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 46:1158-1164 (1982)
© 1982 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 Cline, G. R.
Right arrow Articles by Reid, C. P. P.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Cline, G. R.
Right arrow Articles by Reid, C. P. P.
Agricola
Right arrow Articles by Cline, G. R.
Right arrow Articles by Reid, C. P. P.

Comparison of the Abilities of Hydroxamic, Synthetic, and Other Natural Organic Acids to Chelate Iron and Other Ions in Nutrient Solution1

Gary R. Cline, P. E. Powell, P. J. Szaniszlo and C. P. P. Reid2

ABSTRACT

Chelation modeling was used to predict the abilities of hydroxamate siderophores (HS) and other natural organic acids to chelate Fe and other ions in a modified Hoagland nutrient solution as a function of pH (4.0–10.0). Experimentally determined levels of chelated Fe (pH 5.0–10.0) agreed with our predicted results and with values previously predicted for EDTA (ethylenediaminetetraacetic acid), DTPA (diethylenetriaminepentaacetic acid), and EDDHA [ethylenediamine di(o-hydroxyphenylacetic) acid].

The natural HS, Desferrioxamine B (DFOB), and an unknown mixture of HS isolated from the ectomycorrhizal fungus Boletus edulis, remained fully chelated with Fe at all values of pH. Modeling predicted DFOB to be 99.9% chelated with Fe even in nutrient solution of pH 10.0. No significant chelation of Fe was measured or predicted above pH 6.0 for malate, malonate, oxalate, succinate, {alpha}-ketoglutarate, or pyruvate. Only 4% of citrate was chelated with Fe at pHs 6.0 and 6.4 as determined by direct measurement and computer modeling, respectively.

Solubility constants, derived for Fe(OH)3 (amorphous) (amorph.) and FePO4 (amorph.), indicated that FePO4 (amorph.) can control Fe solubility in nutrient solutions of low pH and reduce the ability of ligands to chelate Fe, relative to conditions in which Fe solubility is governed by Fe(OH)3 (amorph.).

Since our results indicate that microbially produced hydroxamate siderophores have a significant influence on Fe solubility, we discuss how such ligands could be of importance in the Fe nutrition of plants under natural soil conditions.


NOTES

1 This research was supported by the National Science Foundation (Grant no. DEB-79-11276.)

2 Postdoctoral Associate, Dep. of Crop and Soil Sciences, New Mexico State Univ., Las Cruces, NM 88003; Postdoctoral Associate and Professor of Microbiology, Dep. of Microbiology, Univ. of Texas, Austin, TX 78712; and Professor of Forestry, Dep. of Forestry and Wood Sciences, Colorado State Univ., Fort Collins, CO 80523.

Received for publication June 3, 1981. Accepted for publication July 26, 1982.




This article has been cited by other articles:


Home page
Plant Physiol.Home page
A. F. López-Millán, F. Morales, A. Abadía, and J. Abadía
Effects of Iron Deficiency on the Composition of the Leaf Apoplastic Fluid and Xylem Sap in Sugar Beet. Implications for Iron and Carbon Transport
Plant Physiology, October 1, 2000; 124(2): 873 - 884.
[Abstract] [Full Text]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1982 by the Soil Science Society of America.