|
|
|
|||||||||||||||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
Research Paper |
1 Faculty of Chemistry, Jagiellonian University, ul. Ingardena 3, 30-060 Cracow, 2 Regional Laboratory of Physicochemical Analyses and Structural Research, ul. Ingardena 3, 30060 Cracow, 3 Department of Mineralogy and Geochemistry, Academy of Mining and Metallurgy, al. Mickiewicza 30, 30059 Cracow, Poland, and 4 Institute of Physical Chemistry, Friedrich Schiller University, Lessingstrasse 10, 07743 Jena, Germany
* E-mail: dyrek{at}trurl.ch.uj.edu.pl
(Received 20 November 1998; revised 16 August 1999)
Ammoniation of montmorillonites pillared with polyhydroxo-complexes of Al was performed in flow conditions at 7731073 K and monitored by IR spectroscopy. Interaction of the clay with ammonia revealed exchange of terminal and bridging -OH groups by NH2-, NH- and N-species depending on the reaction temperature. Amination begins at 773 K while formation of NH groups starts at 873 K. Transformation of NH- into N-species occurs at 973 K. A mechanism for the ammoniation reaction is proposed and the series of the relative reactivity of OH groups was established: SiOH > MgOHMg > AlOHMg > AlOHAl. This series was rationalized in terms of accessibility of the OH groups.
KEYWORDS: IR, ammoniation, pillared montmorillonite, polyhydroxo complexes
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |