Abstract.
Sources
and
transformation
of
carbon
(C)
were
quantified
using
mass
balance
ecosystem
metabolism
data
for
the
upper
segments
James,
Pamunkey
Mattaponi
estuaries.
The
goal
was
to
assess
role
external
(river
inputs
tidal
exchange)
vs.
internal
(metabolism)
drivers
in
influencing
forms
fluxes
C.
C
their
response
river
discharge
differed
among
estuaries
based
on
physiographic
setting.
which
receives
bulk
from
upland
areas
(Piedmont
Mountain),
exhibited
a
higher
ratio
inorganic
organic
larger
particulate
(POC).
receive
greater
proportion
lowland
(Coastal
Plain)
areas,
characterized
by
low
dissolved
(DIC)
POC
elevated
(DOC).
I
anticipated
that
transport
processes
would
dominate
during
colder
months
when
is
biological
predominate
summer,
leading
attenuation
throughputs
via
degassing
CO2.
Contrary
expectations,
highest
retention
occurred
periods
high
throughput,
as
resulted
loading
POC.
In
cycling
production
respiration
large
comparison
forcing
despite
riverine
influence
these
upper-estuarine
segments.
found
be
net
heterotrophic
C,
export
DIC,
primary
relative
flux
class="inline-formula">2
atmosphere.
contributions
phytoplankton
closer
between
respiration,
with
autochthonous
exceeding
allochthonous
inputs.
Combining
bioenergetics
provided
basis
estimating
utilized
dominant
metazoan.
findings
suggest
invasive
catfish
utilize
15
%
total
up
40
James.
Environmental Science & Technology,
Journal Year:
2023,
Volume and Issue:
57(12), P. 4701 - 4719
Published: March 13, 2023
High-frequency
water
quality
measurements
in
streams
and
rivers
have
expanded
scope
sophistication
during
the
last
two
decades.
Existing
technology
allows
situ
automated
of
constituents,
including
both
solutes
particulates,
at
unprecedented
frequencies
from
seconds
to
subdaily
sampling
intervals.
This
detailed
chemical
information
can
be
combined
with
hydrological
biogeochemical
processes,
bringing
new
insights
into
sources,
transport
pathways,
transformation
processes
particulates
complex
catchments
along
aquatic
continuum.
Here,
we
summarize
established
emerging
high-frequency
technologies,
outline
key
hydrochemical
data
sets,
review
scientific
advances
focus
areas
enabled
by
rapid
development
rivers.
Finally,
discuss
future
directions
challenges
for
using
bridge
management
gaps
promoting
a
holistic
understanding
freshwater
systems
catchment
status,
health,
function.
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
27(16), P. 3923 - 3938
Published: May 2, 2021
Abstract
Soil
respiration
(Rs),
the
efflux
of
CO
2
from
soils
to
atmosphere,
is
a
major
component
terrestrial
carbon
cycle,
but
poorly
constrained
regional
global
scales.
The
soil
database
(SRDB)
compilation
in
situ
Rs
observations
around
globe
that
has
been
consistently
updated
with
new
measurements
over
past
decade.
It
unclear
whether
addition
data
versions
produced
better‐constrained
estimates.
We
compared
two
SRDB
(v3.0
n
=
5173
and
v5.0
10,366)
determine
how
additional
influenced
annual
sum,
spatial
patterns
associated
uncertainty
(1
km
resolution)
using
machine
learning
approach.
A
quantile
regression
forest
model
parameterized
SRDBv3
yielded
sum
88.6
Pg
C
year
−1
,
29.9
(mean
absolute
error)
57.9
(standard
deviation)
whereas
parameterization
SRDBv5
96.5
30.2
average
73.4
.
Empirically
estimated
heterotrophic
(Rh)
v3
v5
were
49.9–50.2
50.1)
53.3–53.5
53.4)
respectively.
SRDBv5’s
inclusion
underrepresented
regions
(e.g.,
Asia,
Africa,
South
America)
resulted
overall
higher
uncertainty.
largest
differences
between
models
different
SRDVB
arid/semi‐arid
regions.
still
biased
toward
northern
latitudes
temperate
zones,
so
we
tested
an
optimized
distribution
measurements,
which
96.4
±
21.4
lower
These
results
support
current
estimates
highlight
biases
influence
interpretation
provide
insights
for
design
environmental
networks
improve
global‐scale
Frontiers in Water,
Journal Year:
2023,
Volume and Issue:
5
Published: May 31, 2023
River
corridors
integrate
the
active
channels,
geomorphic
floodplain
and
riparian
areas,
hyporheic
zone
while
receiving
inputs
from
uplands
groundwater
exchanging
mass
energy
with
atmosphere.
