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[v1]Spatial
Variations
in
Tap
Water
Isotopes
Across
Canada:
Tracing
from
Precipitation
Distribution
Assess
Regional
ResourcesAuthorsShelinaBhuiyanSee
all
authors
Shelina
BhuiyanCorresponding
Author•
Submitting
AuthorUniversity
of
Ottawaview
email
addressThe
was
not
providedcopy
address
Journal of Hydrology,
Journal Year:
2023,
Volume and Issue:
617, P. 129129 - 129129
Published: Jan. 16, 2023
Stable
isotopes
of
precipitation
are
important
natural
tracers
in
hydrology,
ecology,
and
forensics.
The
spatially
explicit
predictions
oxygen
hydrogen
obtained
through
different
interpolation
techniques.
In
the
present
study
we
aim
to
examine
performance
various
techniques
when
predicting
spatial
distribution
stable
isotopes.
efficiency
combined
geostatistical
tools
(i.e.
regression
kriging;
RK)
machine
learning
methods
(including
enhanced
random
forest
methods:
MRRF,
RERF)
compared
interpolating
variability
isotope
values
from
two
sampling
networks
Europe.
To
assess
models,
mean
squared
error
(MSE),
nonparametric
Kling
Gupta
(KGE),
absolute
differences
relative
metrics
were
employed.
It
was
found
that
combination
with
Random
Forest
can
produce
estimations
comparable
accuracy
terms
descending
order
overall
average
MSE,
MRRF:
2.61,
RK:
2.77,
RERF:
2.99,
RF:
3.08.
best
performing
model
variant
(MRRF)
outperformed
kriging
a
hybrid
metric
(KGE)
by
7.5%.
Sequential
rarefying
station
showed
machine-learning
more
capable
maintaining
high
prediction
even
fewer
input
data.
This
be
great
advantage
suitable
method
is
needed
predict
composition
for
large
domains
where
density
data
stations
shows
differences.
PLoS ONE,
Journal Year:
2022,
Volume and Issue:
17(1), P. e0261651 - e0261651
Published: Jan. 7, 2022
A
wide
range
of
hydrological,
ecological,
environmental,
and
forensic
science
applications
rely
on
predictive
“isoscape”
maps
to
provide
estimates
the
hydrogen
or
oxygen
isotopic
compositions
environmental
water
sources.
Many
isoscapes
have
been
developed,
but
few
studies
produced
specifically
representing
groundwaters.
None
these
represented
distinct
subsurface
layers
variations
across
them.
Here
we
compiled
>6
million
well
completion
records
>27,000
groundwater
isotope
datapoints
develop
a
space-
depth-explicit
isoscape
for
contiguous
United
States.
This
3-dimensional
model
shows
that
vertical
heterogeneity
in
is
substantial
some
parts
country
delta
values
often
differ
from
those
coincident
precipitation
surface
resources;
many
patterns
can
be
explained
by
established
hydrological
hydrogeological
mechanisms.
We
validate
against
an
independent
data
set
tap
show
accurately
predicts
communities
known
use
resources.
new
approach
represents
foundation
further
developments
resulting
should
improved
predictions
systems
where
potential
source.
Abstract
Groundwater
supports
agriculture
and
provides
domestic
water
for
over
250
million
people
in
the
Bengal
Basin.
Here
we
investigate
source
of
groundwater
recharge
using
2500
stable
isotope
measurements
from
region.
We
employ
a
Monte
Carlo
statistical
analysis
to
find
distributions
possible
components
by
accounting
variability
ratios
each
sources.
that
sources
have
shifted
last
decades
with
~50%
increase
stagnant
surface
bodies
(mostly
during
latter
part
dry
season)
relative
decrease
contribution
direct
infiltration
precipitation
(which
occurs
mostly
early
monsoon).
attribute
this
shift
an
standing
irrigated
rice
fields
ponds,
downward
hydraulic
gradient
season
driven
pumping.
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.
Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(7)
Published: June 21, 2021
Rising
global
temperatures
are
expected
to
decrease
the
precipitation
amount
that
falls
as
snow,
causing
greater
risk
of
water
scarcity,
groundwater
overdraft,
and
fire
in
areas
rely
on
mountain
snowpack
for
their
supply.
Streamflow
large
river
basins
varies
with
amount,
timing,
type
precipitation,
evapotranspiration,
drainage
properties
watersheds;
however,
these
controls
vary
time
space
making
it
difficult
identify
contributing
most
flow
when.
In
this
study,
we
separate
evaporative
influences
from
source
values
isotopes
Snake
River
Basin
western
United
States
(US)
relate
area
dynamics.
We
developed
isoscapes
(δ2H
δ18O)
basin
found
isotopic
composition
surface
small
watersheds
is
primarily
controlled
by
longitude,
latitude,
elevation.
To
examine
temporal
variability
contributions
flow,
present
a
six-year
record
King
Hill,
Idaho
after
removing
influences.
During
periods
low
were
isotopically
lighter
indicating
larger
contribution
waters
highest
elevation,
eastern
portion
basin.
evaporation
increases
evident
during
summer
likely
reflecting
climate,
changing
availability,
management
strategies
within
Our
findings
potential
tool
identifying
critical
portions
climate
fluctuations
alter
This
can
be
applied
other
continental-interior
where
may
obscure
signatures.
Hydrology,
Journal Year:
2020,
Volume and Issue:
7(4), P. 88 - 88
Published: Nov. 16, 2020
To
investigate
the
hydrology
of
Utah
Lake,
we
analyzed
hydrogen
(δ2H)
and
oxygen
(δ18O)
stable
isotope
composition
water
samples
collected
from
various
components
its
system.
The
average
δ2H
δ18O
values
inlets
are
similar
to
groundwater,
which
in
turn
has
a
that
is
winter
precipitation.
This
suggests
snowmelt-fed
groundwater
main
source
Valley
river
waters.
In
addition,
plot
close
local
meteoric
line,
suggesting
no
significant
evaporation
occurring
these
rivers.
contrast,
lake
outlet
have
higher
δ-values
than
along
lines,
occurrence
evaporation.
Isotope
data
also
indicate
poorly
mixed
horizontally,
but
well
vertically.
Calculations
based
on
mass
balance
equations
provide
estimates
for
percentage
input
lost
by
(~47%),
residence
time
(~0.5
years),
volume
inflow
(~700
million
m3)
during
period
April
November.
short
high
total
coming
might
suggest
more
susceptible
pollution
surface
pollution.