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@ARTICLE{Konrad:1039723,
author = {Konrad, Alexander and Hofmann, Diana and Siemens, Jan and
Stutz, Kenton P. and Lang, Friederike and Mulder, Ines},
title = {{M}icrobial carbon use efficiency of mineral-associated
organic matter is related to its desorbability},
journal = {Soil biology $\&$ biochemistry},
volume = {203},
issn = {0038-0717},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2025-01771},
pages = {109740},
year = {2025},
abstract = {Interactions between organic substances, minerals, and
microorganisms are crucial for organic carbon
(OC)stabilization in soil. We hypothesized that thresholds
of sorption strength (described by the sorption coefficient
ofthe Freundlich isotherms) and desorbability (i.e., the
ratio of the amount desorbed to the amount sorbed) oforganic
monomers control the extent of their microbial
processing.Freundlich sorption isotherms and desorbability
of uniformly 14C-labeled glucose,
acetylglucosamine,phenylalanine, salicylic acid, and citric
acid onto goethite, kaolinite, and illite were studied in
batch experiments.Monomers adsorbed to minerals were mixed
with loamy and sandy arable topsoil and incubated at 25
◦C.Mineralization of mineral-adsorbed monomers was
observed over three weeks, after which the assimilation
intomicrobial biomass, and the 14C remaining in soil were
quantified. Subsequently, the mineralization of
incubatedsoils was observed for additional three weeks after
glucose priming.The adsorption of carboxylic acids onto
minerals exceeded that of (amino) sugars and phenylalanine,
with theoverall highest amounts both adsorbed and retained
after desorption with water for goethite. Assimilation
ofmonomer 14C into microbial biomass and the microbial
carbon use efficiency (CUE) of mineral-adsorbedmonomers in
both soils increased linearly with the monomer desorbability
from mineral phases. Furthermore,the CUEs of monomers
adsorbed to goethite were lower than those of the same
monomers adsorbed to clayminerals. In terms of total amount
of carbon retained in the soil, carboxylic acids adsorbed on
goethite showedhighest values, emphasizing the significance
of oxides for the stabilization of OC within soils. Priming
of incu-bated soil with non-labeled glucose caused an
additional mineralization of monomer-C, with the priming
effectdecreasing from goethite to clay minerals.We conclude
that sorption strength and desorbability shape microbial
utilization of mineral-bound organiccompounds, but no
universal thresholds determine bio-accessibility of sorbed
organic compounds.},
cin = {IBG-3},
ddc = {540},
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:001427425600001},
doi = {10.1016/j.soilbio.2025.109740},
url = {https://juser.fz-juelich.de/record/1039723},
}