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


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Article Info

DATE

2012-10-23

AUTHORS

Amin Eisazadeh, Khairul Anuar Kassim, Hadi Nur

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 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. More... »

PAGES

1435-1440

References to SciGraph publications

  • 1999-04-01. Cation Exchange Capacity of Kaolinite in CLAYS AND CLAY MINERALS
  • 1995-12. Stabilization of lateritic soils with phosphoric acid in GEOTECHNICAL AND GEOLOGICAL ENGINEERING
  • Identifiers

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    http://scigraph.springernature.com/pub.10.1007/s10706-012-9553-y

    DOI

    http://dx.doi.org/10.1007/s10706-012-9553-y

    DIMENSIONS

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