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@ARTICLE{He:256541,
author = {He, Yao and Siemens, Jan and Amelung, Wulf and Goldbach,
Heiner and Wassmann, Reiner and Alberto, Ma. Carmelita R.
and Lücke, Andreas and Lehndorff, Eva},
title = {{C}arbon release from rice roots under paddy rice and
maize-paddy rice cropping},
journal = {Agriculture, ecosystems $\&$ environment},
volume = {210},
issn = {0167-8809},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2015-06425},
pages = {15-24},
year = {2015},
abstract = {Crop rotations encompassing flooded rice and an upland crop
are commonly found in large parts of South and East Asia.
However, also rice farmers in Southeast Asia increasingly
switch from double-cropping paddy rice to one non-flooded
crop–such as maize–in the dry season. We hypothesized
that introducing maize (maize–paddy rice, M-MIX) into a
double paddy rice (R-WET) cropping system will increase
carbon (C) release from rice roots into the rhizosphere and
the dissolved soil C pool. To test this hypothesis we
assessed the kinetics of C release by the rice plants in a
hydroponic greenhouse experiment, and used these data for
interpreting their C release in field experiments using 13C
pulse labeling of rice plants. In the greenhouse we observed
that rice roots released 13C labeled dissolved organic
carbon (DOC) for 21 days with a mean residence time (MRT) of
19 days after exposure to a 13CO2 pulse. The MRT of labeled
dissolved inorganic carbon (DIC) released from rice roots
was only 2 days. In the field 13CO2 pulse labeling increased
the 13C excess of rhizosphere soil up to 0.7 ± 0.2 mg 13C
kg−1 in R-WET and 0.9 ± 0.3 mg kg−1 in M-MIX. The 13C
signature of bulk soil remained unaffected. DOC
concentrations in R-WET were significantly higher than in
M-MIX during the mature grain stage of the rice plants.
Nevertheless, the 13C excess in DOC transiently increased by
only 0.5 μg L−1 after labeling in 13 cm depth in one of
three lysimeters previously cropped with maize (M-MIX),
while no labeled DOC was detected in 13 cm depth of the
R-WET lysimeters and in 60 cm depth of both treatments. In
contrast, the 13C excess of DIC increased by 42.4–93.1 μg
L−1 a few days after labeling with a MRT of 53–66 days
in both treatments. Considering the results of the
greenhouse experiment, this suggests a rapid mineralization
of labeled rhizodeposits in the field and an effective
transient storage of CO2 produced by respiration in soil
water.},
cin = {IBG-3},
ddc = {330},
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:000356996900003},
doi = {dx.doi.org/10.1016/j.agee.2015.04.029},
url = {https://juser.fz-juelich.de/record/256541},
}