ROLE OF WATER IRRIGATION ON POTASSIUM RELEASE IN SOME CALCAREUS SOILS OF NORTHERN IRAQ

A laboratory study was conducted to determine the effect of irrigation water quality on capacity and rate of potassium release in some calcareous soils in Nineveh province. It was constructed by miscible displacement technique with natural un disturbed soil columns using chlorine and sulfuric water...

Full description

Bibliographic Details
Main Author: A. Alhadede
Format: Article
Language:Arabic
Published: College of Agriculture 2018-03-01
Series:Mesopotamia Journal of Agriculture
Subjects:
Online Access:https://magrj.mosuljournals.com/article_161417_cd68bcfb39095670012890879fce6bf8.pdf
_version_ 1811322796238700544
author A. Alhadede
author_facet A. Alhadede
author_sort A. Alhadede
collection DOAJ
description A laboratory study was conducted to determine the effect of irrigation water quality on capacity and rate of potassium release in some calcareous soils in Nineveh province. It was constructed by miscible displacement technique with natural un disturbed soil columns using chlorine and sulfuric water of two different textured soils from location of Zummar of clayey and Sheikh Mohammed of loamy silt texture for ten irrigation epochs on the basis of porosity volume (PV). Results indicated for presence values of desorbed potassium rate with increase of porosity volumes passed through soil columns. Sulfuric water caused more desorption of potassium in comparison with chlorine water. Desorption capacity rate were 1.93, 2.92 c.mole.kg<sup>-1</sup> for Sheikh Mohammed and Zummar locations respectively by using sulfuric water, while desorbed potassium by using chlorine water for the same Soils were 1.12, 2.01 c.mole.kg<sup>-1</sup>. Mathematical description for desorption process appeared harmony of diffusion equation, power function equation, first order equation, zero order equation, while Elovitch equation did not describe desorption process with the same efficiency. K<sup>+</sup> desorption rate due to diffusion equation by using chlorine water were 0.06, 1.2 c.mole.kg<sup>-1.</sup>min<sup>-½</sup> for the Soil of Sheikh Mohammed and Zummar locations respectively, yet using sulfuric water increased desorption rate which were 0.14, 0.22 c.mole.kg<sup>-1.</sup>min<sup>-½</sup> for the same locations respectively.
first_indexed 2024-04-13T13:41:25Z
format Article
id doaj.art-9a110f315882422897f36523429a926c
institution Directory Open Access Journal
issn 1815-316X
2224-9796
language Arabic
last_indexed 2024-04-13T13:41:25Z
publishDate 2018-03-01
publisher College of Agriculture
record_format Article
series Mesopotamia Journal of Agriculture
spelling doaj.art-9a110f315882422897f36523429a926c2022-12-22T02:44:37ZaraCollege of AgricultureMesopotamia Journal of Agriculture1815-316X2224-97962018-03-01461596610.33899/magrj.2018.161417161417ROLE OF WATER IRRIGATION ON POTASSIUM RELEASE IN SOME CALCAREUS SOILS OF NORTHERN IRAQA. Alhadede0Soil Science &amp; Water Resources Dept., College of Agriculture and Forestry, Mosul University. IraqA laboratory study was conducted to determine the effect of irrigation water quality on capacity and rate of potassium release in some calcareous soils in Nineveh province. It was constructed by miscible displacement technique with natural un disturbed soil columns using chlorine and sulfuric water of two different textured soils from location of Zummar of clayey and Sheikh Mohammed of loamy silt texture for ten irrigation epochs on the basis of porosity volume (PV). Results indicated for presence values of desorbed potassium rate with increase of porosity volumes passed through soil columns. Sulfuric water caused more desorption of potassium in comparison with chlorine water. Desorption capacity rate were 1.93, 2.92 c.mole.kg<sup>-1</sup> for Sheikh Mohammed and Zummar locations respectively by using sulfuric water, while desorbed potassium by using chlorine water for the same Soils were 1.12, 2.01 c.mole.kg<sup>-1</sup>. Mathematical description for desorption process appeared harmony of diffusion equation, power function equation, first order equation, zero order equation, while Elovitch equation did not describe desorption process with the same efficiency. K<sup>+</sup> desorption rate due to diffusion equation by using chlorine water were 0.06, 1.2 c.mole.kg<sup>-1.</sup>min<sup>-½</sup> for the Soil of Sheikh Mohammed and Zummar locations respectively, yet using sulfuric water increased desorption rate which were 0.14, 0.22 c.mole.kg<sup>-1.</sup>min<sup>-½</sup> for the same locations respectively.https://magrj.mosuljournals.com/article_161417_cd68bcfb39095670012890879fce6bf8.pdfchlorine watersulfuric waterflow timek+ desorption rate
spellingShingle A. Alhadede
ROLE OF WATER IRRIGATION ON POTASSIUM RELEASE IN SOME CALCAREUS SOILS OF NORTHERN IRAQ
Mesopotamia Journal of Agriculture
chlorine water
sulfuric water
flow time
k+ desorption rate
title ROLE OF WATER IRRIGATION ON POTASSIUM RELEASE IN SOME CALCAREUS SOILS OF NORTHERN IRAQ
title_full ROLE OF WATER IRRIGATION ON POTASSIUM RELEASE IN SOME CALCAREUS SOILS OF NORTHERN IRAQ
title_fullStr ROLE OF WATER IRRIGATION ON POTASSIUM RELEASE IN SOME CALCAREUS SOILS OF NORTHERN IRAQ
title_full_unstemmed ROLE OF WATER IRRIGATION ON POTASSIUM RELEASE IN SOME CALCAREUS SOILS OF NORTHERN IRAQ
title_short ROLE OF WATER IRRIGATION ON POTASSIUM RELEASE IN SOME CALCAREUS SOILS OF NORTHERN IRAQ
title_sort role of water irrigation on potassium release in some calcareus soils of northern iraq
topic chlorine water
sulfuric water
flow time
k+ desorption rate
url https://magrj.mosuljournals.com/article_161417_cd68bcfb39095670012890879fce6bf8.pdf
work_keys_str_mv AT aalhadede roleofwaterirrigationonpotassiumreleaseinsomecalcareussoilsofnortherniraq