Abstract.
Ocean
alkalinity
enhancement
(OAE)
and
direct
ocean
capture
(DOC)
are
emerging
as
promising
technologies
for
enacting
negative
emissions.
Due
to
the
delayed
air-sea
gas
exchange,
potential
premature
subduction
of
surface
water
parcels
extensive
horizontal
transport
on
timescales
equilibration,
experimental
measurement
induced
CO2
uptake
remains
elusive.
Therefore,
problem
measurement,
reporting
verification
(MRV)
hinges
general
circulation
models.
A
number
recent
studies
have
assessed
efficiency
OAE
using
different
model
setups
metrics.
Some
models
use
prescribed
atmospheric
levels,
while
others
fully
coupled
earth-system
The
former
ignores
feedback
effects,
latter
explicitly
them.
In
this
paper
it
is
shown
that,
even
very
small
deployments,
which
do
no
substantially
change
pCO2,
in
oceanic
inventories
differs
significantly
between
these
methods,
due
causing
some
offgassing.
However,
an
analogous
offgassing
occurs
during
air
(DAC).
care
must
be
taken
compute
correct
metrics
when
assessing
with
respect
determining
emissions
credits,
opposed
effect
global
temperatures.
This
examines
commonly
used
efficiency,
their
exact
physical
meanings,
assumptions
inherent
relationship
It
that
metric
η(t),
pCO2atm
simulations,
equals
equivalent
schedule
a
gradual
(DAC)
removal
system.
Biogeosciences,
Journal Year:
2022,
Volume and Issue:
19(23), P. 5375 - 5399
Published: Dec. 1, 2022
Abstract.
Ocean
alkalinity
enhancement
(OAE)
is
a
proposed
method
to
counteract
climate
change
by
increasing
the
of
surface
ocean
and
thus
chemical
storage
capacity
seawater
for
atmospheric
CO2.
The
impact
OAE
on
marine
ecosystems,
including
phytoplankton
communities
which
make
up
base
food
web,
largely
unknown.
To
investigate
influence
communities,
we
enclosed
natural
plankton
community
from
coastal
Tasmania
22
d
in
nine
microcosms
during
spring
bloom.
Microcosms
were
split
into
three
groups,
(1)
unperturbed
control,
(2)
unequilibrated
treatment
where
was
increased
(+495
±
5.2
µmol
kg−1)
but
CO2
not
equilibrium
with
CO2,
(3)
equilibrated
(+500
3.2
Both
treatments
have
increase
inorganic
carbon
sink
21
%.
We
found
that
simulated
had
significant
generally
moderate
effects
various
groups
heterotrophic
bacteria.
More
pronounced
observed
diatom
silicic
acid
drawdown
biogenic
silica
build-up
reduced
at
alkalinity.
Observed
changes
affected
temporal
trends
key
biogeochemical
parameters
such
as
organic
matter
carbon-to-nitrogen
ratio.
Interestingly,
did
noticeably
larger
(and
bacteria)
than
treatment,
even
though
carbonate
chemistry
conditions
much
more
severe.
This
particularly
evident
occurrence
peak
bloom
experiment,
different
control.
Altogether,
inadvertent
appear
be
rather
limited
relative
enormous
climatic
benefit
note,
however,
detailed
widespread
investigations
responses
are
required
confirm
or
dismiss
this
first
impression.
Biogeosciences,
Journal Year:
2023,
Volume and Issue:
20(1), P. 27 - 43
Published: Jan. 3, 2023
Abstract.
Ocean
alkalinity
enhancement
(OAE)
has
recently
gained
attention
as
a
potential
method
for
carbon
dioxide
removal
(CDR)
at
gigatonne
(Gt)
scale,
with
near-coast
OAE
operations
being
economically
favorable
due
to
proximity
mineral
and
energy
sources.
In
this
paper
we
study
critical
questions
which
determine
the
scale
viability
of
OAE.
Which
coastal
locations
are
able
sustain
large
flux
minimal
pH
ΩArag
(aragonite
saturation)
changes?
