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Hey, thanks for listening. 
This is Ross Kenyon. 

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I'm the host of Reversing 
Climate Change, the podcast you 

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are listening to right at this 
very moment. 

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Before we get into the bulk of 
today's show, I'd love to tell 

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you about our sponsor, Philip 
Lee. 

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LLPI really like doing shows 
about the law. 

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I think the law is such a 
fascinating part of our shared 

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social life. 
It structures so much of it. 

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It's badly understood by most 
people. 

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And just structuring deals 
within carbon removal is hard. 

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I'm talking grown up deals here,
like when you're trying to put 

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together an enormous package, 
complicated structuring, a lot 

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of money, changing hands, The 
stakes are high. 

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You really do need a good 
lawyer. 

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I'm sorry to tell you that if 
you are a startup out there in 

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carbon removal, you're going to 
probably pay a fair amount of 

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money to lawyers. 
There's just no way around it. 

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Your choice is basically, do you
get a bad lawyer or a good 

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lawyer? 
One really cool thing I can say 

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on Philip Lee LLP's behalf, 
Well, one, Ryan Covington and I 

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did a very fun show about how 
basically no one except for an 

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elite few really know what 
bankability and project finance 

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even mean. 
And he lays it out very clearly.

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If you'd like to go listen to 
that show, it's awesome and it's

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LinkedIn the show notes. 
And also we end up talking about

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Ernest Hemingway of firm not 
too. 

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So it keeps with the tradition 
of reversing climate change. 

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One also really cool thing is 
that they just won Environmental

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Finances, VCM Law Firm of the 
Year. 

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They put it three years in a 
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It's the only award for legal 
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they have offices in the US, 
Europe, and the UK. 

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You should check out Philip Lee 
LLP. 

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Thank you from the bottom of my 
heart for listening to this, and

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thank you to our sponsors. 
You really make this so that 

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it's something that in a busy 
life with lots of competing 

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priorities, I'm able to keep 
coming back and making more, 

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reversing climate change. 
Thanks so much for what you do. 

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And now? 
Here is the show. 

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Hey, thanks for listening to 
Reversing Climate Change. 

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My name is Ross Kenyon. 
I'm the host of the show. 

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I'm a carbon removal 
entrepreneur, and I'm very happy

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to have an alumnus of the show 
back on. 

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Tyler Kukla is a research 
scientist at Carbon Plan, where 

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he's working on enhanced 
weathering, which if you're not 

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familiar with, is one of the 
main carbon removal pathways 

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which is being commercialized 
and researched right now. 

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I'm going to explain one 
paradigmatic version of it. 

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So much of carbon removal deals 
with putting alkalinity in 

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different places and 
configurations, but one of the 

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main ways of using enhanced 
weathering that is being 

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commercialized by companies 
right now is the laying down of 

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silicate rocks on croplands. 
That silicate rock captures 

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carbon dioxide from the 
atmosphere, and then it washes 

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through the hydrological cycle 
out to rivers, out to the ocean,

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and then it is stored in stable 
forms in the ocean. 

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There's another class of rocks 
called carbonates that can also 

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remove carbon dioxide from the 
atmosphere and store it, but 

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it's a little bit more confusing
because carbonate already has 

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carbon in the rock itself. 
Some of that will likely be 

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released in the application of 
it to soil. 

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It's currently being used for AG
line purposes right now for pH 

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management. 
So there's also a question of 

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additionality with regard to 
carbonates. 

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And for all those reasons and 
probably some others, but also 

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this next reason, carbonates 
have not been as thoroughly 

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investigated as silicates have 
for enhanced rock weathering. 

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And that reason is that in 1996,
there was an IPCC report which 

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made a conservative assumption 
about carbonate rock releasing 

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all of the carbon that is stored
in the carbonate back in the 

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atmosphere when it's applied to 
croplands for pH management. 

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What's so interesting about this
story that Tyler turned me on to

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is that when we don't have good 
information, it makes sense to 

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have a conservative estimate. 
And so the scientists working on

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the carbonate and AG line 
portion of this IPCC report, 

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they decided to make the 
conservative assumption that 

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100% of the carbon of the 
carbonate will be released back 

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into the atmosphere when 
applied. 

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That means that AG liming is 
likely and inherently emitted 

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process. 
And maybe it is at best carbon 

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neutral, but certainly would not
be carbon negative. 

