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@INPROCEEDINGS{Uhlig:1007635,
author = {Uhlig, David and Wu, Bei and Berns, Anne E. and Amelung,
Wulf},
title = {{T}esting {M}g stable isotopes as a potential geochemical
tool in agronomy},
reportid = {FZJ-2023-02127},
year = {2022},
abstract = {A sustainable use of soil resources is urgently required to
cope with the increasing demand for agricultural products
during climate change. Advanced soil cultivation methods
like subsoil management were suggested but analytical tools
to measure changes in the nutrient use efficiency of crops
are still missing. Here we tested the applicability of Mg
stable isotopes as novel evaluation tool in agronomy. To
this end, we conceptually demonstrated under which
conditions changes in the Mg isotope composition (26Mg)
of crops and the bioavailable fraction of Mg in soils
containing low, middle, and high inventories of exchangeable
Mg could be resolved from analytical uncertainty, when
simulating subsoil management. We found that shifts in
26Mg values are only detectable if i) the crop
uptake-related Mg isotope fractionation factor is at the
upper end of hitherto published fractionation factors, ii) a
high Mg uptake flux of crops is matched by a low Mg supply
from the exchangeable fraction, and iii) subsoil management
causes a considerable deepening of the rooting system.We
tested our concept on field trials, where deep loosening
with and without the incorporation of compost was conducted
on Luvisols. Shifts in 26Mg values of crops and the
exchangeable fraction of Mg in soil were mostly unresolvable
from the analytical uncertainty, which positively tested the
Mg isotope concept for well nurtured soils. Yet, systematic
shifts in 26Mg values among crops cultivated on and
beside a melioration strip were found and attributed to the
uplift of isotopically distinct compost-derived Mg on the
melioration strip and root restricting layers beside the
melioration strip. Also, field-based crop uptake-related
‘apparent’ Mg isotope fractionation factors of winter
wheat and spring barley were determined, which differed from
one another. However, the quantitative approach of Mg
isotopes was violated when lime or Mg-carbonate containing
fertilizer were applied to the field. In these cases, the
isotope-derived difference in the Mg use efficiency were
likely caused by the uneven distribution of lime-derived Mg
with depth. Hence, using Mg stable isotopes as a new
geochemical routine for agronomy will require further work
to allow low-demanding, minimally invasive sampling of the
soil-plant system.},
month = {Jul},
date = {2022-07-10},
organization = {Goldschmidt Hawaii 2022, Honolulu
(USA), 10 Jul 2022 - 15 Jul 2022},
subtyp = {Other},
cin = {IBG-3},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217) / BonaRes - (Modul A, Phase 2): Soil3-II -
Nachhaltiges Unterbodenmanagement, Teilprojekt C
(031B0515C)},
pid = {G:(DE-HGF)POF4-2173 / G:(BMBF)031B0515C},
typ = {PUB:(DE-HGF)6},
url = {https://juser.fz-juelich.de/record/1007635},
}