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@ARTICLE{Mukherjee:281970,
author = {Mukherjee, Santanu and Weihermüller, Lutz and Tappe,
Wolfgang and Vereecken, Harry and Burauel, Peter},
title = {{M}icrobial respiration of biochar- and digestate-based
mixtures},
journal = {Biology and fertility of soils},
volume = {52},
number = {2},
issn = {0178-2762},
address = {Berlin},
publisher = {Springer},
reportid = {FZJ-2016-01614},
pages = {151 - 164},
year = {2016},
abstract = {The addition of biochar or digestate as organic amendments
to soils is currently controversially discussed with regard
to its positive and negative effects on C mineralization.
Organic amendments are generally applied to agricultural
fields to improve soil quality and crop yield. In this
study, we present results from short-term respiration
experiments (90 days), where two different biochars
(produced at 400 and 800 °C) as well as digestate from
biogas production were added in different combinations to
two soils (loamy sand and silt loam). Additionally, both
amendments were mixed together into the soil to study
interactions between biochar and digestate effects and
investigate the interactions of both amendments with clay
minerals resulting in a total of 13 mixtures (plus control
soils) per soil type. The results indicate that the rate of
CO2 evolution was not proportional to the amount of C added
to the systems indicating a saturation effect in the C
degradation mechanism. More than 40 $\%$ of the digestate C
was released as CO2 and only 3 $\%$ for the biochar soil
mixture; the recalcitrant nature of biochar and its
suitability for short-term C stabilization in soils
(incubation period of 90 days) were shown. Surprisingly, a
much lower CO2 release (up to 11-fold) was observed in
soil/digestate/biochar compared to soil/digestate mixtures
without biochar. This effect was observed even when only 1
$\%$ (w/w) biochar was added to the digestate/soil mixtures,
indicating that the biochar changed the physicochemical
properties of the system. Additional dissolved organic C
(DOC) sorption experiments revealed that large quantities of
DOC can be sorbed by the biochar reducing the microbial
accessible DOC in the liquid phase and as a consequence also
the CO2 production.},
cin = {IBG-3},
ddc = {630},
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:000373441100003},
doi = {10.1007/s00374-015-1060-x},
url = {https://juser.fz-juelich.de/record/281970},
}