Here,
we
trace
development
of
contemporary
understanding
river
perspectives
geomorphology,
hydrology,
ecology,
biogeochemistry.
We
then
summarize
models
corridor
along
multiple
axes
including
dimensions
space
time,
disturbance
regimes,
connectivity,
hydrochemical
exchange
flows,
legacy
effects
humans.
explore
how
science
can
be
advanced
a
critical
framework
by
moving
beyond
primary
focus
on
discharge-based
controls
toward
multi-factor
that
identify
dominant
processes
thresholds
make
predictions
serve
society.
opportunities
to
investigate
relationships
between
large-scale
spatial
gradients
local-scale
processes,
embrace
riverine
are
temporally
variable
interacting,
acknowledge
services
do
not
respect
disciplinary
boundaries
increasingly
need
integrated
multidisciplinary
investigations,
explicitly
humans
their
management
actions
as
part
corridor.
intend
our
review
stimulate
cross-disciplinary
research
recognizing
occupy
unique
position
Earth's
surface.
Abstract
Processes
that
drive
variability
in
catchment
solute
sourcing,
transformation,
and
transport
can
be
investigated
using
concentration–discharge
(C–Q)
relationships.
These
relationships
reflect
in‐stream
processes
operating
across
nested
temporal
scales,
incorporating
both
short
long‐term
patterns.
Scientists
therefore
leverage
catchment‐scale
C–Q
datasets
to
identify
distinguish
among
the
underlying
meteorological,
biological,
geological
export
patterns
from
catchments
influence
shape
of
their
respective
We
have
synthesized
current
knowledge
regarding
geological,
meteorological
on
for
various
types
diel
decadal
time
scales.
cross‐scale
linkages
tools
researchers
use
explore
these
interactions
Finally,
we
gaps
our
understanding
dynamics
as
reflections
processes.
also
lay
foundation
developing
an
integrated
approach
investigate
relationships,
reflecting
biogeochemical
effects
environmental
change
water
quality.
This
article
is
categorized
under:
Science
Water
>
Hydrological
Quality
Environmental
Change
Frontiers in Water,
Journal Year:
2023,
Volume and Issue:
5
Published: March 13, 2023
The
concurrent
reduction
in
acid
deposition
and
increase
precipitation
impact
stream
solute
dynamics
complex
ways
that
make
predictions
of
future
water
quality
difficult.
To
understand
how
changes
have
influenced
dissolved
organic
carbon
(DOC)
nitrogen
(N)
loading
to
streams,
we
investigated
trends
from
1991
2018
concentrations
(DOC,
~3,800
measurements),
(DON,
~1,160
inorganic
N
(DIN,
~2,130
measurements)
a
forested
watershed
Vermont,
USA.
Our
analysis
included
concentration-discharge
(C-Q)
relationships
Seasonal
Mann-Kendall
tests
on
long-term,
flow-adjusted
concentrations.
whether
hydrologic
flushing
long-term
patterns
by
liberating
DOC
soils,
measured
their
the
leachate
108
topsoil
cores
5
cm
diameter
flushed
with
solutions
simulating
high
low
during
four
different
seasons.
results
indicate
DON
often
co-varied
both
dataset
soil
core
experiment.
Additionally,
winter
produced
especially
all
three
solutes.
This
seasonal
signal
was
consistent
C-Q
relation
showing
materials
(e.g.,
DON),
which
accumulate
winter,
are
into
streams
spring
snowmelt.
Acid
had
opposite
effects
compared
DIN
Low
solutions,
mimic
present
day
precipitation,
highest
Conversely,
generally
These
increasing
trend
decreasing
observed
data.
suggest
liberation
(C)
differed
for
vs.
DIN,
these
impacts
were
reflected
chemistry
patterns.
As
watersheds
continue
recover
deposition,
C:N
ratios
will
likely
increase,
important
consequences
metabolism
biogeochemical
processes.
Water Resources Research,
Journal Year:
2025,
Volume and Issue:
61(2)
Published: Feb. 1, 2025
Abstract
Many
agricultural
landscapes
have
undergone
significant
modifications
to
drain
farmland
and
improve
crop
productivity.
