Soil Biology and Biochemistry,
Journal Year:
2024,
Volume and Issue:
197, P. 109535 - 109535
Published: July 14, 2024
Microbial
processes
mediating
the
cycling
of
carbon
and
nutrients
in
soils
are
complex
thus
difficult
to
predict
with
mathematical
models.
Such
complexity
arises
because
biological
ecological
dynamics
interact
physical
soil
shape
patterns
resource
acquisition
use,
ultimately
organic
matter
stabilization
soil.
In
article
collection
"Advances
Modelling
Soil
Dynamics"
(https://www.sciencedirect.com/special-issue/10DG8MTGCCF),
novel
approaches
tackle
these
complexities
presented.
This
perspective
summarizes
their
findings
by
highlighting
theoretical
advances
outstanding
challenges
modelling
microbial
constraints.
Geoderma,
Journal Year:
2024,
Volume and Issue:
443, P. 116851 - 116851
Published: March 1, 2024
Globally,
soils
hold
approximately
half
of
ecosystem
carbon
and
can
serve
as
a
source
or
sink
depending
on
climate,
vegetation,
management,
disturbance
regimes.
Understanding
how
soil
dynamics
are
influenced
by
these
factors
is
essential
to
evaluate
proposed
natural
climate
solutions
policy
regarding
net
balance.
Soil
microbes
play
key
role
in
both
fluxes
stabilization.
However,
biogeochemical
models
often
do
not
specifically
address
microbial-explicit
processes.
Here,
we
incorporated
processes
into
the
DayCent
model
better
represent
large
perennial
grasses
mechanisms
formation
We
also
take
advantage
recent
improvements
grass
structural
complexity
life-history
traits.
Specifically,
this
study
focuses
on:
1)
plant
sub-model
that
represents
phenology
more
refined
chemistry
with
downstream
implications
for
organic
matter
(SOM)
cycling
though
litter
inputs,
2)
live
dead
microbe
pools
influence
routing
physically
protected
unprotected
pools,
3)
Michaelis-Menten
kinetics
rather
than
first-order
decomposition
calculations,
4)
feedbacks
between
microbial
pools.
evaluated
performance
two
SOM
sub-models,
(MM)
(FO),
using
observations
production,
respiration,
biomass,
from
long-term
bioenergy
research
plots
mid-western
United
States.
The
MM
represented
seasonal
FO
which
consistently
overestimated
winter
respiration.
While
sub-models
were
similarly
calibrated
total,
protected,
measurements,
differed
future
response
most
notably
Adding
will
improve
predictions
balances
but
data
necessary
validate
change
responses
pool
allocation.
Carbon Balance and Management,
Journal Year:
2024,
Volume and Issue:
19(1)
Published: May 29, 2024
Abstract
Climate-smart
agriculture
can
be
used
to
build
soil
carbon
stocks,
decrease
agricultural
greenhouse
gas
(GHG)
emissions,
and
increase
agronomic
resilience
climate
pressures.
The
US
recently
declared
its
commitment
include
the
sector
as
part
of
an
overall
climate-mitigation
strategy,
with
this
comes
need
for
robust,
scientifically
valid
tools
GHG
flux
measurements
modeling.
If
is
contribute
significantly
mitigation,
practice
adoption
should
incentivized
on
much
land
area
possible
mitigation
benefits
accurately
quantified.
Process-based
models
are
parameterized
data
from
a
limited
number
long-term
experiments,
which
may
not
fully
reflect
outcomes
working
farms.
Space-for-time
substitution,
paired
studies,
monitoring
SOC
stocks
emissions
commercial
farms
using
variety
climate-smart
management
systems
validate
findings
experiments
provide
process-based
model
improvements.
Here,
we
describe
project
that
worked
collaboratively
producers
in
Midwest
directly
measure
organic
(SOC)
their
at
field
scale.
We
study,
several
unexpected
challenges
encountered,
facilitate
further
on-farm
collection
creation
secure
database
stock
measurements.
Agronomy,
Journal Year:
2023,
Volume and Issue:
13(7), P. 1783 - 1783
Published: June 30, 2023
The
return
of
crop
residues
and
application
chemical
nitrogen
(N)
can
influence
the
soil
organic
carbon
(SOC)
turnover.
However,
changes
in
response
priming
effect
(PE)
to
N
management
real
farming
systems
are
not
fully
understood.
In
this
research,
we
launched
a
270-day
situ
experiment
three
plots
(N0,
no
N;
N1,
300
kg
hm−2;
N2,
360
hm−2)
on
long-term
maize
farm
order
examine
microbial
mechanisms
that
trigger
PE
presence
13C-labeled
residues.
We
found
N1
decreased
SOC
mineralization
positive
PE,
but
increased
residual
C
use
efficiency
comparison
with
N0
respectively.
be
explained
by
nutrient
mining
theory
for
stoichiometry
decomposition
as
reflected
abundance
oligotrophic
phyla
copiotrophic
N2.
biomass
(MBC),
residue-derived
MBC,
communities’
complexity
were
N2
due
acidification
environment,
enhanced
bacterial
complexity.
keystone
taxa
Vicinamibacteraceae
Gemmatimonas
preferred
recalcitrant
Acidibacter
favored
labile
N1.
fungal
Penicillium,
Sarocladium,
Cladophialophora
exhibited
wide
substrate-use
abilities
N0,
Our
research
depicts
how
structures
reshaped
through
emphasizes
functions
turnover
systems.
Soil Biology and Biochemistry,
Journal Year:
2024,
Volume and Issue:
197, P. 109535 - 109535
Published: July 14, 2024
Microbial
processes
mediating
the
cycling
of
carbon
and
nutrients
in
soils
are
complex
thus
difficult
to
predict
with
mathematical
models.
Such
complexity
arises
because
biological
ecological
dynamics
interact
physical
soil
shape
patterns
resource
acquisition
use,
ultimately
organic
matter
stabilization
soil.
In
article
collection
"Advances
Modelling
Soil
Dynamics"
(https://www.sciencedirect.com/special-issue/10DG8MTGCCF),
novel
approaches
tackle
these
complexities
presented.
This
perspective
summarizes
their
findings
by
highlighting
theoretical
advances
outstanding
challenges
modelling
microbial
constraints.