Abstract.
Ocean
alkalinity
enhancement
(OAE)
is
a
promising
approach
to
marine
carbon
dioxide
removal
(mCDR)
that
leverages
the
large
surface
area
and
storage
capacity
of
oceans
sequester
atmospheric
CO2
as
dissolved
bicarbonate
(HCO3-).
The
SEAMATE
(Safe
Elevation
Alkalinity
for
Mitigation
Acidification
Through
Electrochemistry)
process
uses
electrochemistry
convert
some
salt
(NaCl)
in
seawater
or
brine
into
aqueous
acid
(HCl),
which
removed
from
system,
base
(NaOH),
returned
ocean
with
remaining
seawater.
resulting
increase
pH
causes
shift
inorganic
(DIC)
speciation
toward
carbonate
decrease
surface-ocean
pCO2.
pCO2
results
enhanced
CO2
uptake
reduced
loss
by
due
gas
exchange.
net
result
this
DIC,
where
it
durably
stored
as
mostly
carbonate.
In
study,
we
systematically
test
efficiency
treated
NaOH
at
beaker
(1
L),
aquaria
(15
tank
(6000
L)
scales
establish
operational
boundaries
safety
scaling
up
field
experiments.
Preliminary
show
equilibration
occurred
on
order
weeks
months,
depending
circulation,
air
forcing,
bubbling
conditions
within
tanks.
An
~0.7–0.9
mol
DIC/
added
(in
form
NaOH)
was
observed
through
analysis
bottle
samples
sensor
data,
consistent
value
expected
given
values
system
equilibrium
calculations
range
salinities
temperatures
tested.
Mineral
precipitation
when
bulk
exceeded
10.0
Ωaragonite
exceeded
30.0.
This
dominated
Mg(OH)2
over
hours
1
day
before
shifting
CaCO3,
aragonite
precipitation.
These
combined
models
dilution
advection
alkaline
plumes,
will
allow
estimation
amount
OAE
pilot
studies.
Future
experiments
should
better
approximate
including
sediment
interactions,
biological
activity,
air-sea
exchange
rates,
mixing-zone
dynamics.
The
feasibility
and
performance
of
nuclear
energy
coupled
with
Negative
Emission
Technology
(NET)
processes
were
investigated
in
this
report.
Three
overarching
questions
from
NET
systems
guided
research:
which
would
be
able
to
use
heat
and/or
electricity
power
plants
(NPPs);
what
is
the
cost
a
system;
market
outlook
for
system?
Among
various
NETs
that
are
actively
being
developed,
several
found
potentially
benefit
coupling
an
NPP
via
(1)
large
amounts
decarbonized
constant-output
electricity;
(2)
free
waste
or
cheap
low-temperature
heat;
(3)
high-temperature
heat.
NPPs
compatible
Direct
Air
Capture
(DAC)
systems,
detailed
techno-economic
analysis
NPP&DAC
was
performed.
Preliminary
also
indicated
biomass
water-based
NPPs,
but
further
work
needed
quantify
these
systems.
Design
analyses
completed
both
liquid
solvent
DAC
(L-DAC)
solid
sorbent
(S-DAC)
technologies.
A
1.0-GWth
L-DAC
S-DAC
capture
12–15
Mt
CO2/yr
1.0–1.5
CO2/yr,
respectively.
While
process
enables
much
greater
CO2
than
when
sized
1
GWth
NPP,
NPP&L-DAC
system
considered
requires
>2
natural
gas
oxy-combustion
reach
adequate
temperature
calciner.
generated
combustion
captured
as
part
calcination
process,
addition
air,
resulting
overall
sequestration
close
30%
more
air.
carbon
calculated
levelized
(LCOD)
had
range
$\$170–260$/tCO2
$\$650–680$/tCO2
NPP&S-DAC
For
provides
economic
compared
previous
National
Energy
Laboratory
(NETL)
studies
non-nuclear
leading
reduction
LCOD
by
5–7%
L-DAC,
8–13%
S-DAC.
preliminary
reviewed
potential
prices
eligibility
incentives.
estimated
revenues
(coming
federal
incentive,
commodity
markets,
offset
market)
$\$170–979$
tCO2,
results
show
because
lower
LCOD,
attractive
process.
investment
require
long-term
certainty
sufficient
size,
prices,
Enabling
ramp
operation
up
down
based
on
price
not
expected
significantly
increase
system.
