EFFECT OF WATER IONIC STRENGTH ON SODIUM DESORPTION FOR SOME CALCAREOUS SOILS IN NINEVEH PROVINCE
<strong>A laboratory study was conducted to determine sodium desorption behavior from exchange positions of soil solid phase because of a quiet water flow. Using sulfuric water collected from a sulfuric spring and a chlorine water from Tigris river. The flow was through two disturbed soil colu...
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Format: | Article |
Language: | Arabic |
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College of Agriculture
2019-08-01
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Series: | Mesopotamia Journal of Agriculture |
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Online Access: | https://magrj.mosuljournals.com/article_161345_8cceaa40c19f91f4f6a1ca8f97b42b42.pdf |
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author | H. Ahmed M. A. J. Al-Obaidi M. T. S. Khalil |
author_facet | H. Ahmed M. A. J. Al-Obaidi M. T. S. Khalil |
author_sort | H. Ahmed |
collection | DOAJ |
description | <strong>A laboratory study was conducted to determine sodium desorption behavior from exchange positions of soil solid phase because of a quiet water flow. Using sulfuric water collected from a sulfuric spring and a chlorine water from Tigris river. The flow was through two disturbed soil columns. Soils were sampled from Fadhlia and Hamdania locations in Nineveh province/ northern Iraq. Waters flow were persisted for 240 minutes with 4 cm highness over soils surface was maintained. Leachates were collected every 10 minutes for a total ten extracts which analyzed for Na<sup>+</sup>. Three mathematical kinetic description were considered as an accumulative soluble Na<sup>+</sup>, Na<sup>+</sup> expressed by SAR and ESP concepts , sequences as parabolic diffusion, zero order, 1<sup>st</sup> order, Elovitch and power function (poly ordered) models were applied. Mathematical descriptions revealed succession of 1<sup>st</sup> order and power function models. Na<sup>+</sup> desorption coefficient rate values by 1<sup>st</sup> order model were ranged from </strong><strong>96 ×10<sup>-3</sup></strong><strong> -</strong><strong> 185 × 10<sup>-3</sup> minute for chlorine water, for sulfuric water were from 10 ×10<sup>-3</sup> - 34×10<sup>-3</sup> minute for both locations respectively, while </strong><strong>desorption coefficient rate values </strong><strong>according to power function model were 686 ×10<sup>-3</sup> , 683×10<sup>-3</sup> , 634×10<sup>-3</sup> mg.kg<sup>-1</sup>.min.<sup>.-1</sup> respectively. Results referred also that </strong><strong>Na<sup>+</sup> desorption coefficient rate values</strong><strong> was proportionally increased with waters ionic strength.</strong> |
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language | Arabic |
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series | Mesopotamia Journal of Agriculture |
spelling | doaj.art-cb154efcbf2c4e9c8ccfc07303062db02022-12-21T19:05:14ZaraCollege of AgricultureMesopotamia Journal of Agriculture1815-316X2224-97962019-08-0145314915810.33899/magrj.2019.161345161345EFFECT OF WATER IONIC STRENGTH ON SODIUM DESORPTION FOR SOME CALCAREOUS SOILS IN NINEVEH PROVINCEH. Ahmed0M. A. J. Al-Obaidi1M. T. S. Khalil2College of Agriculture and Forestry, Mosul University. IraqCollege of Agriculture and Forestry, Mosul University. IraqCollege of Agriculture and Forestry, Mosul University. Iraq<strong>A laboratory study was conducted to determine sodium desorption behavior from exchange positions of soil solid phase because of a quiet water flow. Using sulfuric water collected from a sulfuric spring and a chlorine water from Tigris river. The flow was through two disturbed soil columns. Soils were sampled from Fadhlia and Hamdania locations in Nineveh province/ northern Iraq. Waters flow were persisted for 240 minutes with 4 cm highness over soils surface was maintained. Leachates were collected every 10 minutes for a total ten extracts which analyzed for Na<sup>+</sup>. Three mathematical kinetic description were considered as an accumulative soluble Na<sup>+</sup>, Na<sup>+</sup> expressed by SAR and ESP concepts , sequences as parabolic diffusion, zero order, 1<sup>st</sup> order, Elovitch and power function (poly ordered) models were applied. Mathematical descriptions revealed succession of 1<sup>st</sup> order and power function models. Na<sup>+</sup> desorption coefficient rate values by 1<sup>st</sup> order model were ranged from </strong><strong>96 ×10<sup>-3</sup></strong><strong> -</strong><strong> 185 × 10<sup>-3</sup> minute for chlorine water, for sulfuric water were from 10 ×10<sup>-3</sup> - 34×10<sup>-3</sup> minute for both locations respectively, while </strong><strong>desorption coefficient rate values </strong><strong>according to power function model were 686 ×10<sup>-3</sup> , 683×10<sup>-3</sup> , 634×10<sup>-3</sup> mg.kg<sup>-1</sup>.min.<sup>.-1</sup> respectively. Results referred also that </strong><strong>Na<sup>+</sup> desorption coefficient rate values</strong><strong> was proportionally increased with waters ionic strength.</strong>https://magrj.mosuljournals.com/article_161345_8cceaa40c19f91f4f6a1ca8f97b42b42.pdfsulfuric waterzero1st order and power function models |
spellingShingle | H. Ahmed M. A. J. Al-Obaidi M. T. S. Khalil EFFECT OF WATER IONIC STRENGTH ON SODIUM DESORPTION FOR SOME CALCAREOUS SOILS IN NINEVEH PROVINCE Mesopotamia Journal of Agriculture sulfuric water zero 1st order and power function models |
title | EFFECT OF WATER IONIC STRENGTH ON SODIUM DESORPTION FOR SOME CALCAREOUS SOILS IN NINEVEH PROVINCE |
title_full | EFFECT OF WATER IONIC STRENGTH ON SODIUM DESORPTION FOR SOME CALCAREOUS SOILS IN NINEVEH PROVINCE |
title_fullStr | EFFECT OF WATER IONIC STRENGTH ON SODIUM DESORPTION FOR SOME CALCAREOUS SOILS IN NINEVEH PROVINCE |
title_full_unstemmed | EFFECT OF WATER IONIC STRENGTH ON SODIUM DESORPTION FOR SOME CALCAREOUS SOILS IN NINEVEH PROVINCE |
title_short | EFFECT OF WATER IONIC STRENGTH ON SODIUM DESORPTION FOR SOME CALCAREOUS SOILS IN NINEVEH PROVINCE |
title_sort | effect of water ionic strength on sodium desorption for some calcareous soils in nineveh province |
topic | sulfuric water zero 1st order and power function models |
url | https://magrj.mosuljournals.com/article_161345_8cceaa40c19f91f4f6a1ca8f97b42b42.pdf |
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