Quantifying the changes in solute transport caused by human influence on river connectivity in inland river basins
Wenhao Zhang,
No information about this author
Guofeng Zhu,
No information about this author
Ling Zhao
No information about this author
et al.
CATENA,
Journal Year:
2024,
Volume and Issue:
246, P. 108360 - 108360
Published: Sept. 9, 2024
Language: Английский
Investigating the structure of a multiple karst aquifer system and its hydrological process response using high-resolution multi-tracer data
Journal of Hydrology,
Journal Year:
2025,
Volume and Issue:
unknown, P. 133152 - 133152
Published: March 1, 2025
Language: Английский
Ecological regulation of chemical weathering recorded in rivers
Earth and Planetary Science Letters,
Journal Year:
2024,
Volume and Issue:
641, P. 118800 - 118800
Published: June 4, 2024
We
provide
a
new
generalized
framework
accounting
for
the
effects
of
water
and
nutrient
uptake
by
roots
in
weathering
zone
on
broad
patterns
solute
concentration
-
discharge
relationships
rivers.
As
plants
withdraw
from
subsurface,
they
decrease
area-normalized
fluid
drainage
rate.
This
results
flux
to
springs
streams
which
is
function
use
plants,
leading
ecosystem
regulation
characteristic
timescales
chemical
reactions
flow
Our
predictive
quantifies
pore
river
chemistry
generated
water-rock
interactions,
regulated
vegetation
rates.
To
this
we
add
capacity
enrich,
passively
admit,
or
discriminate
against
given
dissolved
based
ecophysiological
needs,
thus
further
modifying
local
species
solution
across
profile.
not
lost
atmosphere
same
manner
as
removed
subsurface
via
evapotranspiration.
Rather,
these
extracted
become
incorporated
into
topsoil
litter
may
be
partially
fully
resolubilized,
creating
an
upper
boundary
condition
depends
recycling
characteristics
ecosystem.
These
processes
are
united
through
advection-reaction
equation
allows
regulate
stream
relationships.
show
that
ecosystems
capable
both
accelerating
impeding
reaction
rates
profile,
ultimately
thermodynamic
ecological
controls
baseflow
rock-derived
solutes
Language: Английский
Experimental constraints on barium isotope fractionation during adsorption–desorption reactions: Implications for weathering and erosion tracer applications
Geochimica et Cosmochimica Acta,
Journal Year:
2024,
Volume and Issue:
384, P. 194 - 212
Published: Aug. 30, 2024
Constraining
the
processes
that
fractionate
barium
isotopes
is
essential
for
utilising
isotope
ratios
as
environmental
tracers.
Barium
concentration
measurements
from
soils,
rivers,
and
estuaries
demonstrate
adsorption–desorption
reactions
significantly
influence
distribution
of
fluid-mobile
at
Earth's
surface,
potentially
driving
isotopic
fractionation.
To
quantify
direction
magnitude
fractionation
resulting
these
reactions,
a
riverine
an
estuarine
series
batch
experiments
were
conducted
using
environmentally
important
adsorbent
minerals
surface
waters.
Himalayan
river
sediment
water
samples
used
to
validate
experimental
results.
Adsorption–desorption
found
be
rapid,
relative
average
transit
time
in
catchments,
largely
reversible.
The
experiment
consistent
with
field
(preferential
adsorption
lighter
isotopes).
reaction
rate,
reversibility,
depend
primarily
on
mineral.
Experiments
performed
iron
oxyhydroxides
(goethite
ferrihydrite)
resulted
greater
degree
compared
clay
(kaolinite
montmorillonite).
Estuarine
experiments,
designed
simulate
passage
through
salinity
gradient,
demonstrated
high
77%
94%
adsorbed
desorbed
upon
addition
seawater
freshwater–equilibrated
minerals.
results
suggest
measured
marine
paleo–archives
(e.g.,
corals)
will
reflect
both
dissolved
freshwater
inputs
ocean.
combined
findings
this
study
indicate
chemical
behaviour
differs
more
conventional
group
1
2
metal
systems
due
significant
proportion
released
bedrock
dissolution
partitioning
mineral
surfaces,
rapid
rates
between
phases,
reversibility.
Consequently,
are
likely
provide
unique
insights
into
complex
array
terrestrial
weathering
erosion
sustain
life
Earth.
Language: Английский
Technical Note on high-frequency, multi-elemental stream water monitoring: experiences, feedbacks, and suggestions from seven years of running three French field laboratories (Riverlabs)
Nicolai Brekenfeld,
No information about this author
Solenn Cotel,
No information about this author
Mikaël Faucheux
No information about this author
et al.
Published: April 3, 2024
Abstract.
High-frequency
and
multi-elemental
stream
water
monitoring
are
acknowledged
as
necessary
to
address
data
limitation
in
the
fields
of
catchment
sciences
freshwater
biogeochemistry.
In
recent
years,
development
bank
analyzers
on-site
field
laboratories
measure
various
solutes
and/or
isotopes
at
sub-hourly
measurement
intervals
is
progress
an
increasing
number
sites.
