGNESIUM IN SALINE SOILS 1- IT'S EFFECT ON CATION EXCHANGE CHARACTERTICS
Mesopotamia Journal of Agriculture
author_facet A.W. Abdul-Kareem
author_sort A.W. Abdul-Kareem
title BEHAVIOR OF MAGNESIUM IN SALINE SOILS 1- IT'S EFFECT ON CATION EXCHANGE CHARACTERTICS
title_short BEHAVIOR OF MAGNESIUM IN SALINE SOILS 1- IT'S EFFECT ON CATION EXCHANGE CHARACTERTICS
title_full BEHAVIOR OF MAGNESIUM IN SALINE SOILS 1- IT'S EFFECT ON CATION EXCHANGE CHARACTERTICS
title_fullStr BEHAVIOR OF MAGNESIUM IN SALINE SOILS 1- IT'S EFFECT ON CATION EXCHANGE CHARACTERTICS
title_full_unstemmed BEHAVIOR OF MAGNESIUM IN SALINE SOILS 1- IT'S EFFECT ON CATION EXCHANGE CHARACTERTICS
title_sort behavior of magnesium in saline soils 1- it's effect on cation exchange charactertics
publisher College of Agriculture
series Mesopotamia Journal of Agriculture
issn 1815-316X
2224-9796
publishDate 2009-03-01
description To study the effect of magnesium on cation exchange characteristics, soil samples were collected from salt-affected soils of five locations from Al-Jazeera northern irrigation project of Nenava province-Iraq. Cation exchange experiment between Ca and Mg in the presence of sodium was carried out to quantify the Mg on the accumulation samples with ten electrolyte solutions using chloride salts of NaCl, MgCl2.6H2O and CaCl2.2H2O with ratio of Na: Ca + Mg ranging from 1: 9 to 9: 1. the SAR ranging from (0-40) and the total concentration of the chloride solutions was 100 mmolcl-1. Revealing soils preference for calcium and magnesium was conducted by using electrolyte solutions with different Mg/Ca ratios. The results showed that the selectivity coefficient values of Mg-Ca ranged between (0.466-0.810) with an average 0.622 which reflect that Ca and Mg are not identical in their exchange behavior and the studied soils showed a preference for Ca in comparison with Mg. The examined soils had a tendency to accumulate exchangeable Na when Mg rather than Ca was the complementary cation, the Na-Mg systems had between 11.5-23.7% more exchangeable Na with an average of 19%.
url https://magrj.mosuljournals.com/article_27390_072405040afed409316380adcf404ca6.pdf
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