What
is
interference
distance
between
adjacent
projects?
How
much
CO2
absorbed
per
unit
added?
quickly
does
induced
deficiency
equilibrate
atmosphere?
Choosing
relatively
conservative
constraints
on
ΔpH
or
ΔOmega,
examine
limits
using
ECCO
LLC270
(0.3∘)
global
circulation
model.
We
find
that
sustainable
rate
varies
over
1–2
orders
magnitude
different
coasts
exhibits
complex
patterns
non-local
dependencies
vary
from
region
region.
general,
in
areas
strong
currents
enables
largest
fluxes
depending
direction
these
currents,
neighboring
sites
can
exhibit
far
400
km
more.
At
steady
state
most
regional
stretches
coastline
accommodate
order
10s
100s
megatonnes
negative
emissions
within
300
coast.
conclude
near-coastal
globally
several
Gt
yr−1
drawdown
constraints,
if
effort
spread
majority
available
coastlines.
Depending
location,
diverse
set
equilibration
kinetics,
determined
by
interplay
gas
exchange
surface
residence
time.
Most
reach
an
uptake
efficiency
plateau
0.6–0.8
mol
after
3–4
years,
there
only
slow
additional
uptake.
Regions
significant
downwelling
(e.g.,
around
Iceland)
should
be
avoided
deployments,
such
up
half
CDR
lost
bottom
waters.
The
ideal
locations,
reaching
molar
ratio
0.8,
include
North
Madagascar,
California,
Brazil,
Peru
close
Southern
Tasmania,
Kerguelen
Patagonia,
where
appears
occur
faster
than
However,
some
Hawaii)
take
significantly
longer
(up
8–10
years)
but
still
eventually
achieve
high
ratios.
Global Change Biology,
Journal Year:
2023,
Volume and Issue:
30(1)
Published: Oct. 31, 2023
Abstract
The
term
carbon
(C)
sequestration
has
not
just
become
a
buzzword
but
is
something
of
siren's
call
to
scientific
communicators
and
media
outlets.
Carbon
the
removal
C
from
atmosphere
storage,
for
example,
in
soil.
It
potential
partially
compensate
anthropogenic
greenhouse
gas
emissions
is,
therefore,
an
important
piece
global
climate
change
mitigation
puzzle.
However,
often
used
misleadingly
and,
while
likely
unintentional,
can
lead
perpetuation
biased
conclusions
exaggerated
expectations
about
its
contribution
efforts.
Soils
have
considerable
take
up
many
are
also
state
continuous
loss.
In
such
soils,
measures
build
soil
may
only
reduction
losses
(C
loss
mitigation)
rather
than
result
real
negative
emissions.
examination
100
recent
peer‐reviewed
papers
on
topics
surrounding
C,
4%
were
found
correctly.
Furthermore,
13%
equated
with
stocks.
review,
further,
revealed
that
leading
will
always
when
non‐CO
2
gases
leakage
taken
into
consideration.
This
paper
highlights
pitfalls
using
incorrectly
calls
accurate
usage
this
going
forward.
Revised
new
terms
suggested
distinguish
clearly
between
SOC
mitigation,
emissions,
accrual
avoid
miscommunication
among
scientists
stakeholder
groups
future.
State of the Planet,
Journal Year:
2023,
Volume and Issue:
2-oae2023, P. 1 - 29
Published: Nov. 27, 2023
Abstract.
Ocean
alkalinity
enhancement
(OAE)
is
an
emerging
strategy
that
aims
to
mitigate
climate
change
by
increasing
the
of
seawater.
This
approach
involves
ocean
enhance
its
capacity
absorb
and
store
carbon
dioxide
(CO2)
from
atmosphere.
chapter
presents
overview
technical
aspects
associated
with
full
range
OAE
methods
being
pursued
discusses
implications
for
undertaking
research
on
these
approaches.
Various
have
been
developed
implement
OAE,
including
direct
injection
alkaline
liquid
into
surface
ocean;
dispersal
particles
ships,
platforms,
or
pipes;
addition
minerals
coastal
environments;
electrochemical
removal
acid
Each
method
has
advantages
challenges,
such
as
scalability,
cost
effectiveness,
potential
environmental
impacts.
