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@ARTICLE{Herbst:1044978,
author = {Herbst, Michael and Mohammed, Gihan and Eichler-Löbermann,
Bettina and Amelung, Wulf and Vanderborght, Jan and Siebers,
Nina},
title = {{L}inking {M}easurable {P}hosphorus {P}ools {W}ith
{S}imulations of {S}oil {P} {D}ynamics: {R}esults for the
{L}ong‐{T}erm {E}xperiment ‘{R}ostock’},
journal = {European journal of soil science},
volume = {76},
number = {4},
issn = {0022-4588},
address = {Oxford [u.a.]},
publisher = {Wiley-Blackwell},
reportid = {FZJ-2025-03468},
pages = {e70160},
year = {2025},
abstract = {Phosphorus (P) is removed from agroecosystems through
harvesting, and sustainable management must include P
fertiliza-tion as P availability affects crop performance.
However, accurate assessment of plant- available P is
challenging. In this study,two promising approaches are
combined to assess the plant- available P of a 22- year
long- term experiment (LTE) near Rostock,Germany. We
hypothesize agreement between a modern P test method and
process- based model estimates of plant- availableP. The
diffusive gradients in thin films (DGT) technique offers an
accurate P test method because it mimics the diffusion
anddesorption of soil P in the presence of root uptake. This
was applied in a synergetic combination with a state-
of- the- art agroeco-system model that was extended with
a P cycling module. The simulations and yearly DGT- P
analyses comprise 4 treatments: noP fertilization, mineral P
fertilization with triple- superphosphate, organic P
fertilization with compost, and mineral plus organicP
fertilization. Soils at 0–30 cm depth were sampled in four
replicates on a yearly basis between 1999 and 2021. In
addition, a Pfractionation was applied for 2015 using the
Hedley approach, which made it possible to link non-
plant- available, steady P frac-tions with the respective
model pools. The comparison between DGT- P determined
plant- available P up to a depth of 30 cm andthat
estimated from the pools of the agroecosystem model AgroC
showed agreement with respect to the differences between
thetreatments and with respect to the temporal evolution (R2
between 0.65 and 0.7). Less agreement was detected for
DGT- P and therespective model pools in deeper soil. A
closer match over soil depth was found between grouped
Hedley P fractions and AgroCmodel pools. Both, model and
DGT- P analyses indicate that a new plant- available P
equilibrium will be established under thenew P management
after about 12 years for the Rostock site, which points to
the resilience of P cycling in agroecosystems. Weconclude
that the combined application of DGT- P analysis and
agroecosystem modeling offers a robust and accurate
quantifica-tion of plant- available P in the plough layer
and can be used to create an agricultural digital twin with
respect to soil P availabilityand its impact on crop yield.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217)},
pid = {G:(DE-HGF)POF4-2173},
typ = {PUB:(DE-HGF)16},
doi = {10.1111/ejss.70160},
url = {https://juser.fz-juelich.de/record/1044978},
}