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@ARTICLE{Kautz:128323,
author = {Kautz, Timo and Amelung, Wulf and Ewert, Frank and Gaiser,
Thomas and Horn, Rainer and Jahn, Reinhold and Javaux,
Mathieu and Kemna, Andreas and Kuzyakov, Yakov and Munch,
Jean-Charles and Pätzold, Stefan and Peth, Stephan and
Scherer, Heinrich W. and Schloter, Michael and Schneider,
Heike and Vanderborght, Jan and Vetterlein, Doris and
Walter, Achim and Wiesenberg, Guido L.B. and Köpke, Ulrich},
title = {{N}utrient acquisition from arable subsoils in temperate
climates: {A} review},
journal = {Soil biology $\&$ biochemistry},
volume = {57},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2013-00062},
pages = {1003 - 1022},
year = {2013},
abstract = {In arable farming systems, the term ‘subsoil’ refers to
the soil beneath the tilled or formerly tilled soil horizon
whereas the latter one is denoted as ‘topsoil’. To date,
most agronomic and plant nutrition studies have widely
neglected subsoil processes involved in nutrient acquisition
by crop roots. Based on our current knowledge it can be
assumed that subsoil properties such as comparatively high
bulk density, low air permeability, and poverty of organic
matter, nutrients and microbial biomass are obviously
adverse for nutrient acquisition, and sometimes subsoils
provide as little as less than $10\%$ of annual nutrient
uptake in fertilised arable fields. Nevertheless, there is
also strong evidence indicating that subsoil can contribute
to more than two-thirds of the plant nutrition of N, P and
K, especially when the topsoil is dry or nutrient-depleted.
Based on the existing literature, nutrient acquisition from
arable subsoils may be conceptualised into three major
process components: (I) mobilisation from the subsoil, (II)
translocation to the shoot and long-term accumulation in the
Ap horizon and (III) re-allocation to the subsoil. The
quantitative estimation of nutrient acquisition from the
subsoil requires the linking of field experiments with
mathematical modelling approaches on different spatial
scales including Process Based Models for the field scale
and Functional–Structural Plant Models for the plant
scale. Possibilities to modify subsoil properties by means
of agronomic management are limited, but ‘subsoiling’
– i.e. deep mechanical loosening – as well as the
promotion of biopore formation are two potential strategies
for increasing access to subsoil resources for crop roots in
arable soils. The quantitative role of biopores in the
nutrient acquisition from the subsoil is still unclear, and
more research is needed to determine the bioaccessibility of
nutrients in subsoil horizons.},
cin = {IBG-2 / IBG-3},
ddc = {570},
cid = {I:(DE-Juel1)IBG-2-20101118 / I:(DE-Juel1)IBG-3-20101118},
pnm = {242 - Sustainable Bioproduction (POF2-242) / 246 -
Modelling and Monitoring Terrestrial Systems: Methods and
Technologies (POF2-246)},
pid = {G:(DE-HGF)POF2-242 / G:(DE-HGF)POF2-246},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000317247100122},
doi = {10.1016/j.soilbio.2012.09.014},
url = {https://juser.fz-juelich.de/record/128323},
}