Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(11)
Published: Oct. 29, 2021
Abstract
Oxidative
weathering
of
sedimentary
rocks
plays
an
important
role
in
the
global
carbon
cycle.
Rhenium
(Re)
has
been
proposed
as
a
tracer
rock
organic
(OC
petro
)
oxidation.
However,
sources
Re
and
its
mobilization
by
hydrological
processes
remain
poorly
constrained.
Here,
we
examine
dissolved
function
water
discharge,
using
samples
collected
from
three
alpine
catchments
that
drain
Switzerland
(Erlenbach
Vogelbach)
Colorado,
USA
(East
River).
The
Swiss
reveal
higher
flux
catchment
with
erosion
rates,
but
have
similar
[Re]/[Na
+
]
[Re]/[SO
4
2−
ratios,
which
indicate
dominance
OC
.
Despite
differences
type
hydro‐climatic
setting,
positive
correlation
between
river
discharge.
We
propose
this
reflects
preferential
routing
near‐surface,
oxidative
zone.
observations
support
use
proxy
to
trace
rock‐organic
oxidation,
suggest
it
may
be
vadose
zone
processes.
apply
estimate
CO
2
release
oxidation
5.7
+6.6
/
−2.0
tC
km
−2
yr
−1
for
Erlenbach.
overall
intensity
was
∼40%,
meaning
corresponding
export
unweathered
sediments
is
large,
findings
call
more
measurements
mountains
rivers
they
cross
floodplains.
Vadose Zone Journal,
Journal Year:
2018,
Volume and Issue:
17(1), P. 1 - 25
Published: Jan. 1, 2018
Core
Ideas
Development
of
a
300‐km
2
mountainous
headwater
testbed
began
in
2016
the
East
River.
The
can
be
used
to
explore
how
watershed
changes
impact
downgradient
water
availability
and
quality.
System‐of‐system,
scale‐adaptive
approaches
potentially
improve
dynamics
simulation.
We
have
new
monitor
simulate
partitioning
system
responses.
River
has
been
developed
as
“community”
testbed.
Extreme
weather,
fires,
land
use
climate
change
are
significantly
reshaping
interactions
within
watersheds
throughout
world.
Although
hydrological–biogeochemical
many
services
valued
by
society,
uncertainty
associated
with
predicting
hydrology‐driven
biogeochemical
remains
high.
With
an
aim
reduce
this
uncertainty,
approximately
observatory
at
River,
CO,
Upper
Colorado
Basin.
site
is
being
for
Department
Energy
supported
Watershed
Function
Project
collaborative
efforts.
Building
on
insights
gained
from
research
“sister”
Rifle,
site,
coordinated
studies
underway
gain
predictive
understanding
retains
releases
water,
nutrients,
carbon,
metals.
In
particular,
project
exploring
early
snowmelt,
drought,
other
disturbances
influence
seasonal
decadal
timescales.
A
system‐of‐systems
perspective
simulation
approach,
involving
combined
archetypal
subsystem
“intensive
sites”
tested
inform
aggregated
predictions
exports.
Complementing
intensive
hydrological,
geochemical,
geophysical,
microbiological,
geological,
vegetation
datasets
long‐term,
distributed
measurement
stations
specialized
experimental
observational
campaigns.
Several
recent
advances
provide
about
sites
well
behavior.
“community
testbed”
currently
hosting
scientists
more
than
30
institutions
advance
methods
understanding.
Water Resources Research,
Journal Year:
2019,
Volume and Issue:
55(5), P. 4233 - 4251
Published: April 15, 2019
Abstract
Understanding
concentration‐discharge
(C‐Q)
relationships
are
essential
for
predicting
chemical
weathering
and
biogeochemical
cycling
under
changing
climate
anthropogenic
conditions.
Contrasting
C‐Q
have
been
observed
widely,
yet
a
mechanistic
framework
that
can
interpret
diverse
patterns
remains
elusive.
This
work
hypothesizes
seemingly
disparate
driven
by
switching
dominance
of
end‐member
source
waters
their
contrasts
arising
from
subsurface
heterogeneity.
We
use
data
Coal
Creek,
high‐elevation
mountainous
catchment
in
Colorado,
recently
developed
watershed
reactive
transport
model
(BioRT‐Flux‐PIHM).
Sensitivity
analysis
Monte‐Carlo
simulations
(500
cases)
show
reaction
kinetics
thermodynamics
distribution
materials
across
depths
govern
the
chemistry
gradients
shallow
soil
water
deeper
groundwater
entering
stream.
The
alternating
organic‐poor
geo‐solute‐rich
dry
conditions
organic‐rich
geo‐solute‐poor
during
spring
melt
leads
to
flushing
pattern
dissolved
organic
carbon
dilution
geogenic
solutes
(e.g.,
Na,
Ca,
Mg).
In
addition,
extent
concentration
regulates
power
law
slopes
(
b
)
via
general
equation
.
At
low
ratios
versus
concentrations
(C
ratio
=
C
sw
/C
gw
<
0.6),
occurs;
at
high
>
1.8),
arises;
chemostasis
occurs
between.
quantitatively
interprets
values
11
(dissolved
carbon,
P,
NO
3
−
,
K,
Si,
Mg,
Al,
Mn,
Fe)
three
catchments
(Coal
Shale
Hills,
Plynlimon)
differing
climate,
geologic,
land
cover
indicates
potentially
broad
regulation
heterogeneity
determining
wide
applications
this
quantifying
values,
which
implications
transformation
scale.
