Cation Exchange Capacity of Phosphoric Acid and Lime Stabilized Montmorillonitic and Kaolinitic Soils

Studies on the chemically stabilized soils have shown that the effectiveness of treatment is largely dependent on soil’s natural environment. In this research, the time-dependent changes induced in permanent cation exchange capacity of lime and phosphoric acid treated soils, comprised mainly of mont...

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Published inGeotechnical and geological engineering Vol. 30; no. 6; pp. 1435 - 1440
Main Authors Eisazadeh, Amin, Kassim, Khairul Anuar, Nur, Hadi
Format Journal Article
LanguageEnglish
Published Dordrecht Springer Netherlands 01.12.2012
Springer Nature B.V
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Abstract Studies on the chemically stabilized soils have shown that the effectiveness of treatment is largely dependent on soil’s natural environment. In this research, the time-dependent changes induced in permanent cation exchange capacity of lime and phosphoric acid treated soils, comprised mainly of montmorillonite and kaolinite minerals, were investigated. Also, in order to study the relationship between the exchange capacity and acidity/alkalinity of pore water, pH measurements were 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 CEC p values at longer curing periods. Nevertheless, the kaolinite mineral with pH-dependent structural properties, showed a rather limited behavior in the acidic medium. From engineering point of view, the lime treated samples revealed the highest degree of improvement with an approximately ten-fold strength increase in comparison to the natural soil over an 8 months curing period.
AbstractList Studies on the chemically stabilized soils have shown that the effectiveness of treatment is largely dependent on soil’s natural environment. In this research, the time-dependent changes induced in permanent cation exchange capacity of lime and phosphoric acid treated soils, comprised mainly of montmorillonite and kaolinite minerals, were investigated. Also, in order to study the relationship between the exchange capacity and acidity/alkalinity of pore water, pH measurements were 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. Nevertheless, the kaolinite mineral with pH-dependent structural properties, showed a rather limited behavior in the acidic medium. From engineering point of view, the lime treated samples revealed the highest degree of improvement with an approximately ten-fold strength increase in comparison to the natural soil over an 8 months curing period.
Studies on the chemically stabilized soils have shown that the effectiveness of treatment is largely dependent on soil’s natural environment. In this research, the time-dependent changes induced in permanent cation exchange capacity of lime and phosphoric acid treated soils, comprised mainly of montmorillonite and kaolinite minerals, were investigated. Also, in order to study the relationship between the exchange capacity and acidity/alkalinity of pore water, pH measurements were 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 CEC p values at longer curing periods. Nevertheless, the kaolinite mineral with pH-dependent structural properties, showed a rather limited behavior in the acidic medium. From engineering point of view, the lime treated samples revealed the highest degree of improvement with an approximately ten-fold strength increase in comparison to the natural soil over an 8 months curing period.
Author Kassim, Khairul Anuar
Nur, Hadi
Eisazadeh, Amin
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  surname: Eisazadeh
  fullname: Eisazadeh, Amin
  email: A.Eisazadeh@yahoo.com, aeisazadeh@utm.my
  organization: Geotechnic and Transportation Department, Faculty of Civil Engineering, Universiti Teknologi Malaysia
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  givenname: Khairul Anuar
  surname: Kassim
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  surname: Nur
  fullname: Nur, Hadi
  organization: Ibnu Sina Institute for Fundamental Science Studies, Universiti Teknologi Malaysia
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Cites_doi 10.1007/BF00422210
10.1016/0013-7952(96)00028-2
10.1016/0016-7061(84)90065-X
10.1061/(ASCE)1090-0241(1997)123:2(183)
10.1346/CCMN.1999.0470207
10.1061/(ASCE)0733-9410(1996)122:5(329)
10.1201/9781482274769
ContentType Journal Article
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Geotechnical and Geological Engineering is a copyright of Springer, (2012). All Rights Reserved.
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Issue 6
Keywords Phosphoric acid
Lime
Cation exchange capacity
Stabilization
Bentonite
pH
Kaolinite
Language English
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PK Mathew (9553_CR10) 1997; 123
S Ross (9553_CR15) 1989
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Snippet Studies on the chemically stabilized soils have shown that the effectiveness of treatment is largely dependent on soil’s natural environment. In this research,...
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StartPage 1435
SubjectTerms Acidic soils
Acidity
Alkalinity
Cation exchange
Cation exchanging
Cations
Civil Engineering
Curing
Curing (processing)
Earth and Environmental Science
Earth Sciences
Exchange capacity
Geotechnical Engineering & Applied Earth Sciences
Hydrogeology
Ions
Kaolinite
Lime
Lime soil stabilization
Minerals
Montmorillonite
Montmorillonites
Organic chemistry
pH effects
Phosphoric acid
Pore water
Soil
Soil chemistry
Soil investigations
Soil lime
Soil stabilization
Soil treatment
Technical Note
Terrestrial Pollution
Time dependence
Waste Management/Waste Technology
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Title Cation Exchange Capacity of Phosphoric Acid and Lime Stabilized Montmorillonitic and Kaolinitic Soils
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