C&EN Uncovered: Can altering ocean chemistry fight climate change?

Stereo Chemistry

Can climate catastrophe be stymied by tweaking seawater chemistry?

In this episode of C&EN Uncovered, host Craig Bettenhausen speaks with C&EN reporter Fionna Samuels about her recent C&EN cover story concerning Ocean Alkalinity Enhancement (OAE) as a method to combat climate change by increasing ocean alkalinity to absorb more CO2. Uncovered offers a deeper look at subjects from recent stories pulled from the pages of Chemical & Engineering News. Check out Fionna's story on engineering our oceans to mitigate the effects of Climate Change.

Subscribe to Stereo Chemistry now on Apple Podcasts, Spotify, or wherever you listen to podcasts.

Credits

Executive Producer: David Anderson

Host: Craig Bettenhausen

Reporter: Fionna Samuels

Video + Audio Producer: Jeremy Barr

Episode artwork: Michael Sswat

Music: Commercial Flow, Shutterstock

Contact Stereo Chemistry: Contact us on social media at @cenmag or email cenfeedback@acs.org.

2025-06-19 21 min Transcript

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Transcript

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Craig Bettenhausen: Craig,
welcome to CNN uncovered. I'm

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Craig Bettenhausen. CNN
uncovered is a podcast series

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00:00:05,190 --> 00:00:07,650
from Stereo Chemistry. In each
episode, we'll take another look

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at a recent cover story in
chemical and Engineering News,

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and hear from CNN reporters
about striking moments from

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their reporting, their biggest
takeaways, and what got left on

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the cutting room floor. This
episode, we're looking at a

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recent cover story about a CO
two abatement method called

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Ocean alkalinity enhancement
that aims to use the world's

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oceans to remove more carbon
from the atmosphere. Are Earth's

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vast oceans our biggest allies
in the fight against greenhouse

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gasses. Can we augment the power
of nature to keep our planet

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alive longer? We'll put a link
to the story in today's show

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notes. I'm here with CNN
assistant editor Fiona Samuels,

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who wrote the article. Hi Fiona.

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Fionna Samuels: Hi Craig. It's
so nice to be here.

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Craig Bettenhausen: Yeah, good
to have you.

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for

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So for anyone that hasn't had a
chance to read the story yet,

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can you give a brief recap of
what's in the article? Yeah, so

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basically, I reported on a few
different experiments, field

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trials, specifically, that are
happening around the world to

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look at how we can add alkaline
substances to ocean water in

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order to help it draw down more
carbon dioxide from the

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atmosphere. And all of this is
in an effort to sort of stymie

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the worst effects of climate
change. And how did you get

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interested in this topic? It
actually started out looking at

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solar radiation modification, or
solar geoengineering, which is

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putting stuff into the
atmosphere to reflect sunlight

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back into space. But it turns
out that there are almost no

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field trials happening in that
space right now because it's so

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controversial, and the method is
very questionable. But there is

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quite a few different things
happening in the marine carbon

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dioxide removal space. So
instead of reflecting sunlight

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to cool the planet, removing
carbon dioxide to help cool the

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planet, interesting. So one of
the things I had noticed in your

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story is this experiment called
Loch Ness. Tell me about Loch

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Ness. The experiment not the
Celtic sea monster or both. I'm

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flexible.

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Fionna Samuels: So unlike the
monster, I guess this experiment

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is real and it's officially
happening. They just got the

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permit, finally approved with
the EPA. It's being led by a

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researcher at Woods Hole
Oceanographic Institute. His

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name is Dr Adam Subhas, and what
they're doing is they are

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releasing a solution of sodium
hydroxide into the water and

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looking at where that alkaline
water goes, and measuring a

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whole bunch of different things
to try to see if they can

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quantify how much carbon dioxide
is absorbed by the water because

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of that increased alkalinity.
Seems too simple to be

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intuitive. Can you explain how
would dumping a bunch of lye

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into the water do anything about
carbon dioxide in the

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atmosphere. Well, so carbon
dioxide dissolves in water

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naturally. This is an ongoing
geochemical process, and when

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the gas dissolves into the
water, it quickly reacts to form

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carbonic acid, which then
dissolves into different

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carbonate ions. And because it's
an acid protons, so that's why

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we get ocean acidification. And
it was really interesting

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because many of the researchers
that I spoke to for this story

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started off as researchers of
ocean acidification. So the pH

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plays a big role in how much
carbon dioxide can be absorbed

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and then sequestered in ocean
water. And by raising the pH or

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making it more alkaline, not
only are you sort of combating

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that acidification that happens
with carbon dioxide dissolution,

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but you're also making it so
more carbon dioxide can be

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absorbed and then sequestered as
carbonate ions and bicarbonate

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ions. It's a little bit like
magic, to be honest.