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And what's interesting about 
this is that that is a 

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responsible decision that was 
made, gosh, how long ago? 

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30 years ago now. 
And that has led to effects that

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have shaped the commercial 
routes of carbon removal. 

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We have spent way more time on 
silicate rock for enhanced 

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weathering than we have for 
carbonates, at least partially 

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as a result of this conservative
assumption, which has been 

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challenged by science and is 
undergoing revision now. 

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And there's debates happening 
within certain communities 

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within carbon removal and in the
Academy. 

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And we'll see which way this all
pans out. 

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And if that sounds really nerdy 
to you, fine, I understand. 

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But I think what I want you to 
keep your eye on here is not 

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necessarily the state of the 
science of the silicate and 

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carbonate debate for feedstocks 
with an enhanced weathering. 

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That's of course interesting and
very important. 

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But what's more interesting to 
me is how one decision that 

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probably didn't feel super 
relevant at the time of the 1996

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IPCC report, I doubt the 
scientists working on this. 

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We're thinking that 30 years 
from now, this will potentially 

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distort the carbon removal 
marketplace and which types of 

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rock are eligible to be used as 
carbon removal and will lead 

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people towards silicate rock 
rather than carbonates. 

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It's just funny. 
It's not like there's silicate 

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scientists and business people 
on the grassy Knoll or anything 

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like that. 
Like these are good reasons that

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this is made for. 
And it's just one of those 

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things that history, causality, 
contingency, entropy, and how 

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that affects things over the 
course of decades are really 

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unpredictable. 
I doubt any of the people 

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working on this had an inkling 
of their responsible 

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conservative decision about how 
to estimate the carbon reversal 

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of AG liming would lead us down 
this path. 

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And that's what's so interesting
to me too. 

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It's not that anyone did 
anything wrong. 

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It's not even about weighing in 
on which rock is best in which 

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cases. 
It's just about how many 

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decisions do we make now will 
impact our future decisions, 

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which is especially important 
because so much of carbon 

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removal right now is early days.
And there is a desire to 

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regulate things and to have 
stable expectations of what is 

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acceptable and what is not. 
And we will almost certainly be 

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making rules that our 
descendants will look at be 

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like, wow, that really sent us 
down a wrong path. 

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That was incorrect. 
And it was really hard to change

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even once we knew it was 
incorrect or was not the whole 

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story. 
I think that's a thing that 

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should encourage us to try 
really hard to get things right 

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now, but also to have mercy for 
ourselves and for the people who

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came before us trying to do 
their best, and also knowing 

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that causality is an 
unpredictable thing. 

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Tyler and I dig into so many 
more details about this in 

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particular, and some of the 
philosophical historical 

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linkages here that endlessly 
fascinate me. 

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Thank you so much for listening.
If you want to open up your 

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podcast app and give the show 5 
stars may be ready to review on 

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your podcast out, that would be 
great. 

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But also I, I think I just want 
to start the show today. 

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So I'm not going to, I'm not 
going to stick my hand out 

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today. 
You get a free pass, $5 a month.

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You can be a paid subscriber. 
Blah blah blah if you. 

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Want to support the show? 
Go check out the show notes. 

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I think I'd rather just get you 
right into the heart of the 

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conversation with Tyler, so here
I go. 

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Here it is, Tyler. 
You were brave and you decided 

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to come back into the lion's den
where you're going to get 

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grilled by me about. 
Silicates for having us. 

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Yeah, I'm so happy to have you. 
I think this is one of those 

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things that's been percolating 
for a long time. 

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I've been hearing people talk 
about this issue for seemingly 

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years. 
It's maybe coming into the 

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mainstream of carbon removal 
more seriously now. 

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There's so much to talk about. 
I also don't even know how to 

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start this conversation because 
some parts of this are science 

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related, but this podcast is 
also about the downstream 

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effects of policy and like 
design decisions that impact how

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science and markets are built 
downstream from that. 

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Do you even agree with that 
framing? 

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Is that the correct way to 
understand this? 

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I think that makes sense to me. 
I, I would think about this 

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through kind of the lens of past
dependence, which is something 

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that we've talked about before. 
And I think that through that 

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lens, like if you want to talk 
about how do you get stuck doing

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one thing that maybe isn't the 
thing you want to be doing? 

