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


     


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 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 (20)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Koski-Vähälä, J.
Right arrow Articles by Tallberg, P.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Koski-Vähälä, J.
Right arrow Articles by Tallberg, P.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Koski-Vähälä, J.
Right arrow Articles by Tallberg, P.
Related Collections
Right arrow Surface Water Quality
Right arrow Nutrient Management
Right arrow Water Pollution

Phosphorus Mobilization from Various Sediment Pools in Response to Increased pH and Silicate Concentration

J. Koski-Vähäläa, H. Hartikainenb and P. Tallberga

a Dep. of Limnology and Environmental Protection, P.O. Box 27, FIN-00014 Helsinki Univ., Finland
b Dep. of Applied Chemistry and Microbiology, P.O. Box 27, FIN-00014 Helsinki University, Finland



View larger version (35K):

[in a new window]
 
Fig. 1. The experimental design and the laboratory procedure. Three replicates were used

 


View larger version (26K):

[in a new window]
 
Fig. 2. The effect of the different treatments on the desorption of labeled 33P (A, top) and unlabeled P (B, bottom) from the NaOH fraction, and on the recovery of released P in the NH4F fraction and in the interstitial water. Values are percent units of the P amount in the NaOH fraction in the control sample without pH manipulation and Si enrichment. High Si = high Si enrichment, elevated pH + high Si = elevated pH combined with high Si enrichment

 





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 © 2001 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.