Interactions of n-alkylammonium ions with mica-type layer lattices
Author:
- G. F. WalkerGWG. F. Walker
- 1 December 1967
- journal article
- Published by Mineralogical Society in Clay Minerals
- Vol. 7 (2) , 129-143
Abstract
The literature on the complexes of n-alkylammonium ions with layer silicates is characterized by marked divergences, not only in the deductions and conclusions of the different investigators but also in their experimental results. An attempt is made to reconcile and rationalize the differences, and to form a self-consistent picture of these systems.Given a saturating solution of sufficient concentration, the complexes tend during their formation to adopt an arrangement in which silicate layers are separated by double layers of ions oriented so that the alkyl chains are extended away from the silicate surfaces at a high angle. Water molecules, salt and free alkylamine may also be present in the interlayer spaces. When the excess material is removed by washing and the complexes dried, ideally the alkyl chains from opposing surfaces move over one another and interpenetrate so as to form a single layer of ions. During the contraction, however, the chains interact with one another and tend to stick at some point short of complete interpenetration. Weak attractive forces acting to bring the silicate layers together, and consisting mainly of electrostatic forces originating in the mineral layers and van der Waals interactions arising from increasing association of opposing alkyl chains with increasing interpenetration, are insufficient to overcome this tendency fully. As a result, an alkyl chain of given length can give rise to a series of complexes differing in their XRD characteristics.Previous workers have noted the difficulty of achieving reproducible results and some have recommended grinding the complexes, but it appears that this treatment significantly alters the nature of the end-product.Keywords
This publication has 14 references indexed in Scilit:
- Complexes between n-alkylamines and nickel cyanideTransactions of the Faraday Society, 1967
- Organic Derivatives of Mica‐type Layer‐SilicatesAngewandte Chemie International Edition, 1963
- Mica-Type Layer Silicates with Alkylammonium IonsClays and clay minerals (National Conference on Clays and Clay Minerals), 1961
- Notizen: Über eine einfache Möglichkeit zur Abschätzung der Schichtladung glimmerartiger SchichtsilikateZeitschrift für Naturforschung B, 1960
- Swelling of Some Vermiculite-Organic Complexes in WaterClays and clay minerals (National Conference on Clays and Clay Minerals), 1960
- ÜBER DEN EINFLUSS VON WASSERSTOFFBRÜCKENBINDUNGEN AUF EIN- UND ZWEIDIMENSIONALE INNERKRISTALLINE QUELLUNGSVORGÄNGE1959
- Über das Kationenaustauschvermögen der Tonminerale. II. Der Kationenaustausch bei den Mineralen der Glimmer-, Vermikulit- und MontmorillonitgruppeZeitschrift für anorganische und allgemeine Chemie, 1958
- Die innerkristalline Quellung als allgemeines Modell für QuellungsvorgängeEuropean Journal of Inorganic Chemistry, 1958
- BatavitZeitschrift für Naturforschung B, 1951
- Organophilic Bentonites. I. Swelling in Organic Liquids.The Journal of Physical Chemistry, 1949