Abstract.
The
demanding
precision
of
triple
oxygen
isotope
(Δ17O)
analyses
in
water
has
restricted
their
measurement
to
dual-inlet
mass
spectrometry
until
the
recent
development
commercially
available
infrared
laser
analyzers.
Laser-based
measurements
ratios
are
now
increasingly
performed
by
laboratories
seeking
better
constrain
source
and
history
meteoric
waters.
However,
practice,
these
subject
large
analytical
errors
that
remain
poorly
documented
scientific
literature
instrument
manufacturers,
which
can
effectively
restrict
confident
application
Δ17O
settings
where
variations
relatively
class="inline-formula">∼
25–60
per
meg).
We
present
our
operating
method
a
Picarro
L2140-i
cavity
ring-down
spectrometer
(CRDS)
during
analysis
low-latitude
rainwater
confidently
resolving
daily
(differences
10–20
meg)
was
desired.
Our
approach
optimized
over
3
years
uses
combination
published
best
practices
plus
additional
steps
combat
spectral
contamination
trace
amounts
dissolved
organics,
which,
for
class="inline-formula">Δ17O,
emerges
as
much
more
substantial
problem
than
previously
documented,
even
pure
rainwater.
resolve
extreme
sensitivity
organics
through
removal
via
Picarro's
micro-combustion
module,
whose
performance
is
evaluated
each
sequence
using
alcohol-spiked
standards.
While
correction
sample-to-sample
memory
instrumental
drift
significantly
improves
traditional
metrics,
corrections
have
only
marginal
impact
(0–1
meg
error
reduction)
on
class="inline-formula">Δ17O.
post-processing
scheme
analyzer's
high-resolution
data,
class="inline-formula">δ2H
(0.25
‰
allows
rich
troubleshooting
data
processing
compared
default
user-facing
output.
In
addition
competitive
we
report
long-term,
control
standard
root
mean
square
12
meg.
Overall
6
meg,
calculated
averaging
three
replicates
spread
across
distinct,
independently
calibrated
sequences)
comparable
requires
6.3
h
sample.
demonstrate
rainfall
dataset
from
Uganda
offer
recommendations
other
efforts
aim
measure
CRDS.
Atmospheric measurement techniques,
Journal Year:
2023,
Volume and Issue:
16(6), P. 1663 - 1682
Published: March 29, 2023
Abstract.
The
demanding
precision
of
triple
oxygen
isotope
(Δ17O)
analyses
in
water
has
restricted
their
measurement
to
dual-inlet
mass
spectrometry
until
the
recent
development
commercially
available
infrared
laser
analyzers.
Laser-based
measurements
ratios
are
now
increasingly
performed
by
laboratories
seeking
better
constrain
source
and
history
meteoric
waters.
However,
practice,
these
subject
large
analytical
errors
that
remain
poorly
documented
scientific
literature
instrument
manufacturers,
which
can
effectively
restrict
confident
application
Δ17O
settings
where
variations
relatively
(∼
25–60
per
meg).
We
present
our
operating
method
a
Picarro
L2140-i
cavity
ring-down
spectrometer
(CRDS)
during
analysis
low-latitude
rainwater
confidently
resolving
daily
(differences
∼
10–20
meg)
was
desired.
Our
approach
optimized
over
3
years
uses
combination
published
best
practices
plus
additional
steps
combat
spectral
contamination
trace
amounts
dissolved
organics,
which,
for
Δ17O,
emerges
as
much
more
substantial
problem
than
previously
documented,
even
pure
rainwater.
resolve
extreme
sensitivity
organics
through
removal
via
Picarro's
micro-combustion
module,
whose
performance
is
evaluated
each
sequence
using
alcohol-spiked
standards.
While
correction
sample-to-sample
memory
instrumental
drift
significantly
improves
traditional
metrics,
corrections
have
only
marginal
impact
(0–1
meg
error
reduction)
on
Δ17O.
post-processing
scheme
analyzer's
high-resolution
data,
δ2H
(0.25
‰
allows
rich
troubleshooting
data
processing
compared
default
user-facing
output.
In
addition
competitive
we
report
long-term,
control
standard
root
mean
square
12
meg.
Overall
(Δ17O
6
meg,
calculated
averaging
three
replicates
spread
across
distinct,
independently
calibrated
sequences)
comparable
requires
6.3
h
sample.
demonstrate
rainfall
dataset
from
Uganda
offer
recommendations
other
efforts
aim
measure
CRDS.