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Craig Bettenhausen: And what
kind of scales would this need

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to operate on to make an impact?

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Fionna Samuels: Well, that's a
great question. So right now,

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humanity is releasing carbon
dioxide on gigaton orders of

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magnitude. So that's 1 billion
metric tons, and it's our annual

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emissions are close to 40
billion metric tons. Obviously

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we need to reduce emissions.
That's number one. But there are

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certain sectors that can't be
easily decarbonized. So

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aviation, agriculture, those
cows are going to keep farting.

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So we need to do more than just
radically decrease emissions.

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Scientists think we need to also
start removing carbon dioxide

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from the atmosphere, but if
we're thinking on gigaton scale

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of emissions, we want to
probably remove gigatons of

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carbon dioxide. That would be
great. We can't do that right

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now. We're not even to millions
of metric tons. So one of the

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researchers, David Ho, had a
really good analogy. He thinks

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of carbon removal like a time
machine. So if you're thinking

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we're emitting 40 billion metric
tons of carbon dioxide annually

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around the globe. And if we
could remove 1 million metric

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tons with these carbon dioxide
removal techniques, you would

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have had gone back 13 minutes in
time. That's equivalent to 13

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minutes of carbon emissions. So
the scale is huge, and.

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It's impossible to do it with
carbon dioxide removal

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techniques alone. Emission
reduction is absolutely vital.

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Craig Bettenhausen: So I can
imagine getting sodium hydroxide

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on a laboratory scale. You can
get it at the hardware store,

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but on that kind of scale, we're
not just talking about that kind

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of material. Where are we going
to get that much base

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equivalence, that much
alkalinity? Yeah,

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Fionna Samuels: so now you're
talking about sort of the life

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cycle of these sort of
techniques. And there's actually

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a few different techniques. It's
not just putting sodium

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hydroxide in the water. So with
sodium hydroxide, the Loch Ness

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team is truly only interested in
figuring out if ocean alkalinity

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enhancement is a viable
solution, and so they're

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basically using the cleanest
form of alkalinity in the sense

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that sodium hydroxide, they can
be incredibly confident of what

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they're putting in the water.
They can be very confident about

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the kinds of reactions that are
happening. Sodium ions already

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exist in seawater. Hydroxide
ions also exist in seawater, but

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obviously at a far lower
abundance and the pH, they very

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well constrained how the pH will
fluctuate after their release

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and at different timescales
after the release. That's why

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they're using sodium hydroxide
in the real world. You're right.

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Sodium hydroxide is not
necessarily a viable way to

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increase the alkalinity of these
bodies of water, because you

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would need vast amounts of it.
And right now, a lot of sodium

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hydroxide is actually produced
in chlorine chemical reactions,

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but we produce chlorine for
other chemistry is happening

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anyway. Other researchers are
looking at alkaline minerals. So

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like olivine is a big one, and
that would come from mining

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minerals around the world. We
humanity, different people are

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already sort of spreading these
mined minerals on agricultural

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fields and elsewhere. So those
sources of mineral alkalinity

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exist already, which is why
these folks who are using

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minerals argue that that might
be a better option. A third

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technique actually uses
electrolysis to separate

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alkaline seawater from acidic
seawater. But the problem with

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that is then you have a bunch of
acid, and there's not a huge

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market for acid to change the pH
of things. So you're right when

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it comes to scalability, the
life cycle of these chemicals is

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very important to consider,
where they're coming from, where

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the byproducts are going. If
we're thinking about mining

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alkaline minerals, you need to
think about if those mines are

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emitting more carbon than can be
taken up by the ocean or other

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carbon dioxide removal
techniques where the energy is

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coming from. All of this stuff
is a big question mark. The

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field trials right now are
really focused on whether or not

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the chemistry is workable from a
standpoint of like we

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theoretically know that this
should work, but does it in the

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real world.

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Craig Bettenhausen: So that
suggests the question, how are

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they going to tell what are they
measuring to see if this

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Fionna Samuels: works? They're
measuring a bunch of different

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things. So the Woods Hole folks
are. They're throwing the whole

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instrument laboratory at the
problem. They're going to be

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taking water in through the ship
that they're driving and

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releasing the alkaline solution
behind to sample for the

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pressures of oxygen and carbon
dioxide dissolved in the water.