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Like the first thing you need to
do is identify that you're 

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trying to get somewhere, right? 
You have a destination or a goal

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that you're trying to achieve. 
And it's hard to talk about the 

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path that you're on unless you 
have agreement around what that 

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goal is or where you're trying 
to go. 

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But once you do have that and 
you open up the conversation to 

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to think about like, where 
should we be going with this, 

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then you have to think about, 
well, how do we recognize that? 

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Like, the thing that we're doing
maybe isn't the thing that we 

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want to be doing or we are 
ignoring a parallel path that 

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could be really useful. 
And I think that's kind of 

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what's happening in the world of
enhanced rock weathering right 

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now. 
And that's what I think would be

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fun to dig into. 
Yeah. 

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What do you think when you think
about like past dependence and 

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carbon removal? 
So many things. 

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I'm, I'm almost flabbergasted 
that you asked me because so 

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many of the things that I think 
about relate to, is it better to

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have a rule here or no? 
And I think the default 

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assumption for a lot of people 
is like more regularized 

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assumptions and behaviors would 
be good. 

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But you also never get to see 
what are the things that you 

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designed out ex ante because you
forbid them before they had a 

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chance to be tried out. 
So whenever there are rules that

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are really strict, are we 
limiting the innovation space in

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ways that it might get us to a 
local optimum, but not the 

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global optimum? 
And the thing that's hard about 

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it is that it was probably 
entirely rational for many of 

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these path dependencies to exist
when they started. 

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But you don't necessarily know 
that you're in a cul-de-sac 

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until you're there. 
And then you're like, oh, crap. 

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Like that was like medium term, 
correct, but long term it was 

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incorrect. 
Now what? 

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And then you talking to me about
this like, wow, is enhanced 

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weathering in one of these two? 
And it's also so hard to talk 

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about this because so many 
people's livelihoods depend upon

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it, and therefore we need to be 
very careful unless we are 

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prepared to receive very annoyed
emails. 

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Tyler, are you really putting me
in this position right now? 

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I mean, I guess I also have that
to stake as well. 

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So it's it. 
Hopefully you're you. 

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Got carbon plans? 
So like your e-mail is already 

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full. 
Like you're fine. 

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Yeah, exactly. 
Don't. 

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Worry about it. 
I think one thing that gives me 

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hope is that like we are in the 
early stages of developing 

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enhanced rock weathering in 
particular and open system 

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carbon removal and carbon 
removal more broadly. 

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And it's not like the path is 
necessarily an emergent property

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as this like innumerable actors 
that are all playing the game 

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and like we nobody is really 
driving the ship and it's just 

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kind of going where these like 
forces that we have no control 

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over are dictating it. 
I think we do have a little bit 

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more control over where we 
explore, where we look and what 

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we're doing. 
And we can't really exercise 

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that control unless we're having
conversations like this about 

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where should things be going 
and, and how to do it. 

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You and I maybe don't have that 
control, but there are small 

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enough number of actors in the 
game right now that and it's 

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early enough on that I think 
that it's not too hard to solve 

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problems of like, Oh no, maybe 
we're a little bit stuck 

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somewhere that we don't want to 
be. 

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00:11:33,920 --> 00:11:37,520
Why do you think we get stuck 
specifically within enhanced 

229
00:11:37,640 --> 00:11:41,920
rock weathering? 
I, well, I don't think enhanced 

230
00:11:41,920 --> 00:11:43,200
rock weathering as a whole is 
stuck. 

231
00:11:43,200 --> 00:11:45,320
I think there's one specific 
piece of enhanced rock 

232
00:11:45,320 --> 00:11:48,120
weathering that like maybe we 
should be looking in a parallel 

233
00:11:48,120 --> 00:11:50,600
direction somewhere else. 
And the thing that makes me 

234
00:11:50,600 --> 00:11:54,640
think that is that anytime that 
I think you see a divergent 

235
00:11:54,640 --> 00:11:58,400
between like where investment is
going and what research says 

236
00:11:58,400 --> 00:12:02,640
might be promising, anytime that
divergent emerges, it's worth 

237
00:12:02,640 --> 00:12:05,120
thinking critically about 
whether or not that's justified,

238
00:12:05,360 --> 00:12:07,280
right? 
Do we want that gap to exist? 

