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


     


Published online 20 April 2005
Published in J Environ Qual 34:926-935 (2005)
DOI: 10.2134/jeq2004.0101
© 2005 American Society of Agronomy, Crop Science Society of America, and 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 Related articles in JEQ
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (4)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Ilg, K.
Right arrow Articles by Kaupenjohann, M.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Ilg, K.
Right arrow Articles by Kaupenjohann, M.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Ilg, K.
Right arrow Articles by Kaupenjohann, M.
Related Collections
Right arrow Phosphorus
Right arrow Colloids
Right arrow Nutrients
Right arrow Soil Chemistry
Right arrow Vadose Zone Processes and Chemical Transport

Colloidal and Dissolved Phosphorus in Sandy Soils as Affected by Phosphorus Saturation

Katrin Ilg*, Jan Siemens and Martin Kaupenjohann

Department of Soil Science, Institute of Ecology, Berlin University of Technology, Salzufer 11-12, D-10587 Berlin, Germany



View larger version (21K):

[in a new window]
 
Fig. 1. Concentrations of dissolved P as a function of the degree of P saturation. *Significant at the 0.05 probability level. The split line was calculated for samples from the 30- to 60-cm depth of the Dülmen site. Do, Dülmen (old); Dn, Dülmen (new); H, Hamburg; N, Nienburg.

 


View larger version (22K):

[in a new window]
 
Fig. 2. Colloidal P concentrations related to the degree of P saturation. *Significant at the 0.05 probability level. Do, Dülmen (old); Dn, Dülmen (new); H, Hamburg; N, Nienburg.

 


View larger version (25K):

[in a new window]
 
Fig. 3. Effect of the degree of P saturation on concentrations of dissolved P, colloidal P, Fe + Al, P saturation of colloids, and optical density in KCl extracts. *Significant at the 0.05 probability level.

 





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
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 2005 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.