BORON DESORPTION IN SOME CALCAREOUS SOILS OF NINEVEH GOVERNORATE / NORTH OF IRAQ

The investigation was conducted to study the behavior of boron desorption in three calcareous soils, classified as calciorthid. The experiment of boron sorption was conducted by using a different concentrations (0,0.5,1,2,4,6,8,10,20) mg B.L-1 (as boric acid) at 298ْ k while desorption experiment wa...

Full description

Bibliographic Details
Main Authors: M. Al-Obaidi, A. kashmola
Format: Article
Language:Arabic
Published: College of Agriculture 2007-09-01
Series:Mesopotamia Journal of Agriculture
Online Access:https://magrj.mosuljournals.com/article_26511_38515b1bfde867679b905a77bb91f10a.pdf
id doaj-b4fc6bd4d02a4a1388908ccee8eb33ec
record_format Article
spelling doaj-b4fc6bd4d02a4a1388908ccee8eb33ec2020-11-25T02:23:06ZaraCollege of AgricultureMesopotamia Journal of Agriculture1815-316X2224-97962007-09-01353525910.33899/magrj.2007.2651126511BORON DESORPTION IN SOME CALCAREOUS SOILS OF NINEVEH GOVERNORATE / NORTH OF IRAQM. Al-Obaidi0A. kashmola1Soil Dept., College of Agric. and Forestry, Univ. of Mosul, IraqSoil Dept., College of Agric. and Forestry, Univ. of Mosul, IraqThe investigation was conducted to study the behavior of boron desorption in three calcareous soils, classified as calciorthid. The experiment of boron sorption was conducted by using a different concentrations (0,0.5,1,2,4,6,8,10,20) mg B.L-1 (as boric acid) at 298ْ k while desorption experiment was conducted from adsorbed soils by using (0.01) M CaCl2 at (289 ْ k ) in order to study of boron hystersis. Langmuir model was used to describe capability of boron adsorption / desorption then the desorption index was calculated. Obtained results showed that boron adsorption energy was (0.843-0.069) L. mg -1 while boron desorption energy was ( 10.037-22.683) L. mg-1, while the boron desorption index was ( 1.32 - 3.66) for this reason the boron adsorption was not reversible.https://magrj.mosuljournals.com/article_26511_38515b1bfde867679b905a77bb91f10a.pdf
collection DOAJ
language Arabic
format Article
sources DOAJ
author M. Al-Obaidi
A. kashmola
spellingShingle M. Al-Obaidi
A. kashmola
BORON DESORPTION IN SOME CALCAREOUS SOILS OF NINEVEH GOVERNORATE / NORTH OF IRAQ
Mesopotamia Journal of Agriculture
author_facet M. Al-Obaidi
A. kashmola
author_sort M. Al-Obaidi
title BORON DESORPTION IN SOME CALCAREOUS SOILS OF NINEVEH GOVERNORATE / NORTH OF IRAQ
title_short BORON DESORPTION IN SOME CALCAREOUS SOILS OF NINEVEH GOVERNORATE / NORTH OF IRAQ
title_full BORON DESORPTION IN SOME CALCAREOUS SOILS OF NINEVEH GOVERNORATE / NORTH OF IRAQ
title_fullStr BORON DESORPTION IN SOME CALCAREOUS SOILS OF NINEVEH GOVERNORATE / NORTH OF IRAQ
title_full_unstemmed BORON DESORPTION IN SOME CALCAREOUS SOILS OF NINEVEH GOVERNORATE / NORTH OF IRAQ
title_sort boron desorption in some calcareous soils of nineveh governorate / north of iraq
publisher College of Agriculture
series Mesopotamia Journal of Agriculture
issn 1815-316X
2224-9796
publishDate 2007-09-01
description The investigation was conducted to study the behavior of boron desorption in three calcareous soils, classified as calciorthid. The experiment of boron sorption was conducted by using a different concentrations (0,0.5,1,2,4,6,8,10,20) mg B.L-1 (as boric acid) at 298ْ k while desorption experiment was conducted from adsorbed soils by using (0.01) M CaCl2 at (289 ْ k ) in order to study of boron hystersis. Langmuir model was used to describe capability of boron adsorption / desorption then the desorption index was calculated. Obtained results showed that boron adsorption energy was (0.843-0.069) L. mg -1 while boron desorption energy was ( 10.037-22.683) L. mg-1, while the boron desorption index was ( 1.32 - 3.66) for this reason the boron adsorption was not reversible.
url https://magrj.mosuljournals.com/article_26511_38515b1bfde867679b905a77bb91f10a.pdf
work_keys_str_mv AT malobaidi borondesorptioninsomecalcareoussoilsofninevehgovernoratenorthofiraq
AT akashmola borondesorptioninsomecalcareoussoilsofninevehgovernoratenorthofiraq
_version_ 1724859867992162304