Environmental Research Letters,
Journal Year:
2024,
Volume and Issue:
19(7), P. 074033 - 074033
Published: May 29, 2024
Abstract
To
achieve
the
Paris
climate
target,
deep
emissions
reductions
have
to
be
complemented
with
carbon
dioxide
removal
(CDR).
However,
a
portfolio
of
CDR
options
is
necessary
reduce
risks
and
potential
negative
side
effects.
Despite
large
theoretical
potential,
ocean-based
such
as
ocean
alkalinity
enhancement
(OAE)
has
been
omitted
in
change
mitigation
scenarios
so
far.
In
this
study,
we
provide
techno-economic
assessment
large-scale
OAE
using
hydrated
lime
(‘ocean
liming’).
We
address
key
uncertainties
that
determine
overall
cost
liming
(OL)
CO2
uptake
efficiency
per
unit
material,
distribution
strategies
avoiding
carbonate
precipitation
which
would
compromise
efficiency,
technology
availability
(e.g.,
solar
calciners).
find
at
economic
costs
130–295
$/tCO2
net-removed,
could
competitive
option
make
significant
contribution
towards
target.
As
identified
no
showstoppers,
argue
for
more
research
on
ecosystem
impacts,
governance,
monitoring,
reporting,
verification,
development
whether
other
should
considered
part
broader
portfolio.
Biogeosciences,
Journal Year:
2025,
Volume and Issue:
22(2), P. 355 - 384
Published: Jan. 21, 2025
Abstract.
Marine
enhanced
rock
weathering
(mERW)
is
increasingly
receiving
attention
as
a
marine-based
carbon
dioxide
removal
(CDR)
technology.
The
method
aims
to
achieve
ocean
alkalinity
enhancement
(OAE)
by
introducing
fast-weathering
rocks
into
coastal
systems.
latter
envisioned
act
large
natural
biogeochemical
reactor,
where
ambient
physical
and
biological
processes
can
stimulate
dissolution,
thus
generating
concomitant
release
increasing
the
seawater's
capacity
sequester
CO2.
Olivine
has
been
put
forward
prime
candidate
mineral
for
mERW,
but
at
present,
no
peer-reviewed
results
are
available
from
larger-scale
field
studies
in
areas,
so
information
about
olivine
dissolution
marine
systems
largely
derived
laboratory
experiments.
As
result,
key
uncertainties
remain
concerning
efficiency,
CO2
sequestration
potential,
impact
of
olivine-based
mERW
under
relevant
conditions.
In
this
review,
we
summarize
recent
research
advancements
bridge
gap
between
existing
real-world
environment
which
intended
take
place.
To
end,
identify
parameters
that
govern
kinetics
sediments
associated
enable
us
number
still
with
respect
implementation
upscaling
ERW,
well
monitoring,
reporting,
verification
(MRV).
From
our
analysis,
conclude
current
knowledge
base
not
sufficient
predict
outcome
situ
applications.
Particularly,
pore-water
saturation
on
rate
question
additionality
generation
critical
unknowns.
more
confidently
assess
potential
dedicated
pilot
conditions
needed,
should
be
conducted
sufficiently
spatial
scale
monitored
long
enough
time
temporal
resolution.
Additionally,
analysis
indicates
specific
sediment
type
application
site
(e.g.,
cohesive
versus
permeable)
will
factor
applications,
it
significantly
influencing
pH,
dynamics,
generation.
Therefore,
future
also
target
different
types.
State of the Planet,
Journal Year:
2023,
Volume and Issue:
2-oae2023, P. 1 - 9
Published: Nov. 27, 2023
Abstract.
The
Paris
Agreement
to
limit
global
warming
well
below
2
∘C
requires
the
ambitious
reduction
in
greenhouse
gas
emissions
and
balancing
of
remaining
through
carbon
sinks
(i.e.,
deployment
dioxide
removal
or
CDR).
While
climate
mitigation
scenarios
until
now
primarily
consider
land-based
CDR
methods,
there
is
growing
concern
about
their
potential
deliver
sufficient
CDR,
marine
options
are
receiving
more
interest.
Based
on
idealized
theoretical
studies,
ocean
alkalinity
enhancement
(OAE)
appears
as
a
promising
method.
However,
knowledge
base
insufficient
for
robust
assessment
its
practical
feasibility,
side
effects,
social
governance
aspects,
monitoring
verification
issues.
A
number
research
efforts
aims
improve
this
timely
manner.
We
provide
an
overview
current
situation
developing
OAE
method
describe
history
that
has
led
creation
best
practices
guide.
