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Organic matter in clay density fractions from sandy cropland soils with differing land-use history

Steven Sleutel UGent, P Leinweber, Eric Van Ranst UGent, MD Abdul Kader and Kanagaratnam Jegajeevagan (2011) SOIL SCIENCE SOCIETY OF AMERICA JOURNAL. 75(2). p.521-532
abstract
Land-use history is often overlooked when assessing soil fertility of intensive cropland production systems. The unusually high organic carbon (OC) content of many sandy cropland soils in Northwestern Europe is unexpected given their general low clay content (3-8%) and organic matter (OM) input typical of cropland, but appears to be related to historical heathland land-use. Clay fraction OM composition was compared between two groups of sandy cropland soils with (HC) or without (CC) a history of heathland/forest land-use. Light (1.6-2.2 g cm(-3)) and heavy (>2.2 g cm(-3)) clay fractions in HC soils were nearly twice as rich in OC (on average 199 g kg(-1)) compared with those of CC soils (on average 109 g kg(-1)). The hypothesized preferential presence of stable heathland derived OM in light soil fractions, was not supported by our data. Pyrolysis-field ionization mass spectrometry of the clay fractions revealed a more decomposed character of OM in the CC soils and lasting long-term influence of land-use history on SOM composition. This could be concluded from higher proportions of lipids and sterols, a lower thermostability in the HC compared with the CC soils, and enrichment of alkylaromatics and heterocyclic N-containing compounds in the latter. The density fractionation methodology separated organic-mineral particles with similar OM loadings but lower proportions of sterols and medium to long-chained lipids in the heavy compared with the light clay fraction. Given the very high clay OC loadings (6-16 mg C m(-2)) and low binding capacity of the quartz/kaolin ite/mica dominated clays, we hypothesize that OM-OM interactions are involved as an OM stabilization mechanism. However, contrary to our hypothesis high clay OC loading (and hence thick OM layering) were found in all sandy croplands regardless of land-use history or density fraction.
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
keyword
FOREST SOIL, CARBON, HUMIC SUBSTANCES, PYROLYSIS-MASS-SPECTROMETRY, PARTICLE-SIZE FRACTIONS, CHEMICAL-COMPOSITION, ARABLE SOILS, STABILITY, SPECTROSCOPY, LANDSCAPE
journal title
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL
Soil Sci. Soc. Am. J.
volume
75
issue
2
pages
521 - 532
Web of Science type
Article
Web of Science id
000288827000020
JCR category
SOIL SCIENCE
JCR impact factor
1.979 (2011)
JCR rank
8/32 (2011)
JCR quartile
2 (2011)
ISSN
0361-5995
DOI
10.2136/sssaj2010.0094
language
English
UGent publication?
yes
classification
A1
copyright statement
I have transferred the copyright for this publication to the publisher
id
1215999
handle
http://hdl.handle.net/1854/LU-1215999
date created
2011-05-03 08:44:38
date last changed
2016-12-19 15:45:05
@article{1215999,
  abstract     = {Land-use history is often overlooked when assessing soil fertility of intensive cropland production systems. The unusually high organic carbon (OC) content of many sandy cropland soils in Northwestern Europe is unexpected given their general low clay content (3-8\%) and organic matter (OM) input typical of cropland, but appears to be related to historical heathland land-use. Clay fraction OM composition was compared between two groups of sandy cropland soils with (HC) or without (CC) a history of heathland/forest land-use. Light (1.6-2.2 g cm(-3)) and heavy ({\textrangle}2.2 g cm(-3)) clay fractions in HC soils were nearly twice as rich in OC (on average 199 g kg(-1)) compared with those of CC soils (on average 109 g kg(-1)). The hypothesized preferential presence of stable heathland derived OM in light soil fractions, was not supported by our data. Pyrolysis-field ionization mass spectrometry of the clay fractions revealed a more decomposed character of OM in the CC soils and lasting long-term influence of land-use history on SOM composition. This could be concluded from higher proportions of lipids and sterols, a lower thermostability in the HC compared with the CC soils, and enrichment of alkylaromatics and heterocyclic N-containing compounds in the latter. The density fractionation methodology separated organic-mineral particles with similar OM loadings but lower proportions of sterols and medium to long-chained lipids in the heavy compared with the light clay fraction. Given the very high clay OC loadings (6-16 mg C m(-2)) and low binding capacity of the quartz/kaolin ite/mica dominated clays, we hypothesize that OM-OM interactions are involved as an OM stabilization mechanism. However, contrary to our hypothesis high clay OC loading (and hence thick OM layering) were found in all sandy croplands regardless of land-use history or density fraction.},
  author       = {Sleutel, Steven and Leinweber, P and Van Ranst, Eric and Kader, MD Abdul and Jegajeevagan, Kanagaratnam},
  issn         = {0361-5995},
  journal      = {SOIL SCIENCE SOCIETY OF AMERICA JOURNAL},
  keyword      = {FOREST SOIL,CARBON,HUMIC SUBSTANCES,PYROLYSIS-MASS-SPECTROMETRY,PARTICLE-SIZE FRACTIONS,CHEMICAL-COMPOSITION,ARABLE SOILS,STABILITY,SPECTROSCOPY,LANDSCAPE},
  language     = {eng},
  number       = {2},
  pages        = {521--532},
  title        = {Organic matter in clay density fractions from sandy cropland soils with differing land-use history},
  url          = {http://dx.doi.org/10.2136/sssaj2010.0094},
  volume       = {75},
  year         = {2011},
}

Chicago
Sleutel, Steven, P Leinweber, Eric Van Ranst, MD Abdul Kader, and Kanagaratnam Jegajeevagan. 2011. “Organic Matter in Clay Density Fractions from Sandy Cropland Soils with Differing Land-use History.” Soil Science Society of America Journal 75 (2): 521–532.
APA
Sleutel, Steven, Leinweber, P., Van Ranst, E., Kader, M. A., & Jegajeevagan, K. (2011). Organic matter in clay density fractions from sandy cropland soils with differing land-use history. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 75(2), 521–532.
Vancouver
1.
Sleutel S, Leinweber P, Van Ranst E, Kader MA, Jegajeevagan K. Organic matter in clay density fractions from sandy cropland soils with differing land-use history. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL. 2011;75(2):521–32.
MLA
Sleutel, Steven, P Leinweber, Eric Van Ranst, et al. “Organic Matter in Clay Density Fractions from Sandy Cropland Soils with Differing Land-use History.” SOIL SCIENCE SOCIETY OF AMERICA JOURNAL 75.2 (2011): 521–532. Print.