239
00:12:07,280 --> 00:12:08,320
Does it make sense that it 
exists? 

240
00:12:08,320 --> 00:12:12,600
It's not inherently bad, but 
like it should set off alarm 

241
00:12:12,600 --> 00:12:13,840
bells. 
It should force us to think a 

242
00:12:13,840 --> 00:12:16,200
little bit more critically. 
And I think that that's what's 

243
00:12:16,200 --> 00:12:18,120
happening in enhanced rock 
weathering. 

244
00:12:18,120 --> 00:12:22,440
And what I mean by that is that 
we have built the entire field 

245
00:12:22,680 --> 00:12:25,360
around one kind of rock or one 
set of minerals. 

246
00:12:25,360 --> 00:12:28,480
And these are silicate minerals.
And we know that carbonates, 

247
00:12:28,480 --> 00:12:31,560
which is another kind of rock or
mineral set of minerals, can 

248
00:12:31,560 --> 00:12:34,680
also do carbon removal. 
And we have largely ignored 

249
00:12:34,680 --> 00:12:37,680
carbonates. 
And that's not what I think. 

250
00:12:37,680 --> 00:12:40,000
If you, it's not like we looked 
at the research, like a decades 

251
00:12:40,000 --> 00:12:42,720
of research and said, OK, well, 
silicates are the only way to go

252
00:12:42,720 --> 00:12:45,120
or even just like the optimal 
way to go. 

253
00:12:45,120 --> 00:12:46,880
That's not it. 
There isn't like a good 

254
00:12:46,880 --> 00:12:50,280
scientific justification for 
building and coalescing this 

255
00:12:50,280 --> 00:12:52,720
entire field of enhanced 
weathering around silicates and 

256
00:12:52,720 --> 00:12:55,320
largely ignoring carbonates. 
We know that these rocks have 

257
00:12:55,320 --> 00:12:56,560
their own strengths and 
weaknesses. 

258
00:12:56,560 --> 00:12:58,600
It's not like it. 
It's not that it doesn't matter 

259
00:12:58,600 --> 00:13:00,600
which one you choose. 
It definitely matters. 

260
00:13:01,200 --> 00:13:03,440
But we also know that there are 
examples in the literature of 

261
00:13:03,440 --> 00:13:06,360
each one of these types of rocks
winning out over the other. 

262
00:13:06,760 --> 00:13:09,560
And so I think there's a good 
case to be made that if we want 

263
00:13:09,560 --> 00:13:12,960
enhanced rock weathering to 
contribute the most that it can 

264
00:13:12,960 --> 00:13:16,240
to our our climate goals and our
carbon removal capacity, we need

265
00:13:16,240 --> 00:13:18,440
to be exploring both carbonates 
and silicates. 

266
00:13:19,160 --> 00:13:22,080
That's not the world that we 
live in right now, right? 

267
00:13:22,080 --> 00:13:24,600
I, what we don't want to end up 
in is a world where, you know, 

268
00:13:24,680 --> 00:13:27,160
we could be doing 1 unit of 
enhanced rock weathering for 

269
00:13:27,160 --> 00:13:29,480
carbon removal, but we're doing 
half because we kind of let this

270
00:13:29,480 --> 00:13:34,960
entire side of the field kind of
it, we, we ignored it And I, I 

271
00:13:34,960 --> 00:13:36,400
don't have a good answer as to 
why we're here. 

272
00:13:36,400 --> 00:13:38,520
I think there's a million 
reasons as to why the field has 

273
00:13:38,520 --> 00:13:41,400
built itself around silicates. 
I think a lot of it has to do 

274
00:13:41,400 --> 00:13:43,200
with one. 
That's where we started. 

275
00:13:43,520 --> 00:13:45,760
And there are a lot of positive 
feedbacks that emerge around the

276
00:13:45,760 --> 00:13:48,200
thing that you start with. 
And they are really complicated 

277
00:13:48,400 --> 00:13:52,480
and there's no simple answer. 
But I think that like the the 

278
00:13:52,640 --> 00:13:57,600
overarching theme that emerges 
for me that is maybe so vague to

279
00:13:57,600 --> 00:14:01,000
the point that it's not not 
useful is that silicates offer 

280
00:14:01,000 --> 00:14:03,600
this really easy and simple 
story. 