Hydrological Processes,
Journal Year:
2018,
Volume and Issue:
32(14), P. 2187 - 2202
Published: May 15, 2018
Abstract
Critical
zone
influences
on
hydrologic
partitioning,
subsurface
flow
paths
and
reactions
along
these
dictate
the
timing
magnitude
of
groundwater
solute
flux
to
streams.
To
isolate
first‐order
controls
seasonal
streamflow
generation
within
highly
heterogeneous,
snow‐dominated
basins
Colorado
River,
we
employ
a
multivariate
statistical
approach
end‐member
mixing
analysis
using
suite
daily
chemical
isotopic
observations.
Mixing
models
are
developed
across
11
nested
(0.4
85
km
2
)
spanning
gradient
climatological,
physical,
geological
characteristics.
Hydrograph
separation
rain,
snow,
as
end‐members
indicates
that
contributions
streams
is
significant.
Mean
annual
ranges
from
12%
33%
whereas
maximum
17%
50%
occur
during
baseflow.
The
direct
relationship
between
snow
water
equivalent
scale
dependent
with
trend
toward
self‐similarity
when
exceed
5.5
.
We
find
recharge
increases
in
high
relief
upper
subalpine
where
accumulation
coincident
reduced
conifer
cover
lower
canopy
densities.
model
for
furthest
downstream
site
did
not
transfer
upstream
basins.
resulting
error
predicted
stream
concentrations
points
weathering
function
source
rock
shifts
path.
Additionally,
potential
microbial
sulfate
reduction
floodplain
sediments
low‐gradient,
meandering
portion
river
sufficient
modify
hillslope
alter
ratios
analysis.
Soil
flushing
response
snowmelt
included
an
but
identified
important
mechanism
release
solutes
mountainous
watersheds.
End‐member
used
combination
high‐frequency
observations
reveals
aspects
catchment
hydrodynamics
scale.
Hydrology and earth system sciences,
Journal Year:
2022,
Volume and Issue:
26(19), P. 5163 - 5184
Published: Oct. 14, 2022
Abstract.
Rivers
and
river
habitats
around
the
world
are
under
sustained
pressure
from
human
activities
changing
global
environment.
Our
ability
to
quantify
manage
states
in
a
timely
manner
is
critical
for
protecting
public
safety
natural
resources.
In
recent
years,
vector-based
network
models
have
enabled
modeling
of
large
basins
at
increasingly
fine
resolutions,
but
computationally
demanding.
This
work
presents
multistage,
physics-guided,
graph
neural
(GNN)
approach
basin-scale
learning
streamflow
forecasting.
During
training,
we
train
GNN
model
approximate
outputs
high-resolution
model;
then
fine-tune
pretrained
with
observations.
We
further
apply
graph-based,
data-fusion
step
correct
prediction
biases.
The
GNN-based
framework
first
demonstrated
over
snow-dominated
watershed
western
United
States.
A
series
experiments
performed
test
different
training
imputation
strategies.
Results
show
that
trained
can
effectively
serve
as
surrogate
process-based
high
accuracy,
median
Kling–Gupta
efficiency
(KGE)
greater
than
0.97.
Application
graph-based
data
fusion
reduces
mismatch
between
observations,
much
50
%
KGE
improvement
some
cross-validation
gages.
To
improve
scalability,
graph-coarsening
procedure
introduced
larger
basin.
coarsening
achieves
comparable
skills
only
fraction
cost,
thus
providing
important
insights
into
degree
physical
realism
needed
developing
large-scale
models.
Global Biogeochemical Cycles,
Journal Year:
2024,
Volume and Issue:
38(2)
Published: Feb. 1, 2024
Abstract
Rivers
and
streams
play
an
important
role
within
the
global
carbon
cycle,
in
part
through
emissions
of
dioxide
(CO
2
)
to
atmosphere.
However,
sources
this
CO
their
spatiotemporal
variability
are
difficult
constrain.
Recent
work
has
highlighted
carbonate
buffering
reactions
that
may
serve
as
a
source
high
alkalinity
systems.
In
study,
we
seek
develop
quantitative
framework
for
fluxes
patterns
stable
radio‐
isotope
composition
dissolved
inorganic
(DIC).
We
incorporate
DIC
speciation
calculations
isotopologues
into
stream
network
model
perform
series
simulations,
ranging
from
degassing
groundwater
seep
hydrologically‐coupled
5th‐order
network.
find
contribute
>60%
high‐alkalinity,
moderate
groundwater‐CO
environments.
atmosphere
equilibration
timescales
minimally
affected,
which
contradicts
hypotheses
maintains
across
Strahler
orders
contrast,
dramatically
increases
timescales,
acts
decouple
variations
isotopic
even
under
low
alkalinity.
This
significantly
complicates
common
method
identification.
Based
on
similar
impacts
atmospheric
isotopologues,
partitioning
corridor
carbonate‐dominated
watersheds.
Together,
these
results
provide
guide
fieldwork
interpretations
variable
alkalinities.