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@ARTICLE{Squaris:11859,
author = {Séquaris, J.-M. and Guisado, G. and Magarinos, M. and
Moreno, C. and Burauel, P. and Narres, H.-D. and Vereecken,
H.},
title = {{O}rganic-carbon fractions in an agricultural topsoil
assessed by the determination of the soil mineral surface
area},
journal = {Journal of plant nutrition and soil science},
volume = {173},
issn = {1436-8730},
address = {Weinheim},
publisher = {Wiley-VCH},
reportid = {PreJuSER-11859},
pages = {699 - 705},
year = {2010},
note = {We thank three anonymous reviewers and the Associate Editor
for their numerous valuable comments which helped to improve
the manuscript. This work was performed as part of the HGF
strategy fund project "Soil Functions" We thank C Walraf for
her skilful laboratory assistance and J. Borchardt
(Troposphere, ICG 2) for his help with the N<INF>2</INF>
gas-adsorption technique We are grateful to Dr. M. Kehl
(INRES, Bonn University) for the particle-size-distribution
analysis The elemental chemical analyses performed at the
Central Division of Analytical Chemistry (ZCH) are
gratefully acknowledged G Guisado (gregorig@ucr.edu), M. R.
Magarinos (rosario.magarinos-bernabe@basf.com), and C Moreno
(clkcarlos2@mixmail.com) on leave from the University of
Burgos (Spain) were supported by the European Community
(Erasmus Grant)},
abstract = {According to recent conceptual models, the organic carbon
(OC) of soils can be divided into OC fractions of increasing
stability from labile free OC to resistant OC associated
with the soil mineral phase. In this study, we present a
method for quantifying two OC fractions based on soil
aggregate-size fractionation and the N-2 gas-adsorption
method. For this purpose, we analyzed soil material of the
plow layer of a Haplic Chernozem subjected to different
fertilizer treatments (no fertilizer, mineral fertilizer,
mineral and organic fertilizer). The total organic-C
concentration (TOO) and the clay content of the different
size fractions were determined as well as the specific
surface area (SSA(mineral)) and the sample pore volume after
thermal oxidation (OC-free). The TOC of the different
soil-aggregate fractions was linearly related to
SSA(mineral). Clay-associated OC and nonassociated OC
fractions of the different soil samples were quantified
using two methods based on the OC surface loading at the
clay fraction. The application of organic fertilizer
increased the amount of nonassociated OC but hardly affected
the concentration of clay-associated OC. This finding agrees
with previous studies on C dynamics in soils and indicates a
finite capacity of soil materials to sequester OC. Even
without any addition of organic fertilizer, the mineral
phase of the analyzed soil material appears to be
C-saturated.},
keywords = {J (WoSType)},
cin = {ICG-4 / JARA-ENERGY},
ddc = {570},
cid = {I:(DE-Juel1)VDB793 / $I:(DE-82)080011_20140620$},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Agronomy / Plant Sciences / Soil Science},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000283628200008},
doi = {10.1002/jpln.200800224},
url = {https://juser.fz-juelich.de/record/11859},
}