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They're also going to be looking
at how the pH changes. They're

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going to be looking at total
dissolved inorganic carbon,

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which is all those carbonate
ions. They're going to be

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looking at changes in the marine
life in the area. Of course,

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they're going to make sure that
they're not, or they plan to

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make sure that they're not going
to be dumping anything on a

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whale's head, right? But as long
as there's not any big animals

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around the they're gonna dump
this solution, and then they

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will be taking a plankton net
and dragging the plankton net

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behind the boat to look at how
these little, tiny marine plant,

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like creatures, plankton, is
hard to find. Sorry,

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Craig Bettenhausen: yeah, things
at the bottom of the food web,

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how the bottom of the food web?
Yes, yes, they're

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Fionna Samuels: looking at how
plankton, which is the bottom of

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the food web, will be affected
by this experiment in the real

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world, because other researchers
have already looked at how

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plankton are affected in
microcosms and mesocosms, which

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are basically containers filled
with seawater.

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Craig Bettenhausen: Yes, I liked
in your story, you had this

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vocabulary where the mesocosms,
and started right off with that,

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I immediately, I was like, I
need to I'm in just so I can

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find out what that word means.

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Fionna Samuels: Yeah. So
mesocosm is basically like a

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giant test tube, like 1000s of
liters of water in a test in an

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enclosed container. And then the
microcosms are smaller volumes

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of water, so more on the liter
scale. And the nice thing about

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microcosms is that, because
they're so small, you can

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standardize a bunch of
experiments across the world,

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you can have a bunch of
different labs doing a very

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similar experiment with
different samples of water. So

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like you can go out and scoop
ocean water off the coast of

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Maine or off the coast of
Australia or off the coast of

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England, right? Like any of
these places

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Craig Bettenhausen: and the
mesocosms, these are in the

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water. But not the water can't
pass from one side of this

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mesocosm out into the general
correct

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Fionna Samuels: so the 1000
liter containers, the mesocosms,

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they are just containers in the
ocean. The researchers flood the

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container, collect all this
water and then make sure that if

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there are any fish or anything
else accidentally get caught up,

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to remove the fish. Because
that's too complex, they're

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really only interested in the
plankton, the bottom of the food

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web at this point. Historically,
the research so far has really

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only been interested at that
level. Future research, though,

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might look at some fish larva,
but yeah, and then that water is

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totally isolated from the
surrounding water, so anything

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that's added to the mesocosm is
contained within the mesocosm,

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and you don't worry about
putting anything into the

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surrounding open water system.

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Craig Bettenhausen: Yeah. I
wanted to ask about that because

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you encountered some critics,
some people that aren't happy

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about this. Were they worried
about the Loch Ness project

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specifically? Were they
skeptical about ocean alkalinity

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enhancement, or were they
against climate change

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mitigation as a whole effort?

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Fionna Samuels: Yeah, so I
think, I think you're talking

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about James Carey, one of the
sources in my story, yes, he was

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skeptical about Loch Ness
specifically, but also about

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ocean alkalinity enhancement,
more generally, Loch Ness, he's

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not totally convinced that they
will be able to measure all the

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things that they want to
measure, because it's just open

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water systems are incredibly
complex, and so measuring

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anything in the open ocean is
going to be very difficult. The

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Signal to Noise is very hard to
tease out. So he was skeptical

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about that. But more broadly, I
think he has concerns about

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scalability. And scalability is
a big question in all of these

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things, because we are emitting
so much carbon dioxide that it

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almost doesn't pay to do any of
this before seriously figuring

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out ways to cut emissions. The
scientists, of course, argue

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that we need to have a solid
research based foundation to

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even have discussions about
carbon dioxide removal on a

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grand scale. But others, of
course, worry that focusing on

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research for future
applications, sort of moves the

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goal post for the current needs
of just emission reductions.

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Yeah, I run

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Craig Bettenhausen: into that
debate a lot like I should be

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redoing this at all, and it's a
lot of the same dynamics of a

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lot of people think we will need
these carbon removal

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technologies a little bit down
the line. But yeah, there's

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lower hanging fruit that we
should be picking but it won't

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be ready then, if we don't start
working on it. Now, it's a

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difficult balance.

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Fionna Samuels: Yeah,
definitely. And again, all the

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researchers that I talked to
were not interested in selling

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carbon credits and they weren't
interested in trying to make

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this a commercial sort of
opportunity. They're really just

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wondering, Will this work, and
the models that climate

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scientists have run suggest that
ocean alkalinity enhancement and

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other carbon dioxide removal
techniques could be incredibly

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valuable, worthwhile pursuits in
the fight against climate

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change. But without doing these
experiments in the real world,

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in field trials, there's just a
big question mark about whether

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the real world is too
complicated for this to work.

