SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 53:1668-1673 (1989)
© 1989 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
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 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 Google Scholar
Google Scholar
Right arrow Articles by McBride, M.
Right arrow Articles by Kung, K.-H.
Right arrow Search for Related Content
PubMed
Right arrow Articles by McBride, M.
Right arrow Articles by Kung, K.-H.
Agricola
Right arrow Articles by McBride, M.
Right arrow Articles by Kung, K.-H.

Complexation of Glyphosate and Related Ligands with Iron (III)

Murray McBride* and King-Hsi Kung

Dep. of Agronomy, Cornell Univ., Ithaca, NY 14850

*Corresponding author.

ABSTRACT

The extent of chelation of aqueous Fe3+ by glyphosate [isopropylamine salt of N-(phosphonomethyl)glycine] and the related ligands glycine, iminodiacetic acid and aminomethylphosphonic acid was estimated over a range of pH and ligand/Fe3+ ratios. Electron spin resonance (ESR) and UV-visible spectroscopy were used to detect chelation, evidenced by changes in the inner-sphere coordination environment of Fe3+. Generally, the spectroscopic methods confirmed the degree of chelation predicted from the known stability constants of these Fe3+complexes. The importance of the phosphonomoeity in conferring a high degree of stability to the complexes were confirmed and the Fe3+-glyphosate soluble complex persisted in aqueous solution to pH 4 and higher. The Fe3+complexes without the phosphonate group failed to form or existed only in very acidic solution, since they were easily dissociated upon the hydrolysis of Fe3+ as the pH was raised. Infrared spectroscopy of glyphosate adsorbed on goethite confirmed direct coordination of the functional groups with surface Fe3+, and suggested that the strong adsorption of glyphosate on oxides is a consequence of the same chelation mechanism observed in solution.

Received for publication February 27, 1989.


This article has been cited by other articles:


Home page
Clays and Clay MineralsHome page
A. L. Gimsing and O. K. Borggaard
PHOSPHATE AND GLYPHOSATE ADSORPTION BY HEMATITE AND FERRIHYDRITE AND COMPARISON WITH OTHER VARIABLE-CHARGE MINERALS
Clays and Clay Minerals, February 1, 2007; 55(1): 108 - 114.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
K. A. Barrett and M.B. McBride
Trace Element Mobilization in Soils by Glyphosate
Soil Sci. Soc. Am. J., September 20, 2006; 70(6): 1882 - 1888.
[Abstract] [Full Text] [PDF]




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 © 1989 by the Soil Science Society of America.