Subsurface
field
drainage,
ditching
channelization
of
streams
limit
opportunities
for
biogeochemical
processing
carbon
nutrients
within
the
channel
network.
In
this
study,
we
used
spatially
rich
water
quality
data
collected
from
two
contrasting
regions
an
watershed
in
south‐central
Minnesota,
USA
assess
how
features,
such
as
channelization,
tile
presence
lakes
or
wetlands,
influence
nitrate
(NO
3
−
)
dissolved
organic
(DOC).
channelized
upstream
region,
land
use
is
predominantly
(>92%)
with
subsurface
drainage
commonly
discharging
directly
stream
channel.
Further
downstream,
more
natural
increasing
including
riparian
wetlands.
We
concept
reach
leverage
interpret
behavior
(i.e.,
source
vs.
sink)
each
region
watershed.
Results
indicate
variability
between
distinct
regions,
suggesting
that
characteristics
lentic
waters
play
a
role
regulating
processing.
The
upstream,
acts
primarily
conservative
transporter
small
both
NO
DOC
across
sampling
dates.
contrast,
lentic‐influenced
exhibited
shifts
sink
over
time,
especially
,
influenced
by
factors
hydrologic
connectivity
discharge.
These
findings
highlight
value
collecting
resolved
enhance
our
understanding
which
may
be
useful
inform
effective
management
conservation
strategies.
Journal of Geophysical Research Biogeosciences,
Journal Year:
2025,
Volume and Issue:
130(4)
Published: March 27, 2025
Abstract
Headwater
streams
make
up
nearly
80%
of
the
stream
network
by
length
and
play
an
important
role
in
shaping
physical,
chemical,
biological
functions
downstream
waters.
In
Southeastern
US,
these
systems
are
beginning
to
experience
increases
frequency
duration
drying,
but
it
is
unclear
how
increased
drying
will
impact
water
quality.
To
begin
address
this
issue,
we
examined
nitrogen
dynamics
a
forested
headwater
across
annual
event.
The
event
was
divided
into
seasonal
wet
(March–June),
dry‐down
(June–October),
rewet
(November–March)
periods.
We
used
combination
quality
sensors
at
watershed
outlet,
spatially
distributed
synoptic
sampling
net
denitrification
conditions
physicochemical
variables
watershed,
series
potential
experiments
examine
variation
biogeochemical
state
At
nitrate
concentrations
were
positively
correlated
with
watershed‐scale
connectivity
during
period,
while
streamflow
period.
Throughout
varied
more
seasons
than
space,
greater
Further,
temperature,
nitrate,
ammonium
inversely
related
streamflow.
Finally,
measurements
confirmed
period
experienced
highest
rates.
Our
results
highlight
connection
between
humid
systems,
providing
key
information
for
developing
predictive
understanding
streams.
Hydrological Processes,
Journal Year:
2024,
Volume and Issue:
38(6)
Published: June 1, 2024
Abstract
Understanding
controls
on
solute
export
to
streams
is
challenging
because
heterogeneous
catchments
can
respond
uniquely
drivers
of
environmental
change.
To
understand
general
patterns,
we
used
a
large‐scale
inductive
approach
evaluate
concentration–discharge
(C–Q)
metrics
across
spanning
broad
range
catchment
attributes
and
hydroclimatic
drivers.
We
leveraged
paired
C–Q
data
for
11
solutes
from
CAMELS‐Chem,
database
built
upon
an
existing
dataset
relatively
undisturbed
the
contiguous
USA.
Because
relationships
with
Q
thresholds
reflect
shift
in
dynamics
are
poorly
characterized
diverse
catchments,
analysed
using
Bayesian
segmented
regression
quantify
relationship.
Threshold
responses
were
rare,
representing
only
12%
relationships,
56%
which
occurred
predominantly
sourced
bedrock.
Further,
dominated
by
one
or
two
patterns
that
reflected
vertical
solute–source
distributions.
Specifically,
bedrock
had
diluting
43%–70%
soils
more
enrichment
35%–51%
catchments.
also
linked
patterns.
The
generally
weak
despite
diversity
attribute
types
considered.
However,
central
USA
typically
drove
most
divergent
behaviour
solutes.
illustrate
how
our
generated
new
hypotheses
be
tested
at
discrete,
representative
deductive
approaches
better
processes
underlying
Finally,
given
these
long‐term
minimally
disturbed
findings
as
benchmarks
change