281
00:14:03,600 --> 00:14:06,000
And that story is the story that
we tell ourselves and enhanced 

282
00:14:06,000 --> 00:14:08,200
rock weathering. 
And there are a few elements of 

283
00:14:08,200 --> 00:14:10,200
that story that are particularly
good for silicates. 

284
00:14:10,200 --> 00:14:12,800
But the the big picture is that 
there is a really nice story, 

285
00:14:13,040 --> 00:14:16,480
and these easy early stories 
tend to stick for a whole bunch 

286
00:14:16,480 --> 00:14:18,800
of reasons. 
I'll tell the story, Tyler. 

287
00:14:21,000 --> 00:14:24,400
Well, I mean, I it's worth 
thinking about the narrative 

288
00:14:24,400 --> 00:14:26,200
itself, right? 
Anytime you have a really nice 

289
00:14:26,200 --> 00:14:29,840
story and you get little quick 
tag lines for podcasts and news 

290
00:14:29,840 --> 00:14:31,960
articles. 
But researchers also have an 

291
00:14:31,960 --> 00:14:33,880
easy job framing their research 
project. 

292
00:14:33,880 --> 00:14:36,080
And when the field is over here,
you want to ask research 

293
00:14:36,080 --> 00:14:38,400
questions around where the field
is going already. 

294
00:14:38,400 --> 00:14:40,840
And attention attracts 
attention. 

295
00:14:41,440 --> 00:14:44,080
So it's really easy to to kind 
of build stuff around that. 

296
00:14:44,080 --> 00:14:46,400
The first piece of like why 
carbonates, I think are a tough 

297
00:14:46,400 --> 00:14:50,440
story has to do with something 
that the Intergovernmental Panel

298
00:14:50,440 --> 00:14:54,240
on Climate Change, the IPCC 
wrote all the way back in 1996 

299
00:14:54,480 --> 00:14:56,880
when they weren't talking about 
carbon removal or enhanced rock 

300
00:14:56,880 --> 00:14:58,720
weathering at all. 
And it's a really. 

301
00:14:58,760 --> 00:15:00,560
My Tamaguchi. 
Back then, I wasn't. 

302
00:15:00,600 --> 00:15:02,960
Even. 
Yeah, I know. 

303
00:15:03,080 --> 00:15:04,800
And what even is it called? 
Tamagotchi. 

304
00:15:07,200 --> 00:15:08,680
Few. 
Few people were thinking about 

305
00:15:08,680 --> 00:15:10,200
Nan stock weathering at that 
time. 

306
00:15:11,120 --> 00:15:13,640
It's, it's, it's not the IPC's 
fault that they weren't thinking

307
00:15:13,640 --> 00:15:16,040
about it. 
But so the IPCC, they put out 

308
00:15:16,040 --> 00:15:19,880
this report every 10 years or 
so, which is is not frequent. 

309
00:15:19,880 --> 00:15:21,680
And we're coming up on the next 
round right now. 

310
00:15:21,680 --> 00:15:23,280
So this is going to be coming 
full circle. 

311
00:15:23,680 --> 00:15:26,840
The report is the National 
Greenhouse Gas Inventory Report,

312
00:15:26,840 --> 00:15:30,040
guidelines for how you calculate
as a country, how you calculate 

313
00:15:30,040 --> 00:15:31,680
emissions from your country, 
basically. 

314
00:15:32,040 --> 00:15:34,560
And one of the guidelines that 
they have in this very long, 

315
00:15:34,560 --> 00:15:37,880
very dense report has to do with
what happens when you spread 

316
00:15:37,880 --> 00:15:41,240
carbonate rocks on fields. 
Because the kind of kicker here,

317
00:15:41,240 --> 00:15:43,280
and one of the things that makes
carbonates and silicates 

318
00:15:43,280 --> 00:15:46,400
different in enhanced rock 
weathering is that we're already

319
00:15:46,400 --> 00:15:49,000
spreading carbonates on 
agricultural fields, not just in

320
00:15:49,000 --> 00:15:51,560
the US, but in a bunch of places
around the world. 

321
00:15:51,560 --> 00:15:53,520
And we're not doing that for 
carbon removal, even though 

322
00:15:53,520 --> 00:15:55,400
carbonates can be used for 
carbon removal. 