This
required
very
high
justify
deployment
continuous
expensive
In
analysis,
new
research
uncovered,
follow-up
recommended
investigation,
including
study
other
such
pyrolysis
gasification
storage,
seawater
capture.
ACS Applied Materials & Interfaces,
Journal Year:
2023,
Volume and Issue:
16(1), P. 712 - 722
Published: Dec. 29, 2023
Mineralization
by
MgO
is
an
attractive
potential
strategy
for
direct
air
capture
(DAC)
of
CO2
due
to
its
tendency
form
carbonate
phases
upon
exposure
water
and
CO2.
Hydration
during
this
process
typically
assumed
not
be
rate
limiting,
even
at
ambient
temperatures.
However,
surface
passivation
hydrated
likely
reduces
the
capacity.
Here,
we
examine
initial
hydration
reactions
that
occur
on
MgO(100)
surfaces
determine
whether
they
could
potentially
impact
uptake.
We
first
used
atomic
force
microscopy
(AFM)
explore
changes
in
reaction
layers
(pH
=
6
12)
MgO-saturated
solution
11)
found
are
heterogeneous
nonuniform.
To
how
relative
humidity
(R.H.)
affects
reactivity,
reacted
samples
room
temperature
nominally
dry
N2
(∼11–12%
R.H.)
up
12
h,
humid
(>95%
5,
10,
15
min,
33
75%
R.H.
8
days.
X-ray
reflectivity
electron
analysis
reveal
rapidly
air,
but
growth
layer
slows
after
formation.
Reaction
thickness
strongly
correlated
with
R.H.,
denser
forming
compared
33%
or
N2.
The
amorphous
poorly
crystalline
based
grazing
incidence
diffraction
measurements.
After
days,
increases
density
as
sample
5–15
min.
This
may
represent
step
toward
crystallization
layer.
Overall,
high
favors
formation
a
hydrated,
disordered
MgO.
Based
our
results,
DAC
location
higher
will
favorable,
slow
significantly
from
rates
short
timescales,
presumably
passivation.
Abstract.
Ocean
alkalinity
enhancement
(OAE)
is
a
promising
approach
to
marine
carbon
dioxide
removal
(mCDR)
that
leverages
the
large
surface
area
and
storage
capacity
of
oceans
sequester
atmospheric
CO2
as
dissolved
bicarbonate
(HCO3-).
The
SEAMATE
(Safe
Elevation
Alkalinity
for
Mitigation
Acidification
Through
Electrochemistry)
process
uses
electrochemistry
convert
some
salt
(NaCl)
in
seawater
or
brine
into
aqueous
acid
(HCl),
which
removed
from
system,
base
(NaOH),
returned
ocean
with
remaining
seawater.
resulting
increase
pH
causes
shift
inorganic
(DIC)
speciation
toward
carbonate
decrease
surface-ocean
pCO2.
pCO2
results
enhanced
CO2
uptake
reduced
loss
by
due
gas
exchange.
net
result
this
DIC,
where
it
durably
stored
as
mostly
carbonate.
In
study,
we
systematically
test
efficiency
treated
NaOH
at
beaker
(1
L),
aquaria
(15
tank
(6000
L)
scales
establish
operational
boundaries
safety
scaling
up
field
experiments.
Preliminary
show
equilibration
occurred
on
order
weeks
months,
depending
circulation,
air
forcing,
bubbling
conditions
within
tanks.
An
~0.7–0.9
mol
DIC/
added
(in
form
NaOH)
was
observed
through
analysis
bottle
samples
sensor
data,
consistent
value
expected
given
values
system
equilibrium
calculations
range
salinities
temperatures
tested.
Mineral
precipitation
when
bulk
exceeded
10.0
Ωaragonite
exceeded
30.0.
This
dominated
Mg(OH)2
over
hours
1
day
before
shifting
CaCO3,
aragonite
precipitation.
These
combined
models
dilution
advection
alkaline
plumes,
will
allow
estimation
amount
OAE
pilot
studies.
Future
experiments
should
better
approximate
including
sediment
interactions,
biological
activity,
air-sea
exchange
rates,
mixing-zone
dynamics.