Abstract
The
analysis
of
the
stable
isotopic
composition
hydrogen
and
oxygen
in
water
samples
from
soils
plants
can
help
to
identify
sources
vegetation
uptake.
This
approach
requires
that
heterogeneous
nature
plant
soil
matrices
is
carefully
accounted
for
during
experimental
design,
sample
collection,
extraction
analyses.
comparability
shortcomings
different
methods
extracting
analyzing
have
been
discussed
specialized
literature.
Yet,
despite
insightful
comparisons
benchmarking
methodologies
laboratories
worldwide,
community
still
lacks
a
roadmap
guide
extraction,
analyses,
many
practical
issues
potential
users
remain
unresolved:
example,
which
(soil
or
plant)
pool(s)
does
extracted
represent?
These
constitute
hurdle
implementation
by
newcomers.
Here,
we
summarize
discussions
led
framework
COST
Action
WATSON
(“WATer
isotopeS
critical
zONe:
groundwater
recharge
transpiration”—CA19120).
We
provide
guidelines
(1)
sampling
material
analysis,
(2)
laboratory
situ
(3)
measurements
composition.
highlight
importance
considering
process
chain
as
whole,
design
minimize
biased
estimates
relative
contribution
conclude
acknowledging
some
limitations
this
methodology
advice
on
collection
key
environmental
parameters
prior
article
categorized
under:
Science
Water
>
Hydrological
Processes
Environmental
Change
Extremes
Hydrological Processes,
Journal Year:
2022,
Volume and Issue:
36(10)
Published: Sept. 12, 2022
Abstract
Ecohydrological
investigations
commonly
use
the
stable
isotopes
of
water
(hydrogen
and
oxygen)
as
conservative
ecosystem
tracers.
This
approach
requires
accessing
analysing
from
plant
soil
matrices.
Generally,
there
are
six
steps
involved
to
retrieve
hydrogen
oxygen
isotope
values
these
matrices:
(1)
sampling,
(2)
sample
storage
transport,
(3)
extraction,
(4)
pre‐analysis
processing,
(5)
isotopic
analysis,
(6)
post‐processing
correction.
At
each
step,
cumulative
errors
can
be
introduced
which
sum
non‐trivial
magnitudes.
These
impact
subsequent
interpretations
about
cycling
partitioning
through
soil–plant‐atmosphere
continuum.
steps,
multiple
possible
options
select
resulting
in
tens
thousands
combinations
used
by
researchers
go
samples
data.
In
a
newly
emerging
field,
so
many
create
interpretive
confusion
major
issues
with
data
comparability.
points
need
for
development
shared
standardized
approaches.
Here
we
critically
examine
state
process
chain,
reflecting
on
associated
provide
suggestions
move
our
community
towards
standardization.
Assessing
this
‘process
chain’
will
help
us
see
problem
its
entirety
facilitate
action
agreed
upon
Isotopes in Environmental and Health Studies,
Journal Year:
2022,
Volume and Issue:
58(4-6), P. 363 - 379
Published: Oct. 11, 2022
In
Germany,
river
monitoring
for
tritium
started
in
the
early
1970s.
Today
this
network
consists
of
50
stations
and
includes
stable
isotopes.
The
isotope
time
series
to
end
2021
are
at
least
four
years
some
up
30
long.
Daily
water
samples
were
collected
during
an
extraordinary
dry
season
from
October
2018
until
January
2019
six
selected
Rhine
five
Elbe
basin.
most
dominating
effects
seasonal
altitude
effects,
but
also
a
continental
effect
is
visible.
isotopes
indicate
snow
ice
melt
contributions
Danube
summer
months
consecutive
dilution
these
signals
by
mixing
with
tributary
rivers.
Close
coasts
northern
patterns
reflect
influence
seawater
tides.
2018/2019
surprisingly
do
not
exhibit
extreme
changes
rather
trends
enhanced
groundwater
contribution.
Long-term
continual
data
across
scales
important
comparing
identifying
hydrological
processes
German
basins
different
size
mean
catchment
altitudes,
highlight
benefits
co-organized
national
network.
GEM - International Journal on Geomathematics,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: June 12, 2023
Abstract
Stable
isotopes
of
hydrogen
and
oxygen
are
important
natural
tracers
with
a
wide
variety
environmental
applications
(e.g.,
the
exploration
water
cycle,
ecology
food
authenticity).
The
spatially
explicit
predictions
their
variations
obtained
through
various
interpolation
techniques.
In
present
work,
classical
random
forest
(RF)
two
its
variants
were
applied.
RF
version
employing
buffer
distance
(RF
sp
)
applied
to
each
month
separately,
while
model
was
trained
using
all
data
year
as
categorical
variables
tg
).