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
Biogeosciences,
Journal Year:
2025,
Volume and Issue:
22(2), P. 405 - 415
Published: Jan. 22, 2025
Abstract.
The
urgent
necessity
of
reducing
greenhouse
gas
emissions
is
coupled
with
a
pressing
need
for
widespread
implementation
carbon
dioxide
removal
(CDR)
techniques
to
limit
the
increase
in
mean
global
temperature
levels
below
2
°C
compared
pre-industrial
times.
One
proposed
CDR
method,
ocean
alkalinity
enhancement
(OAE),
mimics
natural
rock
weathering
processes
by
introducing
suitable
minerals
into
ocean,
thereby
increasing
and
promoting
CO2
chemical
absorption.
While
theoretical
studies
hold
promise
OAE
as
climate
mitigation
strategy,
careful
consideration
its
ecological
implications
essential.
Indeed,
impact
enhanced
on
marine
organisms
remains
subject
investigation,
it
may
lead
changes
species
composition.
implicates
favorable
conditions
calcifying
enhancing
saturation
state
calcium
carbonate
decreasing
energetic
costs
calcification.
This
affect
primary
production
improving
phytoplankton,
among
which
coccolithophores
play
leading
role.
They
contribute
<
10
%
but
are
responsible
large
proportion
calcite
deposition.
previous
research
has
extensively
studied
effects
acidification
coccolithophores,
fewer
have
explored
impacts
elevated
pH
alkalinity.
In
this
context,
we
sensitivity
Emiliania
huxleyi,
most
coccolithophore
species,
culture
experiment.
We
monitored
species'
growth
calcification
response
progressively
total
(TA).
Above
change
(ΔTA)
∼
600
µmol
kg−1,
concentrations
decreased,
E.
huxleyi
rate
diminished,
suggesting
threshold
concentration
100
µatm
necessary
optimal
growth.
cellular
organic
ratio
(PIC
:
POC)
remained
stable
over
range.
Due
enhancement,
formation
was
lower.
rapidly
advancing
already
reached
field-testing
stage.
Hence,
our
study
contributes
critical
part
investigations
required
comprehend
potential
biological
before
large-scale
adopted.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(11), P. 2777 - 2794
Published: June 12, 2024
Abstract.
Gigatonne-scale
atmospheric
carbon
dioxide
removal
(CDR)
will
almost
certainly
be
needed
to
supplement
the
emission
reductions
required
keep
global
warming
between
1.5–2
°C.
Ocean
alkalinity
enhancement
(OAE)
is
an
emerging
marine
CDR
method
with
addition
of
pulverised
minerals
surface
ocean
being
one
widely
considered
approach.
A
concern
this
approach
potential
for
dissolution
products
released
from
impact
phytoplankton
communities.
We
conducted
experiment
10
pelagic
mesocosms
(M1–M10)
in
Raunefjorden,
Bergen,
Norway,
assess
implications
simulated
silicate-
and
calcium-based
mineral
OAE
on
a
coastal
plankton
community.
Five
(M1,
M3,
M5,
M7,
M9)
were
enriched
silicate
(∼
75
µmol
L−1
Na2SiO3),
along
gradient
0
∼
600
kg−1,
magnesium
proportion
additions.
The
other
five
(M2,
M4,
M6,
M8,
M10)
same
calcium
explored
many
components
community,
microbes
fish
larvae,
here
we
report
influence
based
diatom
silicification.
Macronutrients
(nitrate
phosphate)
limited
silicification
at
onset
until
nutrient
additions
day
26.
Silicification
was
significantly
greater
silicate-based
treatment,
all
genera
except
Cylindrotheca
displaying
increase
as
result
increased
concentration
dissolved
silicate.
In
contrast
effect
differences
concentrations
two
treatments,
increases
only
influenced
genera,
Pseudo-nitzschia
Nitzschia.
four
(Arcocellulus,
Cylindrotheca,
Skeletonema,
Thalassiosira)
investigated
displayed
no
significant
changes
kg−1
above
natural
levels.
summary,
our
findings
illustrate
that
via
methods
has
genus-specific
impacts
diatoms.
This
research
underscores
importance
understanding
full
breadth
different
approaches,
their
risks,
co-benefits,
interactive
effects.
Frontiers in Climate,
Journal Year:
2024,
Volume and Issue:
6
Published: April 12, 2024
Research
over
the
past
decade
has
resulted
in
various
methods
for
removing
CO
2
from
atmosphere
using
seawater
and
electrochemically
generated
acids
bases.