323
00:15:55,640 --> 00:15:58,320
We're doing it because there are
agronomic benefits, because it 

324
00:15:58,320 --> 00:16:01,440
neutralizes acidity in the soil.
The plants like that they can 

325
00:16:01,440 --> 00:16:03,920
release calcium and and plants 
need calcium. 

326
00:16:04,280 --> 00:16:07,160
So there are clear benefits to 
spreading carbonate on fields. 

327
00:16:07,480 --> 00:16:10,360
And IPCC says, well, we want to 
make sure that we're accounting 

328
00:16:10,360 --> 00:16:13,440
for any emissions that are 
associated with this, not just 

329
00:16:13,440 --> 00:16:16,120
the trucking emissions, which is
dealt with elsewhere like the 

330
00:16:16,120 --> 00:16:21,000
shipping emissions, but also 
like if the carbon in it, 

331
00:16:21,160 --> 00:16:23,360
carbonates have carbon in them. 
And we'll get more to this in a 

332
00:16:23,360 --> 00:16:25,000
moment it. 
Better, but it better have it in

333
00:16:25,000 --> 00:16:26,200
there they. 
Better have carbon in them 

334
00:16:26,200 --> 00:16:31,480
because the name, the name that 
says so if the carbon in that 

335
00:16:31,480 --> 00:16:33,760
rock is released to the 
atmosphere, we want to make sure

336
00:16:33,760 --> 00:16:37,560
that we're accounting for that. 
And the ITCC in 1996 in the 

337
00:16:37,760 --> 00:16:42,080
their greenhouse gas inventory 
guidelines said, look, without 

338
00:16:42,080 --> 00:16:44,840
any better information about 
what's going on, the safest 

339
00:16:44,840 --> 00:16:48,360
assumption is just that all of 
the carbon in this rock is going

340
00:16:48,360 --> 00:16:52,240
into the atmosphere. 
Just just go with that in 2008. 

341
00:16:52,240 --> 00:16:53,920
So that sparked a bunch of Geo 
chemistry. 

342
00:16:53,920 --> 00:16:55,480
Like this isn't really how it 
works. 

343
00:16:55,480 --> 00:16:58,040
Like we know that a lot of the 
carbon that's in the rock can be

344
00:16:58,040 --> 00:17:00,880
stored in the water durably 
along with carbon from the 

345
00:17:00,880 --> 00:17:04,079
atmosphere, which is how 
carbonates do carbon dioxide 

346
00:17:04,079 --> 00:17:05,760
removal. 
They store their own carbon, but

347
00:17:05,760 --> 00:17:08,200
also atmosphere carbon when they
dissolve. 

348
00:17:08,839 --> 00:17:12,680
And they, a handful of papers 
came out looking at what is the 

349
00:17:12,720 --> 00:17:15,880
carbon effect of adding 
carbonate to fields even when 

350
00:17:15,880 --> 00:17:17,359
we're not trying to do carbon 
removal. 

351
00:17:17,640 --> 00:17:20,400
Some papers found that you get 
carbon removal, which is great. 

352
00:17:20,680 --> 00:17:23,480
Other papers found that like if 
we want to update an emissions 

353
00:17:23,480 --> 00:17:25,680
factor and we're being kind of 
conservative about what's 

354
00:17:25,680 --> 00:17:28,400
happening with the balance of 
carbon into the system and 

355
00:17:28,400 --> 00:17:33,760
carbon out of the system, that 
it's easy to with an error like 

356
00:17:33,760 --> 00:17:36,160
land and that carbonates are 
emitting carbon to the 

357
00:17:36,160 --> 00:17:38,240
atmosphere. 
So one of the papers that came 

358
00:17:38,240 --> 00:17:42,120
out updated the emissions factor
for the United States to about 

359
00:17:42,120 --> 00:17:44,920
half of the carbon gets emitted 
to the atmosphere rather than 

360
00:17:44,920 --> 00:17:47,800
all of it. 
And this is the one the United 

361
00:17:47,800 --> 00:17:49,640
States has mostly used since 
then. 

362
00:17:50,080 --> 00:17:55,400
But what this also means in that
paper is Weston McBride 2005. 