The
choice
technique
may
depend
factors
regional
oceanographic
conditions,
source
availability,
engineering
feasibility.
considers
methods,
accelerated
weathering
limestone,
liming,
creation
hydrated
carbonates,
environments.
In
each
case,
technologies
are
considered,
best-practice
drawn.
social
impacts
will
likely
specific
technology
local
context
in
which
it
deployed.
Therefore,
essential
feasibility
undertaken
parallel
with,
informed
by,
wider
impact
assessments.
While
shows
promise
a
mitigation
strategy,
acknowledge
limitations
uncertainties.
Further
development
needed
understand
long-term
effects,
optimize
techniques,
address
unintended
consequences.
should
be
viewed
complementary
extensive
emission
reductions,
improved
if
operated
using
energy
supply
chains
minimal
CO2
emissions.
International Journal of Electrical Power & Energy Systems,
Journal Year:
2023,
Volume and Issue:
155, P. 109544 - 109544
Published: Oct. 6, 2023
Expansion
of
the
energy
demand
accompanies
fossils'
substitution
for
renewables,
requiring
sustainable
pathways
working
through
varying
levels
economic
wealth
and
resource
availability.
Fossil
reserves,
renewable
resources,
transition
metals,
water,
carbon
storage
sites
are
concentrated
in
a
few
countries,
some
relying
on
monetizing
these
resources
to
leverage
growth.
Accelerating
from
fossils
renders
cleaner
while
introducing
co-benefits
impacts,
price
pressure,
safety
issues.
The
affects
energy-intensive
sectors
propagating
clean
strategies
posing
issues
that
may
hinder
development
goals
(SDG).
A
broader
focus
is
needed,
with
clear
vision
many
goals.
work
targer
this
gap
targeted
critical
literature
review
identify
industries
prioritize.
Among
issues,
capture
mitigation
most
cited
aspects.
As
evidenced
by
number
citations
reviewed
works,
waves
progress
among
industries:
Oil
Gas,
Cross
Sectors
Nations
segments
show
fast
responses
occurring
Energy
industry,
Mining,
Heavy
Truck,
Aviation
delayed
decarbonization.
response
lags
attributed
uneven
complexity
achieving
decarbonization
sectors,
which
depend
capital-intensive
long-turnaround
assets
protective
measures.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(1), P. 261 - 277
Published: Jan. 16, 2024
Abstract.
Ocean
alkalinity
enhancement
(OAE)
is
an
emerging
approach
for
atmospheric
carbon
dioxide
removal
(CDR).
The
net
climatic
benefit
of
OAE
depends
on
how
much
it
can
increase
CO2
sequestration
relative
to
a
baseline
state
without
OAE.
This
so-called
“additionality”
be
calculated
as
follows:
Additionality=COAE-ΔCbaseline.
So
far,
feasibility
studies
have
mainly
focussed
enhancing
in
the
oceans
stimulate
(COAE);
however,
primary
focus
has
not
been
such
anthropogenic
would
modify
natural
cycle
and
associated
(ΔCbaseline).
Here,
I
present
incubation
experiments
which
materials
considered
(sodium
hydroxide,
steel
slag,
olivine)
are
exposed
beach
sand
investigate
influence
sources
sinks.
show
that
strongly
reduce
generation
alkalinity,
thereby
reducing
additionality.
because
increases
calcium
carbonate
saturation
state,
reduces
dissolution
from
sand,
source.
argue
this
“additionality
problem”
potentially
widespread
applies
many
marine
systems
where
implementation
–
far
beyond
scenario
investigated
study.
However,
problem
mitigated
by
dilute
dosing
into
ocean
environment
avoidance
cycling
hotspots,
sediments.