This
Perspective
aims
to
present
a
unified
framework
comparing
these
approaches.
Specifically,
can
all
be
seen
as
falling
into
one
of
two
categories:
those
that
result
net
increase
ocean
alkalinity
use
“ocean
sponge”
atmospheric
(ocean
enhancement,
or
OAE)
cycle
pump”
cycling,
OAC).
In
this
Perspective,
approaches
marine
carbon
dioxide
removal
(mCDR)
electrochemistry
are
compared
framework,
similarities
differences
categories
explored.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(11), P. 2859 - 2876
Published: June 13, 2024
Abstract.
Ocean
alkalinity
enhancement
(OAE)
is
a
negative
emissions
technology
(NET)
that
shows
significant
potential
for
climate
change
mitigation.
By
increasing
the
bicarbonate
ion
concentration
in
ocean
water,
OAE
could
enhance
long-term
carbon
storage
and
mitigate
acidification.
However,
side
effects
and/or
co-benefits
of
on
natural
planktonic
communities
remain
poorly
understood.
To
address
this
knowledge
gap,
mesocosm
experiment
was
conducted
oligotrophic
waters
Gran
Canaria.
A
CO2-equilibrated
total
(TA)
gradient
employed
increments
300
µmol
L−1,
ranging
from
∼
2400
to
4800
L−1.
This
study
represents
first
attempt
evaluate
impacts
under
conditions.
The
results
show
net
community
production
(NCP),
gross
(GP),
respiration
(CR)
rates,
metabolic
balance
(GP:CR)
did
not
exhibit
linear
response
whole
gradient.
Instead,
polynomial
regression
models
were
observed
all
rates
up
ΔTA
1800
relation
dissolved
inorganic
(DIC)
concentrations.
Notably,
1500
L−1
treatments
showed
peaks
NCP
shifting
heterotrophic
an
autotrophic
state,
with
values
4
8
O2
kg−1
d−1,
respectively.
These
optimum
curve
also
reflected
nanoplankton
abundance,
size-fractionated
chlorophyll
a,
14C
uptake
data.
Furthermore,
abiotic
precipitation
occurred
highest
treatment
after
day
21,
but
no
impact
measured
parameters
detected.
Overall,
damaging
effect
range
applied
here
phytoplankton
primary
production,
metabolism,
composition
be
inferred.
In
fact,
co-benefit
form
positive
curvilinear
DIC
treatment.
Further
experimental
research
at
scale
key
gain
better
understanding
short-
communities.
Abstract
Carbon
dioxide
removal
from
the
atmosphere
and
storage
over
long
times
scales
in
terrestrial
marine
reservoirs
is
urgently
needed
to
limit
global
warming
for
sustainable
management
of
carbon
cycle.
Ocean
alkalinity
enhancement
by
artificial
addition
carbonate
minerals
seafloor
has
been
proposed
as
a
method
sequester
atmospheric
CO
2
store
it
ocean
dissolved
bicarbonate.
Here,
reaction-transport
model
used
scrutinize
efficacy
calcite
dissolution
at
well-studied
site
southwestern
Baltic
Sea
–
brackish
coastal
water
body
northern
Europe.
We
find
that
most
simply
buried
without
under
moderate
rates.
Applying
other
sites
suggests
rates
efficiencies
are
higher
areas
with
low
salinity
undersaturated
bottom
waters.
A
simple
box
predicts
tentative
net
uptake
rate
3.2
megatonnes
per
year
wider
after
continually
adding
muddy
sediments
10
years.
More
robust
estimates
now
require
validation
field
studies.
Ocean
alkalinity
enhancement
(OAE)
based
on
enhanced
weathering
of
olivine
(EWO)
is
a
promising
marine
carbon
dioxide
removal
(mCDR)
technique.
Previous
research
primarily
focuses
the
toxicological
effects
potentially
toxic
metals
(PTMs)
released
from
olivine.
In
this
Perspective,
we
explore
overlooked
impacts
EWO
environmental
media
in
two
scenarios:
applied
to
beaches/shallow
continental
shelves
and
offshore
dispersion
by
vessels.
We
analyze
potential
migration
pathways
iron
PTMs
(e.g.,
nickel
chromium)
after
their
release,
interactions
with
manganese
oxides
sediments,
causing
secondary
contamination.
Additionally,
propose
mitigation
strategies
prevent
PTM
concentrations
exceeding
local
quality
standards,
including
use
alkalization
equipment
control
levels.
This
Perspective
underscores
need
for
thorough
assessments
prior
large-scale
implementation
ensure
sustainability
efficacy
mCDR
efforts.