Hydrogeochemical Evolution, Isotopic Insights, and Genetic Models of Geothermal Water in Anhui Province, China
Xiaoping Zhou,
No information about this author
Yinxue Peng,
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Yunfeng Li
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et al.
Water,
Journal Year:
2025,
Volume and Issue:
17(2), P. 236 - 236
Published: Jan. 16, 2025
Anhui
Province
is
rich
in
geothermal
water
resources,
making
the
study
of
its
hydrochemical
evolution
and
genetic
models
essential
for
scientific
development
sustainable
utilization.
This
combines
hydrogen–oxygen
isotopic
data
from
different
regions
to
analyze
hydrogeochemical
characteristics
recharge
mechanisms
basin-type
mountainous-type
waters.
The
results
show
that
predominantly
Cl–Na
type,
with
water–rock
interactions
mainly
including
halite
dissolution,
gypsum
dedolomitization,
silicate
hydrolysis.
groundwater
system
relatively
closed
off,
slow
flow
rates.
In
contrast,
mountainous
HCO3–Na·Ca,
SO4–Na·Ca,
SO4–Na
types,
primarily
involving
calcite
dolomite
dissolution.
Enhanced
precipitation
infiltration
due
fault
structures
leads
stronger
an
open-system
characteristic.
two
types
reveal
structural
thermal
reservoirs
under
geological
settings,
highlighting
significant
control
background
on
formation.
Language: Английский
Influence of roughness and slip velocity on the evolution of frictional strength
Quan Gan,
No information about this author
Xinyuan Zhang,
No information about this author
Qiang Li
No information about this author
et al.
International Journal of Rock Mechanics and Mining Sciences,
Journal Year:
2025,
Volume and Issue:
188, P. 106076 - 106076
Published: Feb. 26, 2025
Language: Английский
Study on the Genetic Mechanism of Carbonate Rock Type Hot Mineral Water─A Case Study of Diaozhen, Jinan
Mengyuan Hao,
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Tianming Tang,
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Chang Lu
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et al.
ACS Omega,
Journal Year:
2024,
Volume and Issue:
9(24), P. 26458 - 26471
Published: June 6, 2024
Geothermal
resources
are
one
of
the
most
valuable
in
renewable
energy
because
their
advantages
green
environmental
protection,
stability,
and
reliability.
Carbonate
rock
type
geothermal
reservoirs
have
great
research
significance.
abundant
Shandong
area.
In
this
paper,
we
take
carbonate-type
reservoir
Diaozhen
area
Jinan
City
as
object,
analyze
regional
geological
conditions,
identify
structure.
Through
physical
logging
exploration,
hydrochemical
analysis,
isotope
testing,
drilling
reveal
genesis
mechanism
construct
genetic
model
carbonate
system.
The
results
show
that
belongs
to
a
low-temperature
field
weak
open
karst
thermal
is
mainly
Ordovician
Majiagou
group
limestone.
insulation
caprock
overlying
Quaternary
Neogene
strata
with
cumulative
thickness
1376
m.
geophysical
exploration
wells
data
verify
Mingshui
fracture
seen
around
1630–1645m,
diorite
intrusion
at
1610m.
connects
deep
shallow
aquifers
fluid
migration
channel.
water
from
recharge
atmospheric
precipitation,
rich
ion
content
easy
enrichment
trace
elements.
recharged
by
circulation
lateral
runoff
water.
After
long-distance
migration,
groundwater
continuously
absorbs
heat
surrounding
heated
raw
part.
Deep
rises
along
water-conducting
mixes
cold
form
shallow,
Language: Английский
Evolution of Karst Geothermal Hydrochemical Characteristics and Genesis Mechanism in Northern Jinan, Shandong, Eastern China
Shuchun Wang,
No information about this author
Z. A. Liu,
No information about this author
Wei Zhou
No information about this author
et al.
ACS Omega,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Aug. 16, 2024
The
study
of
geothermal
water
hydrochemical
characteristics
and
solute
transport
evolution
can
provide
a
reliable
hydrogeochemical
basis
for
the
development
protection
resources.
Currently,
there
is
lack
systematic
research
on
mechanism
fields
in
northern
Jinan,
which
limits
use
fields.
In
this
study,
properties
groundwater
Jinan
were
described
by
analyzing
16
samples
3
cold
samples.
results
show
that
during
transformation
from
south
to
north,
contents
major
ions
all
an
increasing
trend
obvious
zoning
characteristics.
type
evolved
HCO3–Ca
HCO3–Ca·Mg
type,
then
further
SO4–Ca
SO4–Ca·Na
water.
Dissolution–precipitation
carbonate,
sulfate,
halite,
silicate
minerals
one
important
processes
controls
chemical
source
mainly
atmospheric
precipitation
Taiyi
Mountain,
with
altitude
698.99–1464.91
m.s.a.l.
thermal
reservoir
temperature
area
estimated
be
55.62–98.16
°C.
This
paper
proposes
conceptual
model
karst
flow
system
provides
new
idea
exploring
genesis
under
similar
geological
conditions.
Language: Английский
Study on the improvement of geothermal cement properties by nanofluid composed of deep eutectic solvent and graphene oxide
Wenxi Zhu,
No information about this author
Bingjie Wang,
No information about this author
S. Cui
No information about this author
et al.
Scientific Reports,
Journal Year:
2024,
Volume and Issue:
14(1)
Published: Nov. 23, 2024
Guided
by
the
goal
of
improving
heat
transfer
efficiency
geothermal
cement,
development
high
thermal
conductivity
fillers
is
urgently
needed.
Considering
drawbacks
carbon-based
in
deteriorating
strength
and
fluidity
this
study
proposes
use
green
low-cost
deep
eutectic
solvents
(DES)
loaded
with
graphene
oxide
to
form
nanofluids
(GONF)
improve
connection
between
cement.
The
basic
properties
GONF-cement
under
storage
conditions
(60–100
°C,
0–36%NaCl)
were
reported,
influence
mechanism
was
analyzed.
following
interesting
conclusions
found:
(1)
oxygen-containing
functional
groups
on
surface
connected
active
sites
DES
through
formation
hydrogen
bond
network,
forming
stable
nanofluids.
(2)
Nanofluids
proven
be
a
(reduce
material
costs
90%)
effective
for
enhancing
mechanical
cement
while
maintaining
appropriate
low
variation
density.
(3)
synergistic
due
fact
that
promotes
hydration
process
providing
reaction
sites,
significantly
reducing
porosity
pore
size
dense
structure
enhances
compressive
shortens
path.
This
enriches
cementing
technology
provides
support
application
exploration
engineering.
Language: Английский