About Us | Help Videos | Contact Us | Subscriptions
 

Abstract

 

This article in SSSAJ

  1. Vol. 30 No. 3, p. 321-327
     
    Received: Sept 27, 1965
    Published: May, 1966


 View
 Download
 Alerts
 Permissions
 Share

doi:10.2136/sssaj1966.03615995003000030010x

Reactions of Surfactants with Montmorillonite: Adsorption Mechanisms1

  1. J. P. Law and
  2. G. W. Kunze2,3

Abstract

Abstract

Four clays were treated with each of eight surfactants at three treatment rates. Volclay and the clay fraction from two montmorillonitic soils were treated with 100, 50, and 10 mmol /100 g.; and kaolinite was treated with 10, 5, and 1 mmol /100g.

Adsorption was measured quantitatively by the thermogravimetric method. Adsorption mechanisms were investigated by X-ray diffraction and differential thermal analysis.

The surfactants included three anionic, three cationic, and two nonionic compounds. The anionics were not adsorbed in appreciable quantities and anion exchange of kaolinite appeared to be equal to or somewhat greater than that of montmorillonite. Anionics had no effect on the d-spacing of montmorillonite and did not interfere with hydration of clay surfaces.

Cationics were strongly adsorbed by the clay surfaces through ionic bonding in amounts equal to or even greater than the cation-exchange capacities of the clays. The excess material was probably held by van der Waals forces between the alkyl radicals which increased with chain length. Their presence on clays significantly reduced hydration and water content to the extent of making the clay surfaces completely hydrophobic at the high treatment rates.

Nonionics were adsorbed by hydrogen bonding of polar-active groups to oxygen-rich clay surfaces. Their sorption energies were somewhat greater than that of water, and they displaced water when adsorbed. Both cationic and nonionic compounds were held in the interlayer spaces of montmorillonite and tended to form double layers if sufficient material was present.

  Please view the pdf by using the Full Text (PDF) link under 'View' to the left.

Copyright © . Soil Science Society of America