SSSAJ
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 2 June 2005
Published in Soil Sci Soc Am J 69:1036-1046 (2005)
DOI: 10.2136/sssaj2004.0148
© 2005 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Abstract Freely available
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 HighWire
Right arrow Citing Articles via ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Wang, J. J.
Right arrow Articles by Harrell, D. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Wang, J. J.
Right arrow Articles by Harrell, D. L.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Wang, J. J.
Right arrow Articles by Harrell, D. L.
Related Collections
Right arrow Sorption/Exchange
Right arrow Heavy Metals
Right arrow Nutrient Management
Right arrow Soil Chemistry
Right arrow Soil Fertility and Productivity

Effect of Ammonium, Potassium, and Sodium Cations and Phosphate, Nitrate, and Chloride Anions on Zinc Sorption and Lability in Selected Acid and Calcareous Soils

Jim Jian Wang* and Dustin L. Harrell

Dep. of Agronomy and Environmental Management, 313 Sturgis Hall, Louisiana State Univ. Agricultural Center, Baton Rouge, LA. 70803



View larger version (29K):

[in a new window]
 
Fig. 1. Zinc sorption on selected acid soils as affected by differing cationic and anionic background solutions. C = equilibrium solution concentration; q = sorbed zinc amount.

 


View larger version (25K):

[in a new window]
 
Fig. 2. Zinc sorption on selected calcareous soils as affected by differing cationic and anionic cationic background solutions. C = equilibrium solution concentration; q = sorbed zinc amount.

 


View larger version (12K):

[in a new window]
 
Fig. 3. Relationship between the total Zn sorption (at the highest initial Zn concentration in KH2PO4 background) and the amorphous Fe content for acid and calcareous soils. q = sorbed zinc amount.

 


View larger version (29K):

[in a new window]
 
Fig. 4. Sorption isotherms for total, labile, and nonlabile Zn sorption for an acidic Dundee soil as affected by different background cationic and anionic species. C = equilibrium solution concentration; q = sorbed zinc amount.

 


View larger version (27K):

[in a new window]
 
Fig. 5. Sorption isotherms for total, labile, and nonlabile Zn sorption for a calcareous Norwood soil as affected by different background cationic and ionic species. C = equilibrium solution concentration; q = sorbed zinc amount.

 





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 © 2005 by the Soil Science Society of America.