SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
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 Google Scholar
Google Scholar
Right arrow Articles by Siebner-Freibach, H.
Right arrow Articles by Chen, Y.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Siebner-Freibach, H.
Right arrow Articles by Chen, Y.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Siebner-Freibach, H.
Right arrow Articles by Chen, Y.
Related Collections
Right arrow Sorption/Exchange
Right arrow Nutrient Cycling
Right arrow Soil Chemistry
Published in Soil Sci. Soc. Am. J. 68:470-480 (2004).
© 2004 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

DIVISION S-2—SOIL CHEMISTRY

Interaction of Iron Chelating Agents with Clay Minerals

H. Siebner-Freibacha, Y. Hadarb and Y. Chen*,a

a Dep. of Soil and Water Sciences, Faculty of Agricultural, Food and Environmental Quality Sciences, the Hebrew University of Jerusalem, P.O. Box 12, Rehovot 76100, Israel
b Dep. of Microbiology and Plant Pathology, Faculty of Agricultural, Food and Environmental Quality Sciences, the Hebrew University of Jerusalem, P.O. Box 12, Rehovot 76100, Israel

* Corresponding author (yonachen{at}agri.huji.ac.il).

Organic ligands play an important role in metal transport and availability in soils. However, their interaction with the solid phase of soils has not been sufficiently investigated. Two efficient Fe chelators were investigated in this study, as free ligands as well as Fe complexes: (i) the microbial siderophore ferrioxamine B (desferrioxamine B [DFOB] and ferrioxamine B [FOB], respectively); (ii) the synthetic chelating agent ethylenediamine di-o-hydroxyphenylacetic acid (EDDHA and FeEDDHA, respectively). Batch experiments were conducted to characterize their adsorption to Ca- and Na-montmorillonite as well as to Fe-montmorillonite (for EDDHA and FeEDDHA) and Ca-kaolinite. Kinetics of adsorption, equilibrium adsorption isotherms, and effects of pH on adsorption were measured. Adsorption of DFOB and FOB to montmorillonite was rapid and adsorption isotherms indicated high affinity. The type of saturating cation affected the adsorption of DFOB but not that of FOB. Significant hysteresis between adsorption and desorption was exhibited. The effect of Ca2+ in solution on desorption compared with that of Na+, was found to vary with their solution concentrations. Ethylenediamine di-o-hydroxyphenylacetic acid adsorption to montmorillonite exhibited a linear adsorption isotherm and significantly higher affinity than that of FeEDDHA. The adsorption decreased significantly with the following order of saturating cation: Ca2+ > Fe3+ > Na+. Adsorption of all examined substances to kaolinite was extremely low. Adsorption mechanisms of DFOB and EDDHA and their Fe complexes to clays and the environmental implications are discussed.

Abbreviations: CAS, Chrome Azurol S • CEC, cation-exchange capacity • DFOB, desferrioxamine B • EDDHA, ethylenediamine di-o-hydroxyphenylacetic acid • FOB, ferrioxamine B







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2004 by the Soil Science Society of America.