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 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 (7)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Koopmans, G. F.
Right arrow Articles by van Riemsdijk, W. H.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Koopmans, G. F.
Right arrow Articles by van Riemsdijk, W. H.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Koopmans, G. F.
Right arrow Articles by van Riemsdijk, W. H.
Related Collections
Right arrow Soil Kinetics
Right arrow Soil Models
Right arrow Nutrient Cycling
Right arrow Plant and Soil Interactions
Right arrow Phosphorus

Phosphorus Desorption Dynamics in Soil and the Link to a Dynamic Concept of Bioavailability

G. F. Koopmansa,*, W. J. Chardona, P. de Willigena and W. H. van Riemsdijkb

a Alterra, Wageningen University and Research Centre (WUR), P.O. Box 47, 6700 AA, Wageningen, the Netherlands
b Department of Soil Quality, Wageningen University, WUR, P.O. Box 8005, 6700 EC, Wageningen, the Netherlands



View larger version (23K):

[in a new window]
 
Fig. 1. Desorption isotherm of the soils of the pot experiment (Koopmans et al., 2004) describing the relationship between the P concentration measured in 1:10 (w/v) 0.01 M CaCl2 extracts (vigorous shaking) and the total pool of sorbed P (open symbols). The Langmuir equation was fitted to the data. Furthermore, the total pool of sorbed P is plotted against the P concentration as a function of time measured in 1:10 (w/v) 0.01 M CaCl2 extracts obtained under mild shaking conditions in the batch experiments (closed symbols).

 


View larger version (18K):

[in a new window]
 
Fig. 2. Measured (symbols) and predicted P concentrations (lines) in 0.01 M CaCl2 extracts with varying soil to solution ratios as a function of time at a fitted pore volume fraction of 0.035. The CaCl2 extracts were obtained from the initial soil under mild shaking conditions in the batch experiments. The open triangle represents the P concentration measured in the 1:10 (w/v) 0.01 M CaCl2 extract with vigorous shaking. The dotted line represents the predicted P concentration at a soil to solution ratio of 1:10 (w/v) whereby the radius of the spherical aggregate was set at 0.1 mm.

 


View larger version (15K):

[in a new window]
 
Fig. 3. Measured (symbols) and predicted P concentrations (lines) in 1:10 (w/v) 0.01 M CaCl2 extracts as a function of time. The CaCl2 extracts were obtained from the soils of the 5- and 10-cm treatments sampled after 151 and 978 d of plant uptake of P in the batch experiments.

 


View larger version (19K):

[in a new window]
 
Fig. 4. Profile of the P concentration along the radius of the spherical aggregate simulated for P desorption from the initial soil to an external solution with a soil to solution ratio of 1:10 (w/v) (x = 0 mm corresponds with the center of the spherical aggregate).

 


View larger version (16K):

[in a new window]
 
Fig. 5. Profile of the P concentration (A) and the amount of P sorbed to the solid phase (B) along the radius of the spherical aggregate simulated for the measured plant uptake of P in the 5-cm treatment (x = 0 mm corresponds with the center of the spherical aggregate).

 


View larger version (27K):

[in a new window]
 
Fig. 6. Simulated maximal P desorption rate from the spherical aggregate, the actual plant uptake rate, and the P content measured in the grass harvested in the 10-cm treatment as a function of time. The inserted figure shows the dynamic bioavailability index (DBI) as a function of time.

 





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 © 2004 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.