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


     


Published online 13 May 2005
Published in Vadose Zone J 4:329-336 (2005)
DOI: 10.2136/vzj2004.0102
© 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 ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Rodríguez, S. B.
Right arrow Articles by Álvarez-Benedí, J.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Rodríguez, S. B.
Right arrow Articles by Álvarez-Benedí, J.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Rodríguez, S. B.
Right arrow Articles by Álvarez-Benedí, J.
Related Collections
Right arrow Batch Studies
Right arrow Kinetics
Right arrow Nutrient Management

Characterization of Nitrogen Transformations, Sorption and Volatilization Processes In Urea Fertilized Soils

S. Bolado Rodrígueza,*, A. Alonso-Gaiteb and J. Álvarez-Benedíb

a Dep. de Ingeniería Química, Univ. de Valladolid, Spain
b Inst. Tecnológico Agrario de Castilla y León, Valladolid, Spain



View larger version (12K):

[in a new window]
 
Fig. 1. Schematic of the two models used: (a) considers linear local equilibrium and reversible NH4+ sorption, (b) considers NH4+ sorption and desorption as independent kinetics processes. Both models consider first-order kinetics for urea hydrolysis and pseudo-first order kinetics process for ammonia volatilization. KD is a distribution coefficient and kV, kN, kHU, kads, kdes are rate coefficients (volatilization rate, nitrification rate, urea hydrolysis rate, adsorption rate, and desorption rate, respectively).

 


View larger version (28K):

[in a new window]
 
Fig. 2. Schematic of the experimental system.

 


View larger version (25K):

[in a new window]
 
Fig. 3. Evolution of the different nitrogen forms described with the model assuming local equilibrium adsorption and the presence of an activation (lag) time for urea hydrolysis. Parameters used for this example are for the loamy sand (LS) soil at 28°C and {theta} = 0.15 cm3/cm3: U0 = 9.30 mg N/cm3, kV = 0.0095/h, KD = 0.025, tact = 200 h, kHU (hydrolysis rate constant) = 0.03/h. The value of kN (nitrification rate constant) was set to 0.001/h in order to reproduce the nitrification curve in the graph.

 


View larger version (24K):

[in a new window]
 
Fig. 4. Evolution of the different nitrogen forms described with the model assuming ammonium adsorption-desorption kinetics and the presence of an activation (lag) time for urea hydrolysis. Parameters used for this example are for the loamy sand (LS) soil at 28°C and volumetric moisture content ({theta}) = 0.15 cm3/cm3: initial concentration of urea (U0) = 9.30 mg N/cm3, volatilization coefficient (kV) = 0.0095/h, adsorption rate coefficient (kads) = 0.055/h, desorption rate coefficient (kdes) = 10–5/h, effective activation/adaptation time for the microbial population (tact) = 200 h, and hydrolysis rate constant (kHU) = 0.03/h. The value of kN (nitrification rate constant) was set to 0.001/h in order to reproduce the nitrification curve in the graph.

 


View larger version (23K):

[in a new window]
 
Fig. 5. Experimental results for volatilized ammonia in the Sandy Clay Loam (SCL) soil at 28°C (circles) and 18°C (squares). Open symbols represent experiments carried out at volumetric moisture content ({theta}) = 0.20 cm3/cm3; solid symbols represent experiments at {theta} = 0.33 cm3/cm3. Lines show model response with parameters presented in Table 3.

 


View larger version (18K):

[in a new window]
 
Fig. 6. Experimental results for the loamy sand soil at 28°C using two different initial levels of urea. Squares represent volatilized amounts of ammonia for experiments using an initial urea concentration of 2 g/kg, and circles represent volatilized amounts of ammonia for experiments using an initial urea concentration of 0.2 g/kg. Open symbols show experiments carried out at volumetric moisture content ({theta}) = 0.15 cm3/cm3, and solid symbols represent experiments at {theta} = 0.22 cm3/cm3. Lines show model response using the parameters presented in Table 3.

 





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2005 by the Soil Science Society of America.