Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Clays and Clay Minerals Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Clays and Clay Minerals; December 2000; v. 48; no. 6; p. 665-681
© 2000 Clay Minerals Society
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (22)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Yu, C.-H.
Right arrow Articles by Teppen, B. J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

MOLECULAR DYNAMICS SIMULATIONS OF THE ADSORPTION OF METHYLENE BLUE AT CLAY MINERAL SURFACES

Ching-Hsing Yu1, Susan Q. Newton1, Mya A. Norman1, David M. Miller2, Lothar Schäfer1 and Brian J. Teppen3

1 Department of Chemistry, University of Arkansas, Fayetteville, Arkansas 72701 USA
2 Department of Crop, Soil, and Environmental Sciences, University of Arkansas, Fayetteville, Arkansas 72701 USA
3 Department of Crop and Soil Sciences, Michigan State University, East Lansing, Michigan 48824-1325 USA

E-mail of corresponding author: schafer{at}protein.uark.edu

Molecular dynamics simulations were performed of the adsorption of methylene blue (MB) on model beidellite, montmorillonite, and muscovite mica surfaces, using a previously determined empirical force field developed for dioctahedral clays. The simulations show that the adsorption of MB on mineral surfaces can result in a variety of configurations, including single and double layers of MB parallel to the basal surface, and irregular clusters. The d(001) values of ~12.3 and ~15.7 Å are assigned to dry phases with parallel single and double layers of MB, respectively, in agreement with X-ray studies. At intermediate MB loadings, stacks inclined to basal surfaces are formed. The stacks of MB ions inclined by 65–70° relative to the (001) plane of muscovite are not found on dry surfaces, in contrast to previous studies. Configurations similar to those proposed by others form spontaneously in the presence of H2O, but the ions in the model systems are not quite as ordered and not ordered in exactly the same way as the ones previously described, and they display a mobility that is not compatible with strict atomic order. The formation of a triple layer of H2O interspersed with ions may occur in the interlayer. Overall, the results of the simulations confirm that the MB-ion method must be used with great caution in surface-area determinations, because of the multiplicity of possible configurations. At the same time, the ability for adsorption to occur as either single or multiple MB layers is useful to determine cation-exchange capacity over a wide range of surface-charge densities.

Key Words: Adsorption of Methylene Blue • Clay Cation-Exchange Capacity Determination • Clay Surface-Area Determination • Molecular Dynamics Simulations




This article has been cited by other articles:


Home page
Soil Sci.Home page
B. J. Teppen and D. M. Miller
Hydration Energy Determines Isovalent Cation Exchange Selectivity by Clay Minerals
Soil Sci. Soc. Am. J., December 2, 2005; 70(1): 31 - 40.
[Abstract] [Full Text] [PDF]


Home page
Clay MineralsHome page
J. Bujdak, J. BUJDAK, N. IYI, Y. KANEKO, and R. SASAI
Molecular orientation of methylene blue cations adsorbed on clay surfaces
Clay Minerals, December 1, 2003; 38(4): 561 - 572.
[Abstract] [Full Text] [PDF]


Home page
Clays and Clay MineralsHome page
J. Bujdak, J. Bujdak, and N. Iyi
VISIBLE SPECTROSCOPY OF CATIONIC DYES IN DISPERSIONS WITH REDUCED-CHARGE MONTMORILLONITES
Clays and Clay Minerals, August 1, 2002; 50(4): 446 - 454.
[Abstract] [Full Text] [PDF]


Home page
Clay MineralsHome page
F. GILLOT, D. RIGHI, and M. L. RAISANEN
Layer-charge evaluation of expandable clays from a chronosequence of podzols in Finland using an alkylammonium method
Clay Minerals, December 1, 2001; 36(4): 571 - 584.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Clay Minerals Society