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@ARTICLE{MenezesBlackburn:902960,
author = {Menezes-Blackburn, Daniel and Bol, Roland and Klumpp, Erwin
and Missong, Anna and Nischwitz, Volker and Haygarth, Philip
M.},
title = {{C}itric {A}cid {E}ffect on the {A}bundance, {S}ize and
{C}omposition of {W}ater-{D}ispersible {S}oil {C}olloids and
{I}ts {R}elationship to {S}oil {P}hosphorus {D}esorption:
{A} {C}ase {S}tudy},
journal = {Journal of soil science and plant nutrition},
volume = {21},
number = {3},
issn = {0717-635X},
address = {[Cham]},
publisher = {Springer International Publishing},
reportid = {FZJ-2021-04706},
pages = {2436 - 2446},
year = {2021},
abstract = {Citric acid exudation by plant roots is often linked to the
mobilisation of recalcitrant soil phosphorus (P) for plant
nutrition. In this case study, we have explored the effect
of citric acid on the abundance, size and composition of
water-dispersible soil colloids (WDC) to understand the
mineral source of desorbed P and the chemical nature of
P-carrying mobilized colloids. After incubation with citric
acid, WDC were isolated using a soil particle-size
fractionation method consisting of sedimentation,
centrifugation and syringe filtration. The size range and
composition of WDC was assessed using field-flow
fractionation (FFF), combined with inductively coupled
plasma mass spectrometry (ICP-MS) and UV spectrometry, for
in vitro P desorption assay samples under the influence of
increasing doses of citric acid. Three sharp and
well-defined FFF particle size fractions of WDC containing P
(12–23, 23–36 and 36–300 nm), with elution times
matching carbon (C) peaks and offset from Fe, Al and Si
fractions. The concentration of soluble or WDC-associated P,
C, Fe, Al and Si increased in response to increasing citric
acid doses. Silica colloids were only detected using syringe
filtration below 5 µm. The Si, Fe and Al-containing fine
colloid fractions (< 600 nm) were positively correlated
with P (de)sorption parameters measured by diffusive
gradient in thin films in previous work. The P desorbed by
citric acid originated predominantly from the disaggregation
of Fe and Al oxides and silicate clays. The citric acid
effect on mobilizing organic P carrying WDC fractions may
increase soil organic P cycling and availability to plants.},
cin = {IBG-3},
ddc = {570},
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},
UT = {WOS:000663268800001},
doi = {10.1007/s42729-021-00534-9},
url = {https://juser.fz-juelich.de/record/902960},
}