Understanding
potential
slowdown
through
introduction
will
crucial
assessment
Energy & Fuels,
Journal Year:
2022,
Volume and Issue:
36(21), P. 12917 - 12945
Published: Oct. 24, 2022
Analytical
chemistry
is
powerful
in
analyzing
complex
mixtures
of
crude
oil
and
brine
subsurfaces
on
the
basis
atomic
molecular
levels.
Geochemistry
applies
chemical
principles
experiments
to
understand
earth
science
engineering
problems.
Crude
oil's
molecule
structure,
especially
for
resin
asphaltenes,
could
only
be
understood
using
advanced
analytical
techniques.
Fingerprinting
geochemistry
applied
conventional
unconventional
reservoirs
helps
better
identify
hydrocarbon
resources.
Subsequently,
reservoir
fluid
geodynamics
(RFG)
discipline
promoted
because
gap
between
basin
modeling
simulation
models
with
data.
Fluid
migration
elaborated
from
geological
time
when
trap
was
formed
nowadays
span
millions
years.
Also,
asphaltene
data
used
delineate
compartmentalization.
This
work
reviews
state-of-art
theory
technology
upstream
gas
industry
proposes
an
improvement
high-resolution
power
efficient
sustainable
energy
development.
State of the Planet,
Journal Year:
2023,
Volume and Issue:
unknown, P. 1 - 1
Published: Nov. 27, 2023
Abstract.
Ocean
alkalinity
enhancement
(OAE)
is
a
proposed
marine
carbon
dioxide
removal
(mCDR)
approach
that
has
the
potential
for
large-scale
uptake
of
significant
amounts
atmospheric
(CO2).
Removing
anthropogenic
legacy
CO2
will
be
required
to
stabilise
global
surface
temperatures
below
1.5â2ââC
Paris
Agreement
target
2015.
In
this
chapter
we
describe
impacts
various
OAE
feedstocks
on
seawater
carbonate
chemistry,
as
well
pitfalls
need
avoided
during
sampling,
storage,
and
measurement
four
main
chemistry
parameters,
i.e.
dissolved
inorganic
(DIC),
total
(TA),
pH,
fugacity
(fCO3)
might
have
been
precipitated
upon
increase
it
otherwise
interfere
with
number
analyses;
(3)Â
samples
DIC
can
stabilised
avoid
risk
CaCO3
precipitation
sample
storage;
(4)Â
some
require
additional
adjustments
using
available
programs
routines,
instance
if
magnesium
or
concentrations
modified.
Biogeosciences,
Journal Year:
2023,
Volume and Issue:
20(10), P. 1963 - 1977
Published: May 26, 2023
Abstract.
The
Amazon
River
plume
plays
a
critical
role
in
shaping
the
carbonate
chemistry
over
vast
area
western
tropical
North
Atlantic.
We
conduct
sensitivity
analysis
of
hypothetical
ocean
alkalinity
enhancement
(OAE)
via
quicklime
addition
watershed,
examining
response
and
air–sea
carbon
dioxide
flux
to
addition.
Through
series
tests,
we
show
that
detectability
OAE-induced
increment
depends
on
perturbation
strength
(or
size
addition,
ΔTA)
number
samples:
there
is
90
%
chance
meet
minimum
requirement
with
ΔTA>15
µmol
kg−1
sample
>40,
given
background
variability
15–30
kg−1.
pCO2
reduction
at
surface
would
range
between
0–25
µatm
when
ΔTA=20
kg−1,
decreasing
increasing
salinity
(S).
Adding
20
river
mouth
could
elevate
total
uptake
(15<S<35)
by
least
0.07–0.1
Mt
CO2
per
month,
major
portion
occur
saltiest
region
(S>32)
due
its
large
size,
comprising
approximately
80
S>15
area.
However,
lowest-salinity
(S<15)
has
greater
drop
partial
pressure
(pCO2sw)
low
buffer
capacity,
potentially
allowing
for
observational
pCO2sw
this
region.
Reduced
outgassing
part
plume,
while
more
uncertain,
may
also
be
important
additional
uptake.
Such
tests
are
useful
designing
minimalistic
field
trials
setting
achievable
goals
monitoring,
reporting,
verification
purposes.