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Craig Bettenhausen: I'm gonna
reveal my chemist background and

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say I'm curious about at the lab
scale, though. I mean, is there

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solid proof at the liter scale
that making the solution more

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basic will cause carbon dioxide
to dissolve into it? Do we have

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that basis? Really solid?

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Fionna Samuels: Yeah, they
figured that out. They are

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confident that carbon dioxide
will dissolve into water more

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readily if the water is more
basic, which is actually part of

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the reason why the oceans are so
powerful already. So the oceans

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are absorbing vast amounts of
carbon dioxide every year, and

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that's because their sort of
inherent pH is around 8.3 which

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is quite basic compared to other
bodies of water. In fact, tap

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water is often more acidic than
that, and sodium hydroxide is

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often used in municipal water
treatment plants in order to

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change the pH which helps
prevent corrosion from pipes. So

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you know, humans are already
doing pH modification on our

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drinking water and the ocean is
already super basic. It's just a

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question of whether or not we
can see these effects in the

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real world, because the ocean is
so huge.

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Craig Bettenhausen: Yeah. Are
there any other characters from

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your interviews that you wanted
to bring in but didn't quite

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Fionna Samuels: fit? That's a
good question. Yeah, the section

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that ended up not going into the
piece was really about how the

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researchers are communicating
with the public about their

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work, which was more of like a
social sciences kind of

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discussion. And those folks were
all great, and there are some

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really fabulous social science
research happening in this

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space, and really important
takeaways, like you need to talk

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to stakeholders before starting
your experiment, which seems

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really obvious, but sometimes
scientists are so excited to,

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you know, go out and start
collecting data that it might

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not occur to them that the
people living in these areas

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will feel very betrayed, almost,
if this kind of science happens

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without any of their input. And
so it's incredible. Incredibly

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important to have the local
communities involved in the

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whole scientific process from
even before applications for

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permits are submitted. And

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Craig Bettenhausen: so, I mean,
how was the community responding

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to the Loch Ness experiment? I
mean, they had your person that

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was opposed to it because they
didn't think it was going

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Fionna Samuels: to work, yeah.
So there have been some vocal

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opponents in the local
community, but it also seems

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like there was potentially less
I mean, there was some reporting

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that there are local community
members who are still not

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convinced that it's a good idea
to put stuff into the water. But

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there were also the Loch Ness
researchers did take lots of

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conversations into account and
change some of their

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experimental design based on
what the local fishing community

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said and other stakeholders
wanted from the experiment.

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Craig Bettenhausen: Yes, I guess
this is happening out of Cape

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Cod, and that is not an area
known for a lot of community

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activism. It's not a quiet sit
back and let everything happen

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to them, kind of a place, yeah,

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Fionna Samuels: the most
important thing with all of

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these environmental field trials
is to engage community members

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early and for the entire time
that you're doing the

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experiment, and do more than it
goes beyond just educating

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people. It actually requires
that they are involved in the

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decision making process. So Cape
Cod is not the

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Craig Bettenhausen: only place
that they're looking at this

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kind of thing. There are some
other experiments probing this

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idea of ocean alkalinity
enhancement.

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Fionna Samuels: Yeah. So the
other experiment that I talked

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about in the piece was really,
really small scale, tiny scale

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off the coast of Australia.
They're putting minerals down in

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the sediment in the water to
just see how worms and other

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creatures that live down there
will respond their results this

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really recent. It was our
winter, their summer, but they

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just recently finished that
project, and they told me that

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their results are promising. The
worms don't seem to care. But

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the scale at which they were
doing it is so small compared to

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what will need to happen. There

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Craig Bettenhausen: are scale
where they're like swimming down

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there with a single vial.
They're

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Fionna Samuels: swimming down
with a single vial, opening it

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up, pouring it and then watching
for a few weeks, taking samples

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every few weeks, and then taking
up sediment samples. Obviously,

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that's such a small scale that
that's not what any sort of real

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world application will look
like. We do actually have

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examples of real world mineral
applications. So there's a

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company called Vesta that has
done some olivine trials where

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they've put huge amounts of
crushed olivine sand along, I

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think it was the coast of New
Jersey, and off the coast as

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well, obviously, tons and tons
of crushed rock is a lot

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different than a tiny little bio
of crushed rock. And they're

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interested in figuring out some
kind of carbon credit, some way

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of making this technique
profitable. If there's any

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future in these sorts of
techniques, there should be

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small scale, very safe field
trials before actually

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approaching anything that looks
like what we would need to

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combat climate change in a real
way, which is unfortunate. It's

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like such a bummer, right? Like,
the best solution is for

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everyone to bike to work and go
from there,

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Craig Bettenhausen: stop eating
so much meat. Compost. Yeah, oh

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God.

