Cation exchange capacity of a quartz-rich soil in an acidic and basic environment

In this research, the time-dependent changes induced in charge characteristics of phosphoric acid and lime treated quartz-rich kaolinitic soil were investigated. Also, in order to study the relationship between the exchange capacity and the pore water chemistry, pH measurements was performed on cure...

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Main Authors: Eisazadeh, Amin, Kassim, Khairul Anuar, Nur, Hadi
Format: Article
Published: Trans Tech Publications 2011
Subjects:
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author Eisazadeh, Amin
Kassim, Khairul Anuar
Nur, Hadi
author_facet Eisazadeh, Amin
Kassim, Khairul Anuar
Nur, Hadi
author_sort Eisazadeh, Amin
collection ePrints
description In this research, the time-dependent changes induced in charge characteristics of phosphoric acid and lime treated quartz-rich kaolinitic soil were investigated. Also, in order to study the relationship between the exchange capacity and the pore water chemistry, pH measurements was performed on cured samples. Based on the collected data, it was found that the pH of stabilized soils showed a tendency for reaching soil’s natural pH with increasing curing time. In addition, the increase in number of broken bonds around the edges of soil particles and also the formation of cementitious compounds that acquired negative charges contributed to achieving higher CECp values at longer curing periods. From engineering point of view, the lime treated samples revealed the highest degree of improvement with an approximately 16-fold strength increase in comparison to the natural soil over an 8 months curing period.
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spelling utm.eprints-447732017-09-13T01:00:56Z http://eprints.utm.my/44773/ Cation exchange capacity of a quartz-rich soil in an acidic and basic environment Eisazadeh, Amin Kassim, Khairul Anuar Nur, Hadi S Agriculture In this research, the time-dependent changes induced in charge characteristics of phosphoric acid and lime treated quartz-rich kaolinitic soil were investigated. Also, in order to study the relationship between the exchange capacity and the pore water chemistry, pH measurements was performed on cured samples. Based on the collected data, it was found that the pH of stabilized soils showed a tendency for reaching soil’s natural pH with increasing curing time. In addition, the increase in number of broken bonds around the edges of soil particles and also the formation of cementitious compounds that acquired negative charges contributed to achieving higher CECp values at longer curing periods. From engineering point of view, the lime treated samples revealed the highest degree of improvement with an approximately 16-fold strength increase in comparison to the natural soil over an 8 months curing period. Trans Tech Publications 2011 Article PeerReviewed Eisazadeh, Amin and Kassim, Khairul Anuar and Nur, Hadi (2011) Cation exchange capacity of a quartz-rich soil in an acidic and basic environment. Advanced Materials Research, 255-26 . pp. 2766-2770. ISSN 1022-6680
spellingShingle S Agriculture
Eisazadeh, Amin
Kassim, Khairul Anuar
Nur, Hadi
Cation exchange capacity of a quartz-rich soil in an acidic and basic environment
title Cation exchange capacity of a quartz-rich soil in an acidic and basic environment
title_full Cation exchange capacity of a quartz-rich soil in an acidic and basic environment
title_fullStr Cation exchange capacity of a quartz-rich soil in an acidic and basic environment
title_full_unstemmed Cation exchange capacity of a quartz-rich soil in an acidic and basic environment
title_short Cation exchange capacity of a quartz-rich soil in an acidic and basic environment
title_sort cation exchange capacity of a quartz rich soil in an acidic and basic environment
topic S Agriculture
work_keys_str_mv AT eisazadehamin cationexchangecapacityofaquartzrichsoilinanacidicandbasicenvironment
AT kassimkhairulanuar cationexchangecapacityofaquartzrichsoilinanacidicandbasicenvironment
AT nurhadi cationexchangecapacityofaquartzrichsoilinanacidicandbasicenvironment