Sustainability,
Journal Year:
2024,
Volume and Issue:
16(21), P. 9229 - 9229
Published: Oct. 24, 2024
The
Tibetan
Plateau
is
the
“Asia
Water
Tower”
and
pivotal
for
Asia
whole
world.
Groundwater
essential
sustainable
development
in
its
alpine
regions,
yet
chemical
quality
increasingly
limits
usability.
present
research
examines
hydrochemical
characteristics
origins
of
phreatic
groundwater
irrigation
areas.
study
probes
signatures,
quality,
regulatory
mechanisms
a
representative
area
Plateau.
findings
indicate
that
maintains
slightly
alkaline
fresh
status,
with
pH
values
ranging
from
7.07
to
8.06
Total
Dissolved
Solids
(TDS)
between
300.25
638.38
mg/L.
composition
mainly
HCO3-Ca
type,
minority
HCO3-Na·Ca
types,
closely
mirroring
profile
river
water.
Nitrogen
contaminants,
including
NO3−,
NO2−,
NH4+,
exhibit
considerable
concentration
fluctuations
within
aquifer.
Approximately
9.09%
sampled
groundwaters
exceed
NO2−
threshold
0.02
mg/L,
28.57%
surpass
NH4+
limit
0.2
mg/L
potable
water
standards.
All
are
below
permissible
NO3−
(50
mg/L).
Phreatic
exhibits
relatively
good
potability,
as
assessed
by
entropy-weighted
index
(EWQI),
95.24%
having
an
EWQI
value
100.
However,
potential
health
risks
associated
elevated
levels,
rather
than
merit
attention
when
such
consumed
minors
at
certain
sporadic
sampling
locations.
does
not
sodium
hazards
or
soil
permeability
damage,
salinity
require
attention.
makeup
primarily
dictated
rock–water
interactions,
silicate
weathering
cation
exchange
reactions,
occasional
influences
dissolution
evaporites
carbonates,
well
reverse
cation-exchange
processes.
While
agricultural
activities
have
caused
notable
rise
salinity,
they
main
contributors
nitrogen
pollution
area’s
groundwater.
Agricultural-derived
pollutants
vigilant
monitoring
avert
extensive
deterioration
ensure
management
resources
Acque Sotterranee-Italian Journal of Groundwater,
Journal Year:
2025,
Volume and Issue:
14(1)
Published: April 1, 2025
This
paper
presents
an
integrated
study
of
groundwater
quality
for
irrigation
and
its
spatial
distribution
in
the
Bou
Arada-El
Arroussa
plain
to
guide
decision-makers
development
sustainable
resource
management
plans.
Assessing
water
this
involves
a
process
that
begins
with
statistical
analysis
determine
similarities
between
samples
group
them
into
clusters.
is
followed
by
principal
component
on
physico-chemical
data
relationships
variables
visualize
their
independence
correlation
matrix.
Statistical
analyses
combined
graphical
approach
through
diagrams
such
as
Piper,
Gibbs,
Wilcox
USSL
are
used
better
assess
properties,
facies
interactions
minerals
within
aquifer.
In
addition,
geographic
information
system
(GIS)
tools
were
combine
indices
create
map
distribution.
Clustering
results
reveal
three
types
water:
first
type
includes
F04,
F05
P01,
characterized
high
concentration
TDS.
The
second
consists
solely
well
P23,
distinguished
elevated
level
K+,
Mg2+
NO3–
ions.
third
can
be
divided
two
subsets:
one
dominated
SO42–
other
Cl–,
additional
ions
HCO3–,
Ca2+
Na+.
Major
show
order
abundance
was
SO42–>Cl–>HCO3–>Ca2+>Mg2+>NO3–>K+.
Piper
ion
ratios
revealed
similar
obtained
from
cluster
dendrogram:
Ca-Mg-SO4,
mixed
Na-Cl
facies.
hardness
index
(TH)
classifies
hard-brackish
category
due
magnesium
calcium
content,
which
crucial
plant
growth
especially
agricultural
area.
investigation
relationship
chemistry
mineralogical
composition
studied
aquifer
reveals
all
fall
field
corresponding
water-rock
interaction,
exception
F04
showing
predominant
evaporation.
Chadha
diagram
shows
majority
located
reverse
exchange
zone,
reflecting
clay
minerals.
belong
C3-S1
category,
not
suitable
salinity
content.
Evaluation
using
standards
use.
A
multi-criteria
layers
(SAR,
SSP,
PS,
RSC,
Na%
IWQI)
created
synthesis
quality.
western
part
Bou-Arada
El
contains
good-quality
water,
while
Eastern
poorest
related
upwelling
poor-quality
deep
water.