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Fionna Samuels: There's this
carbon dioxide removal technique

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where you use electricity to
take carbon dioxide out of

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seawater and pretty much, and
then you put that carbon dioxide

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into the ground, you inject it
into some sort of geologic

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formation, pretty much everyone
thought that that was a very

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silly approach, because the
ocean is one of the most stable

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places for carbon dioxide to
Live. Carbon dioxide is

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sequestered into carbonate,
which is all of those sorts of

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ions that are in the ocean will
stay in the ocean as carbonate

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for 10,000 years. So it's silly
to take stable carbon dioxide

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out of the ocean to put
somewhere else, because the

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ocean is a really good home for
it. So

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Craig Bettenhausen: in June,
actually, I'm going to visit a

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pilot rig in New York City,
where a startup is testing a

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system like the enhanced ocean
alkalinity that you're

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describing. They're going to add
reactive alkaline minerals to

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remove CO two this time from the
East River in New York, instead

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of the ocean. What should I ask
them? What should I be looking

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for? What

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Fionna Samuels: you should ask
them, how they're measuring how

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much carbon dioxide is being
removed from the air, how

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they're measuring carbon dioxide
uptake. All

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Craig Bettenhausen: right, so is
there anything else to me

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00:19:25,100 --> 00:19:27,080
reporting that you wish you
could have fit in somehow?

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Fionna Samuels: The one thing
that I didn't emphasize, and I

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would like to have emphasized,
is that a big piece of all this

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research is what the researchers
called monitoring, reporting and

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verification, and that goes into
sort of figuring out if this is

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a usable technology for
something like carbon credits.

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And what that means is that you
need to be able to monitor how

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much carbon dioxide is removed.
You need to be able to report

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it, which is a whole different
sort of infrastructure that's

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separate from the science. And
then you need to verify it so

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other people need to be able to
come in. And measure the same

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thing that you measured. And a
lot of this research right now

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depends on modeling. There are
very few field trials, although

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it's a growing field so there
will likely be more field trials

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in the near future, but
monitoring carbon dioxide

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removal on a global scale is
going to be incredibly

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challenging, which is why these
sort of open field trials are so

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important, because if you can
monitor it on the small scale,

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and you can prove that you are
able to monitor how much carbon

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dioxide is removed on the small
scale, and then other people are

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able to verify that you are
measuring what you think you're

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measuring, then that basically
opens the door to realistic

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sorts of deployments in the
future.

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Craig Bettenhausen: Okay, well,
Fiona, thanks for diving deep on

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this with us.

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Fionna Samuels: Thanks for
having me. Thank you so much.

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Craig Bettenhausen: And I
usually use that line. It's not

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always literal, but this time it
was,

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00:20:49,190 --> 00:20:52,430
Fionna Samuels: I was gonna say,
that's a great pun you caught me

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00:20:52,430 --> 00:20:53,570
off guard with that one.

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Craig Bettenhausen: You can find
Fionna Samuels story about

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oceans as climate change allies
on CNN website, or in the April

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00:21:00,740 --> 00:21:04,340
14, 2025, print issue of CNN, we
put a link in the show notes

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along with the episode credits.
We'd love to know what you think

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00:21:06,320 --> 00:21:08,750
of CNN uncovered. You can share
your feedback with us by

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00:21:08,750 --> 00:21:13,040
emailing C E N feedback at ACS,
dot, O, R, G, you can find me on

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00:21:13,040 --> 00:21:15,530
social media as at Craig of
waffles, Fiona. How can

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00:21:15,530 --> 00:21:16,520
listeners get in touch with you?

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00:21:16,580 --> 00:21:18,950
Fionna Samuels: I'm at F
Morningstar on blue sky.

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00:21:19,160 --> 00:21:21,050
Craig Bettenhausen: All right,
this has been C&EN uncovered a

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00:21:21,050 --> 00:21:23,930
series from C&EN Stereo
Chemistry. Stereo Chemistry is

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00:21:23,930 --> 00:21:26,600
the official podcast of chemical
and Engineering News. Chemical

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00:21:26,600 --> 00:21:28,730
and Engineering News is an
independent news outlet

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00:21:28,730 --> 00:21:30,710
published by the American
Chemical Society. Thanks for

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00:21:30,710 --> 00:21:31,100
listening.

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