363
00:17:55,400 --> 00:17:59,520
For any mega nerds out there, 
what this also means is that 

364
00:17:59,560 --> 00:18:02,520
when we started thinking about 
enhanced silicate weathering, we

365
00:18:02,520 --> 00:18:05,000
have this like really nice win 
win narrative that we're 

366
00:18:05,000 --> 00:18:06,920
presented with. 
Which is on the one hand, if you

367
00:18:06,920 --> 00:18:09,280
spread silicates on the street, 
on the field, you can get carbon

368
00:18:09,280 --> 00:18:11,640
removal and that's a win. 
And on the other hand, if you 

369
00:18:11,640 --> 00:18:14,360
stop spreading carbonate in 
order to spread the silicate, 

370
00:18:14,400 --> 00:18:16,840
then you avoid all of the 
emissions that are associated 

371
00:18:16,840 --> 00:18:20,320
with the carbonate that the IPCC
and Weston Mcride and a handful 

372
00:18:20,320 --> 00:18:23,680
of other papers have said exist.
The complication to that 

373
00:18:23,680 --> 00:18:25,960
narrative is that other papers 
will say, no, we have good 

374
00:18:25,960 --> 00:18:28,720
evidence that spreading 
carbonates on Shields is 

375
00:18:28,720 --> 00:18:31,720
actually doing carbon removal. 
It's not emitting carbon to the 

376
00:18:31,720 --> 00:18:33,960
atmosphere. 
And so it's the story isn't that

377
00:18:33,960 --> 00:18:37,000
simple. 
But early on in the world of 

378
00:18:37,080 --> 00:18:39,800
enhanced silicate weathering, it
was easy to say, look, if we 

379
00:18:39,800 --> 00:18:42,880
stop spreading carbonates, we 
avoid those emissions and that's

380
00:18:42,880 --> 00:18:45,720
good. 
So the IPCC kind of unwittingly 

381
00:18:45,720 --> 00:18:49,800
played a really big role in in 
the early narrative of enhanced 

382
00:18:49,800 --> 00:18:52,600
silicate weathering. 
And we're getting over that now.

383
00:18:52,600 --> 00:18:55,160
Like, I think as a field, we 
understand pretty broadly that 

384
00:18:55,280 --> 00:18:57,960
it's more complicated than that.
And the bread crumbs have been 

385
00:18:57,960 --> 00:19:01,640
there all along, but what gets 
picked up early often tends to 

386
00:19:01,640 --> 00:19:03,440
stick. 
So that's the first prong of 

387
00:19:03,640 --> 00:19:07,080
maybe one of the reasons why 
carbonates aren't getting the 

388
00:19:07,080 --> 00:19:08,960
attention that silicates have 
been getting an enhanced 

389
00:19:08,960 --> 00:19:12,480
weathering. 
That's so fascinating. 

390
00:19:12,800 --> 00:19:16,000
It's one of those things that 
was rational at the time. 

391
00:19:16,080 --> 00:19:18,880
If you don't have great 
information and you assume the 

392
00:19:18,880 --> 00:19:21,840
most conservative case, we would
typically say that's an example 

393
00:19:21,840 --> 00:19:24,960
of responsible behavior. 
So we can just infer from that 

394
00:19:24,960 --> 00:19:28,000
that these people are behaving 
responsibly and conservatively 

395
00:19:28,000 --> 00:19:32,920
in appropriate ways. 
But it also seemingly delayed 

396
00:19:33,280 --> 00:19:37,040
carbon removal research into 
carbonates and favored silicates

397
00:19:37,320 --> 00:19:41,600
in a way that may not have taken
place where this one note in a 

398
00:19:41,600 --> 00:19:46,400
96 IPCC report. 
If that didn't exist, we might 

399
00:19:46,400 --> 00:19:49,600
have a more balanced picture of 
enhanced weathering with mineral

400
00:19:49,600 --> 00:19:50,800
types. 
Do you agree with that? 

401
00:19:51,600 --> 00:19:53,880
I think that's fair to say. 
I think that like it, it's not 

402
00:19:53,880 --> 00:19:57,440
like a scientifically rigorous 
reason why we're not doing 

403
00:19:57,440 --> 00:19:59,480
carbonates, but the narrative is
really there and it's 

404
00:19:59,480 --> 00:20:01,360
compelling. 
And it's easy to tell that 

405
00:20:01,360 --> 00:20:03,400
story. 
And there have been papers all 

406
00:20:03,400 --> 00:20:05,000
along. 
Like it's not a mystery to us 

407
00:20:05,000 --> 00:20:07,840
that carbonates can do carbon 
removal, especially on human 

408
00:20:07,840 --> 00:20:10,520
timescales like hundreds to 
thousands of years. 

