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@ARTICLE{Glanville:820998,
author = {Glanville, H. C. and Hill, P. W. and Schnepf, A. and
Oburger, E. and Jones, D. L.},
title = {{C}ombined use of empirical data and mathematical modelling
to better estimate the microbial turnover of isotopically
labelled carbon substrates in soil},
journal = {Soil biology $\&$ biochemistry},
volume = {94},
issn = {0038-0717},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2016-06255},
pages = {154 - 168},
year = {2016},
abstract = {The flow of carbon (C) through soil is inherently complex
due to the many thousands of different chemical
transformations occurring simultaneously within the soil
microbial community. The accurate modelling of this C flow
therefore represents a major challenge. In response to this,
isotopic tracers (e.g. 13C, 14C) are commonly used to
experimentally parameterise models describing the fate and
residence time of individual C compounds within soil. In
this study, we critically evaluated the combined use of
experimental 14C labelling and mathematical modelling to
estimate C turnover times in soil. We applied 14C-labelled
alanine and glucose to an agricultural soil and
simultaneously measured their loss from soil solution
alongside the rate of microbial C immobilization and
mineralization. Our results revealed that chloroform
fumigation-extraction (CFE) cannot be used to reliably
quantify the amount of isotopically labelled 13C/14C
immobilised by the microbial biomass. This is due to
uncertainty in the extraction efficiency values (kec) within
the CFE methodology which are both substrate and incubation
time dependent. Further, the traditional mineralization
approach (i.e. measuring 14/13CO2 evolution) provided a poor
estimate of substrate loss from soil solution and mainly
reflected rates of internal microbial C metabolism after
substrate uptake from the soil. Therefore, while isotope
addition provides a simple mechanism for labelling the
microbial biomass it provides limited information on the
behaviour of the substrate itself. We used our experimental
data to construct a new empirical model to describe the
simultaneous flow of substrate-C between key C pools in
soil. This model provided a superior estimate of microbial
substrate use and microbial respiration flux in comparison
to traditional first order kinetic modelling approaches. We
also identify a range of fundamental problems associated
with the modelling of isotopic-C in soil, including issues
with variation in C partitioning within the community, model
pool connectivity and variation in isotopic pool dilution,
which make interpretation of any C isotopic flux data
difficult. We conclude that while convenient, the use of
isotopic data (13C, 14C, 15N) has many potential pitfalls
necessitating a critical evaluation of both past and future
studies.},
cin = {IBG-3},
ddc = {570},
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:000370094100016},
doi = {10.1016/j.soilbio.2015.11.016},
url = {https://juser.fz-juelich.de/record/820998},
}