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@ARTICLE{Xu:887684,
author = {Xu, Yingde and Sun, Liangjie and Lal, Rattan and Bol,
Roland and Wang, Yang and Gao, Xiaodan and Ding, Fan and
Liang, Siwei and Li, Shuangyi and Wang, Jingkuan},
title = {{M}icrobial assimilation dynamics differs but total
mineralization from added root and shoot residues is similar
in agricultural {A}lfisols},
journal = {Soil biology $\&$ biochemistry},
volume = {148},
issn = {0038-0717},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2020-04345},
pages = {107901 -},
year = {2020},
abstract = {Microbial transformation of crop residue is the key process
of soil organic matter (SOM) formation and mineralization,
which determines soil fertility and affects global climate
change. However, utilization dynamics of residue-derived
carbon (residue C) by various microbial communities is still
not well understood, especially under different residue
quality and soil fertility conditions over a long-term scale
(i.e., >1 year). In this study, a 500-day in-situ field
experiment was conducted using 13C-labeled maize (Zea mays
L.) root and shoot (composed of both stem and leaf) to
examine the role of microbial community composition on the C
processing. Specifically, the mineralization of residue C
and incorporation of residue C into microbial biomass in low
fertility (LF) and high fertility (HF) soils were
investigated. The abundance of 13C in soil samples and
microbial phospholipid fatty acids (PLFAs) were measured
after 60, 90, 150 and 500 days since the residues added. The
results showed that the mineralization rate of residue C was
significantly higher in the LF than that in the HF soil for
the first 150 days, and the shoot-derived C was more
susceptible to degradation than root-derived C, but the
final mineralization rates $(~78\%)$ were not significantly
different among treatments on the day 500. Soil fertility
significantly affected the relative composition of different
microbial groups and distribution of residue C in microbial
communities, but residue type did not do so. Furthermore,
residue C contributed more to PLFA-C pool in the LF than HF
treatments, and the proportion of root C in PLFA-C pool was
higher than that of shoot C, indicating easier
immobilization of root C by soil microbial anabolism.
Accordingly, soil fertility and residue quality could both
regulate the kinetics of the microbial immobilization of
crop residue C, but overall the available residual quantity
of applied (plant-derived) C to enhance or maintain soil C
pool did not depend on them in a long term in the
agricultural Alfisols.},
cin = {IBG-3},
ddc = {540},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000566668900033},
doi = {10.1016/j.soilbio.2020.107901},
url = {https://juser.fz-juelich.de/record/887684},
}