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Modeling soil moisture effects on net nitrogen mineralization in loamy wetland soils

Steven Sleutel UGent, Bram Moeskops UGent, Willy Huybrechts, Annemie Vandenbossche, Joost Salomez UGent, Sara De Bolle UGent, David Buchan UGent and Stefaan De Neve UGent (2008) WETLANDS. 28(3). p.724-734
abstract
Nutrient dynamics in wetland ecosystems are largely controlled by soil moisture content. Therefore, the influence of soil moisture content on N mineralization should be explicitly taken into account in hydro-ecological models. The aim of this research was to establish relationships between N mineralization and soil moisture content in loamy to silty textured soils of floodplain wetlands in central Belgium. Large undisturbed soil cores were taken, incubated for 3 months under various moisture contents, and zero order and first order N mineralization rates were calculated. We used the percentage water-filled pore space (WFPS) as an expression of soil moisture because it is a better index for aeration dependent biological processes than volumetric moisture content or water retention. The relationship between the N mineralization rate and %WFPS was described by a Gaussian model. The optimum WFPS for N mineralization ranged between 57% and 78%, with a mean of 65% +/- 6% WFPS. Expected annual net N mineralization rates at field temperature (9.7 degrees C) and at optimal moisture content varied between 30 and 186 kg N ha(-1) (0-15 cm depth) year(-1), with a mean of 110 +/- 42 kg N ha(-1) (0-15 cm) year(-1). The mean N turnover rate amounted to 2.3 +/- 1.1 g N 100 g(-1) N year(-1). Multiple linear regressions between N mineralization and general soil parameters showed that soil structure has an overriding impact on N mineralization in wetland ecosystems.
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
keyword
N mineralization, Belgium, valley soils, water-filled pore space, N-MINERALIZATION, ORGANIC-MATTER, CROP RESIDUES, WATER, NITRIFICATION, VEGETATION, HYDROLOGY, CARBON, DENITRIFICATION, TEMPERATURE
journal title
WETLANDS
Wetlands
volume
28
issue
3
pages
724 - 734
Web of Science type
Article
Web of Science id
000258711600018
JCR category
ENVIRONMENTAL SCIENCES
JCR impact factor
1.117 (2008)
JCR rank
101/163 (2008)
JCR quartile
3 (2008)
ISSN
0277-5212
DOI
10.1672/07-105.1
language
English
UGent publication?
yes
classification
A1
copyright statement
I have transferred the copyright for this publication to the publisher
id
535823
handle
http://hdl.handle.net/1854/LU-535823
date created
2009-03-31 17:10:11
date last changed
2011-07-26 14:26:58
@article{535823,
  abstract     = {Nutrient dynamics in wetland ecosystems are largely controlled by soil moisture content. Therefore, the influence of soil moisture content on N mineralization should be explicitly taken into account in hydro-ecological models. The aim of this research was to establish relationships between N mineralization and soil moisture content in loamy to silty textured soils of floodplain wetlands in central Belgium. Large undisturbed soil cores were taken, incubated for 3 months under various moisture contents, and zero order and first order N mineralization rates were calculated. We used the percentage water-filled pore space (WFPS) as an expression of soil moisture because it is a better index for aeration dependent biological processes than volumetric moisture content or water retention. The relationship between the N mineralization rate and \%WFPS was described by a Gaussian model. The optimum WFPS for N mineralization ranged between 57\% and 78\%, with a mean of 65\% +/- 6\% WFPS. Expected annual net N mineralization rates at field temperature (9.7 degrees C) and at optimal moisture content varied between 30 and 186 kg N ha(-1) (0-15 cm depth) year(-1), with a mean of 110 +/- 42 kg N ha(-1) (0-15 cm) year(-1). The mean N turnover rate amounted to 2.3 +/- 1.1 g N 100 g(-1) N year(-1). Multiple linear regressions between N mineralization and general soil parameters showed that soil structure has an overriding impact on N mineralization in wetland ecosystems.},
  author       = {Sleutel, Steven and Moeskops, Bram and Huybrechts, Willy and Vandenbossche, Annemie and Salomez, Joost and De Bolle, Sara and Buchan, David and De Neve, Stefaan},
  issn         = {0277-5212},
  journal      = {WETLANDS},
  keyword      = {N mineralization,Belgium,valley soils,water-filled pore space,N-MINERALIZATION,ORGANIC-MATTER,CROP RESIDUES,WATER,NITRIFICATION,VEGETATION,HYDROLOGY,CARBON,DENITRIFICATION,TEMPERATURE},
  language     = {eng},
  number       = {3},
  pages        = {724--734},
  title        = {Modeling soil moisture effects on net nitrogen mineralization in loamy wetland soils},
  url          = {http://dx.doi.org/10.1672/07-105.1},
  volume       = {28},
  year         = {2008},
}

Chicago
Sleutel, Steven, Bram Moeskops, Willy Huybrechts, Annemie Vandenbossche, Joost Salomez, Sara De Bolle, David Buchan, and Stefaan De Neve. 2008. “Modeling Soil Moisture Effects on Net Nitrogen Mineralization in Loamy Wetland Soils.” Wetlands 28 (3): 724–734.
APA
Sleutel, S., Moeskops, B., Huybrechts, W., Vandenbossche, A., Salomez, J., De Bolle, S., Buchan, D., et al. (2008). Modeling soil moisture effects on net nitrogen mineralization in loamy wetland soils. WETLANDS, 28(3), 724–734.
Vancouver
1.
Sleutel S, Moeskops B, Huybrechts W, Vandenbossche A, Salomez J, De Bolle S, et al. Modeling soil moisture effects on net nitrogen mineralization in loamy wetland soils. WETLANDS. 2008;28(3):724–34.
MLA
Sleutel, Steven, Bram Moeskops, Willy Huybrechts, et al. “Modeling Soil Moisture Effects on Net Nitrogen Mineralization in Loamy Wetland Soils.” WETLANDS 28.3 (2008): 724–734. Print.