This
trend
should
likely
persist
future.
Here,
we
share
our
experiences
running
three
French
(called
Riverlabs)
over
seven
years.
technical
note
gives
overview
organizational
points
that
identify
critical
order
provide
guidelines
for
successful
implementation
future
projects
such
equipment.
We
therefore
main
stages
deployment
this
tool
field,
difficulties
encountered
procedures
used
eliminate
their
causes.
Some
aspects
discussed
here
relate
1)
Supply
laboratory:
basic
functioning
pumping,
filtration
analytical
systems,
2)
Data
quality
control
assurance
via
maintenance
services
operations,
3)
harmonization
coordination
laboratory
components,
4)
Team
structure,
skills
organization.
Our
two
conclusions
a
successful,
long-term
these
types
are,
first,
necessity
adapt
several
central
components
local
conditions
(climate,
section,
topography,
turbidity,
power)
and,
second,
need
diverse
in-depth
within
engineering
team.
believe
sharing
experiences,
combined
with
providing
some
practical
suggestions
might
be
useful
colleagues,
who
starting
deploy
or
similar
laboratories.
These
considerations
will
save
time,
improve
performance
ensure
continuous
monitoring.
Language: Английский
Reply on RC2
Ophelie Fovet
No information about this author
Published: June 25, 2024
High-frequency
and
multi-elemental
stream
water
monitoring
are
acknowledged
as
necessary
to
address
data
limitation
in
the
fields
of
catchment
sciences
freshwater
biogeochemistry.
In
recent
years,
development
bank
analyzers
on-site
field
laboratories
measure
various
solutes
and/or
isotopes
at
sub-hourly
measurement
intervals
is
progress
an
increasing
number
sites.
This
trend
should
likely
persist
future.
Here,
we
share
our
experiences
running
three
French
(called
Riverlabs)
over
seven
years.
technical
note
gives
overview
organizational
points
that
identify
critical
order
provide
guidelines
for
successful
implementation
future
projects
such
equipment.
We
therefore
main
stages
deployment
this
tool
field,
difficulties
encountered
procedures
used
eliminate
their
causes.
Some
aspects
discussed
here
relate
1)
Supply
laboratory:
basic
functioning
pumping,
filtration
analytical
systems,
2)
Data
quality
control
assurance
via
maintenance
services
operations,
3)
harmonization
coordination
laboratory
components,
4)
Team
structure,
skills
organization.
Our
two
conclusions
a
successful,
long-term
these
types
are,
first,
necessity
adapt
several
central
components
local
conditions
(climate,
section,
topography,
turbidity,
power)
and,
second,
need
diverse
in-depth
within
engineering
team.
believe
sharing
experiences,
combined
with
providing
some
practical
suggestions
might
be
useful
colleagues,
who
starting
deploy
or
similar
laboratories.
These
considerations
will
save
time,
improve
performance
ensure
continuous
monitoring.
Language: Английский
Stable silicon isotope fractionation reflects the routing of water through a mesoscale hillslope
Andrew Guertin,
No information about this author
Charlie Cunningham,
No information about this author
Julien Bouchez
No information about this author
et al.
Earth and Planetary Science Letters,
Journal Year:
2024,
Volume and Issue:
648, P. 119098 - 119098
Published: Nov. 5, 2024
Language: Английский
Comment on egusphere-2024-902
Jennifer Druhan
No information about this author
Published: May 1, 2024
High-frequency
and
multi-elemental
stream
water
monitoring
are
acknowledged
as
necessary
to
address
data
limitation
in
the
fields
of
catchment
sciences
freshwater
biogeochemistry.
In
recent
years,
development
bank
analyzers
on-site
field
laboratories
measure
various
solutes
and/or
isotopes
at
sub-hourly
measurement
intervals
is
progress
an
increasing
number
sites.
This
trend
should
likely
persist
future.
Here,
we
share
our
experiences
running
three
French
(called
Riverlabs)
over
seven
years.
technical
note
gives
overview
organizational
points
that
identify
critical
order
provide
guidelines
for
successful
implementation
future
projects
such
equipment.
We
therefore
main
stages
deployment
this
tool
field,
difficulties
encountered
procedures
used
eliminate
their
causes.
Some
aspects
discussed
here
relate
1)
Supply
laboratory:
basic
functioning
pumping,
filtration
analytical
systems,
2)
Data
quality
control
assurance
via
maintenance
services
operations,
3)
harmonization
coordination
laboratory
components,
4)
Team
structure,
skills
organization.
Our
two
conclusions
a
successful,
long-term
these
types
are,
first,
necessity
adapt
several
central
components
local
conditions
(climate,
section,
topography,
turbidity,
power)
and,
second,
need
diverse
in-depth
within
engineering
team.
believe
sharing
experiences,
combined
with
providing
some
practical
suggestions
might
be
useful
colleagues,
who
starting
deploy
or
similar
laboratories.
These
considerations
will
save
time,
improve
performance
ensure
continuous
monitoring.
Language: Английский