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@ARTICLE{Agnelli:172188,
author = {Agnelli, A. and Bol, R. and Trumbore, S. E. and Dixon, L.
and Cocco, S. and Corti, G.},
title = {{C}arbon and nitrogen in soil and vine roots in harrowed
and grass-covered vineyards},
journal = {Agriculture, ecosystems $\&$ environment},
volume = {193},
issn = {0167-8809},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2014-05685},
pages = {70 - 82},
year = {2014},
abstract = {To examine the effects of vineyard soil management on soil
C and N content and quality, we studied harrowed and
grass-covered vineyards on a soil developed on
plio-pleistocene, marine sediments. A soil naturally covered
by grasses adjacent to the vineyards served as control. To
reach this goal, we assessed (1) the distribution of C and N
and their 13C and 15N signatures in different soil organic
matter pools, (2) the amount of C and N as live and dead
vine fine roots and their 13C, 15N and 14C signatures, and
(3) the stocks of C and N forms accumulated at two
soil-depth intervals (0–50 and 50–100 cm).Independent of
the soil management, the vines increased the total organic C
and total N content in the deeper soil horizons because of
root turnover and rhizodeposition processes. In the upper
horizons, a greater organic matter accumulation was fostered
by the presence of the grass cover and the absence of
tillage. The grass cover favoured the organic C storage
mainly in the form of particulate and highly stabilised
organic matter (humic acids and humin), and reduced the soil
N content by plant uptake, whereas the harrowing produced a
greater abundance of fulvic acids, which were mainly
ascribed to oxidative processes enhanced by the soil
tillage. In both vineyard soils, decaying vine roots
represented an important source of organic C and N,
especially in the deepest horizons. Indeed, isotope analyses
revealed a more intense degradation of the dead vine roots
in the deeper soil portion, where they likely constituted
the main substrate for soil microorganisms. In the deepest
horizons of the grass-covered vineyard, the greater mean
residence time of the decaying vine roots and the lower root
production were attributed to the easily available energetic
substrates supplied by grass root turnover and
rhizodeposition, which were preferentially used by
microorganisms. This fact fostered a larger C accumulation
in the grass-covered than in the harrowed vineyard.},
cin = {IBG-3},
ddc = {330},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {246 - Modelling and Monitoring Terrestrial Systems: Methods
and Technologies (POF2-246) / 255 - Terrestrial Systems:
From Observation to Prediction (POF3-255)},
pid = {G:(DE-HGF)POF2-246 / G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000338618400008},
doi = {10.1016/j.agee.2014.04.023},
url = {https://juser.fz-juelich.de/record/172188},
}