The Effect of Wetting and Drying Cycles on Potassium Release in Three Soil Orders

This research was conducted to study the potassium release under ten wetting and drying cycles in three soil orders (Mollisols, Vertisols, and Aridisols) collected from three different locations (Sharya, Semeel, and Kanishrin) in Dohuk governorate in Iraqi- Kurdistan region by using Ca-resin capsule...

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Main Authors: Baybeen Saeed Hasen Al-Silevany, Lazkeen Ahmed Merween Mehmedany
Format: Article
Language:English
Published: Polish Society of Ecological Engineering (PTIE) 2023-01-01
Series:Journal of Ecological Engineering
Subjects:
Online Access:http://www.jeeng.net/The-Effect-of-Wetting-and-Drying-Cycles-on-Potassium-Release-in-Three-Soil-Orders,156055,0,2.html
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author Baybeen Saeed Hasen Al-Silevany
Lazkeen Ahmed Merween Mehmedany
author_facet Baybeen Saeed Hasen Al-Silevany
Lazkeen Ahmed Merween Mehmedany
author_sort Baybeen Saeed Hasen Al-Silevany
collection DOAJ
description This research was conducted to study the potassium release under ten wetting and drying cycles in three soil orders (Mollisols, Vertisols, and Aridisols) collected from three different locations (Sharya, Semeel, and Kanishrin) in Dohuk governorate in Iraqi- Kurdistan region by using Ca-resin capsules, and K+ desorption fitted to four model equations to choose the best equation to describe K+. The results of the experiments showed that flocculated water content wetting and drying cycles increased cumulative K-release from Ca-resin capsules until a tenth of the wetting–drying cycle. Potassium desorption according to the kinetic approach showed a significant effect of time on potassium desorption, and potassium desorption conformed to parabolic diffusion equations kinetics was the best equation to describe the desorption of potassium by using Ca-resin with a high coefficient of determination (R2) and low standard error (SE) and the order of the equation in terms of their preference in describing the desorption process is as follows: 1-Parabolic diffusion, 2- Power function, 3-Elovich equation, 4- First-order . The apparent desorption rate coefficient (Kd) for the parabolic diffusion equation ranged from 0.1084-0.0877-0.1040 cmol kg-1 day -1 from Mollisols, Vertisols, and Aridisols respectively. The rate coefficient K desorption (Kd) according to the parabolic diffusion equation had a significant and positive correlation with SO42-, K+, T- CaCO3, HCO3, CEC, and Ca2+ but negatively significant correlated with EC and active CaCO3.
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spelling doaj.art-128aa5c79d614b61a495c9917ce54ace2022-12-22T03:46:46ZengPolish Society of Ecological Engineering (PTIE)Journal of Ecological Engineering2299-89932023-01-0124121822610.12911/22998993/156055156055The Effect of Wetting and Drying Cycles on Potassium Release in Three Soil OrdersBaybeen Saeed Hasen Al-Silevany0https://orcid.org/0000-0001-7604-4147Lazkeen Ahmed Merween Mehmedany1Department of Soil and Water Sciences, College of Agricultural Engineering Sciences, University of Duhok, Kurdistan Region, IraqDepartment of Soil and Water Sciences, College of Agricultural Engineering Sciences, University of Duhok, Kurdistan Region, IraqThis research was conducted to study the potassium release under ten wetting and drying cycles in three soil orders (Mollisols, Vertisols, and Aridisols) collected from three different locations (Sharya, Semeel, and Kanishrin) in Dohuk governorate in Iraqi- Kurdistan region by using Ca-resin capsules, and K+ desorption fitted to four model equations to choose the best equation to describe K+. The results of the experiments showed that flocculated water content wetting and drying cycles increased cumulative K-release from Ca-resin capsules until a tenth of the wetting–drying cycle. Potassium desorption according to the kinetic approach showed a significant effect of time on potassium desorption, and potassium desorption conformed to parabolic diffusion equations kinetics was the best equation to describe the desorption of potassium by using Ca-resin with a high coefficient of determination (R2) and low standard error (SE) and the order of the equation in terms of their preference in describing the desorption process is as follows: 1-Parabolic diffusion, 2- Power function, 3-Elovich equation, 4- First-order . The apparent desorption rate coefficient (Kd) for the parabolic diffusion equation ranged from 0.1084-0.0877-0.1040 cmol kg-1 day -1 from Mollisols, Vertisols, and Aridisols respectively. The rate coefficient K desorption (Kd) according to the parabolic diffusion equation had a significant and positive correlation with SO42-, K+, T- CaCO3, HCO3, CEC, and Ca2+ but negatively significant correlated with EC and active CaCO3.http://www.jeeng.net/The-Effect-of-Wetting-and-Drying-Cycles-on-Potassium-Release-in-Three-Soil-Orders,156055,0,2.htmlpotassiumrelease of potassiumsoil orderskinetics models
spellingShingle Baybeen Saeed Hasen Al-Silevany
Lazkeen Ahmed Merween Mehmedany
The Effect of Wetting and Drying Cycles on Potassium Release in Three Soil Orders
Journal of Ecological Engineering
potassium
release of potassium
soil orders
kinetics models
title The Effect of Wetting and Drying Cycles on Potassium Release in Three Soil Orders
title_full The Effect of Wetting and Drying Cycles on Potassium Release in Three Soil Orders
title_fullStr The Effect of Wetting and Drying Cycles on Potassium Release in Three Soil Orders
title_full_unstemmed The Effect of Wetting and Drying Cycles on Potassium Release in Three Soil Orders
title_short The Effect of Wetting and Drying Cycles on Potassium Release in Three Soil Orders
title_sort effect of wetting and drying cycles on potassium release in three soil orders
topic potassium
release of potassium
soil orders
kinetics models
url http://www.jeeng.net/The-Effect-of-Wetting-and-Drying-Cycles-on-Potassium-Release-in-Three-Soil-Orders,156055,0,2.html
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