Their
performance
in
predicting
spatial
variability
precipitation
stable
isotope
values
for
2008–2017
across
Europe
compared.
addition,
comparison
made
publicly
available
alternative
machine
learning
which
employs
extreme
gradient
boosting.
Input
retrieved
from
Global
Network
Isotopes
Precipitation
(GNIP;
no.
stations:
144)
other
national
datasets
(no.
127).
Comparisons
on
basis
absolute
differences,
median,
mean
error
Lin’s
concordance
correlation
coefficient.
All
capable
reproducing
overall
trends
seasonal
patterns
over
time
measured
at
chosen
validation
site
Europe.
most
predictors
latitude
case
RF,
meteorological
(vapor
pressure,
saturation
vapor
temperature)
models.
Diurnal
temperature
range
had
weakest
predictive
power
every
case.
conclusion,
it
may
be
stated
that
merged
dataset,
combining
GNIP
datasets,
yielded
smallest
1.345‰)
highest
coefficient
(0.987),
boosting
(based
only
data)
1.354‰,
0.984,
although
produced
lowers
median
value
(1.113‰),
1.124‰.
striking
systematic
bias
observed
summer
season
northern
stations;
this,
however,
diminished
2014
onward,
point
after
stations
beyond
55°
N
training
set.
Earth system science data,
Journal Year:
2022,
Volume and Issue:
14(6), P. 2721 - 2735
Published: June 10, 2022
Abstract.
The
characteristics
of
the
CISE-LOCEAN
seawater
isotope
dataset
(δ18O,
δ2H,
referred
to
as
δD)
are
presented
(https://doi.org/10.17882/71186;
Waterisotopes-CISE-LOCEAN,
2021).
This
covers
time
period
from
1998
2021
and
currently
includes
close
8000
data
entries,
all
with
δ18O,
three-quarters
them
also
δD,
associated
a
date
stamp,
space
usually
salinity
measurement.
Until
2010,
samples
were
analyzed
by
isotopic
ratio
mass
spectrometry
since
then
mostly
cavity
ring-down
spectroscopy
(CRDS).
Instrumental
uncertainty
in
this
is
low
0.03
‰
for
δ18O
0.15
δD.
An
additional
related
composition
in-house
standards
that
used
convert
Vienna
Standard
Mean
Ocean
Water
(VSMOW)
scale.
Different
comparisons
suggest
2010
latter
have
remained
within
at
most
0.20
Therefore,
combining
two
uncertainties
suggests
standard
deviation
0.05
0.25
For
some
samples,
we
find
there
has
been
evaporation
during
collection
storage,
requiring
adjustment
produced
CRDS,
based
on
d-excess
(δD
−
8×δ18O).
adds
an
respective
roughly
0.10
issue
conservation
certainly
strong
source
quality
loss
parts
database,
“small”
effects
may
undetected.
internal
consistency
database
can
be
tested
subsets
when
series
obtained
(such
southern
Indian
or
North
Atlantic
subpolar
gyre).
These
overall
spatially
(for
cruise)
temporally
(over
year)
averaged
less
than
However,
18
duplicate
other
laboratories
datasets
intermediate
deep
ocean
larger
scatter.
When
averaging
done
difference
0.082
error
0.016
‰.
Such
average
expected
due
adjustments
applied
LOCEAN
saline
water
either
CRDS
(IRMS),
but
scatter
found
care
needed
merging
different
laboratories.
Examples
surface
gyre
illustrate
temporal
changes
detected
carefully
validated
dataset.
MethodsX,
Journal Year:
2023,
Volume and Issue:
10, P. 102150 - 102150
Published: Jan. 1, 2023
δ17O
and
Δ'17O
are
emerging
tracers
increasingly
used
in
isotope
hydrology,
climatology,
biochemistry.
Differentiating
small
relative
abundance
changes
the
rare
17O
from
strong
covariance
with
18O
imposes
ultra-high
precision
requirements
for
this
analysis.
Measurements
of
by
Cavity
Ringdown
Spectroscopy
(CRDS)
attractive
due
to
ease
sample
preparation,
automated
throughput,
avoidance
chemical
conversions
needed
isotope-ratio
mass
spectrometry.
However,
CRDS
approach
requires
trade-offs
measurement
uncertainty.
In
protocol
document,
we
present
following:•New
analytical
procedures
a
software
tool
conducting
measurements
CRDS.•Outline
robust
uncertainty
framework
determinations.•Description
performance
optimizing
instrumental
stability,
accuracy.