409
00:20:12,560 --> 00:20:14,720
But there, there was this little
tricky piece. 

410
00:20:14,920 --> 00:20:17,280
One thing I want to add is that 
the IPCC updated their 

411
00:20:17,280 --> 00:20:21,080
methodology in 2006 to say, 
look, we're going to add these 

412
00:20:21,080 --> 00:20:23,920
extra tiers so that you can 
choose different numbers for how

413
00:20:23,920 --> 00:20:26,360
much line their carbonate is 
emitting carbon. 

414
00:20:27,280 --> 00:20:29,480
If you have better information 
and you can get better 

415
00:20:29,480 --> 00:20:32,600
information by better data. 
And so the Weston McBride paper 

416
00:20:32,600 --> 00:20:35,880
I talked about, that's what's 
used in the US, that's the 

417
00:20:35,880 --> 00:20:39,080
better data that we use for the 
kind of slightly more 

418
00:20:39,080 --> 00:20:41,840
sophisticated methodology. 
And the most sophisticated, I 

419
00:20:41,840 --> 00:20:44,800
don't know if anybody uses this,
is to run like a complicated 

420
00:20:44,800 --> 00:20:47,040
model and figure out what is the
fate of the carbon in the 

421
00:20:47,040 --> 00:20:49,080
system. 
But one thing that we've gotten 

422
00:20:49,080 --> 00:20:52,600
stuck on, and then this is a bit
of an aside, but for the mega 

423
00:20:52,600 --> 00:20:55,360
nerds out there, is that there 
are system boundary questions 

424
00:20:55,360 --> 00:20:58,480
wrapped up in all of this too. 
So the IPCC, when they're 

425
00:20:58,480 --> 00:21:00,680
talking about what happens to 
the carbon in the carbonate, 

426
00:21:01,000 --> 00:21:04,040
their system boundary is defined
to be just around. 

427
00:21:04,040 --> 00:21:05,640
They were drawing a box around 
the rock. 

428
00:21:05,800 --> 00:21:08,680
That's all that they care about.
So they are not tracking what 

429
00:21:08,680 --> 00:21:11,800
happens to the carbon in the 
atmosphere, at least not in the 

430
00:21:11,800 --> 00:21:14,920
methodology that talks about how
to handle spreading carbonates 

431
00:21:14,920 --> 00:21:17,640
on fields. 
So even if you did account for 

432
00:21:17,640 --> 00:21:21,120
it, they would say that the the 
best you could ever do is 0 

433
00:21:21,120 --> 00:21:22,600
emissions. 
You could never do carbon 

434
00:21:22,600 --> 00:21:25,200
removal with this specific 
methodology. 

435
00:21:25,800 --> 00:21:28,160
You can account for the carbon 
removal somewhere else in their 

436
00:21:28,160 --> 00:21:30,880
methodologies, but it's not 
where we're talking about 

437
00:21:30,880 --> 00:21:32,680
spreading rocks on fields 
essentially. 

438
00:21:33,400 --> 00:21:36,200
So this wasn't, I don't think 
the Super well. 

439
00:21:36,840 --> 00:21:40,600
I think the authors that kind of
tried to amend the early 96 

440
00:21:40,600 --> 00:21:45,040
statement by the IPCC understood
this more or less, but wanted to

441
00:21:45,040 --> 00:21:47,120
write a fuller picture. 
And so all of these papers that 

442
00:21:47,120 --> 00:21:49,920
followed looked at the full 
system and looked at the carbon 

443
00:21:50,160 --> 00:21:52,520
coming out of the atmosphere as 
well as the carbon in the rock. 

444
00:21:53,280 --> 00:21:55,760
But the IPCC itself, for the 
purpose of that methodology, 

445
00:21:55,760 --> 00:21:57,080
they only care about what's in 
the rock. 

446
00:21:57,080 --> 00:22:00,440
So it's either going to be 
emitting or at best no emissions

447
00:22:00,440 --> 00:22:05,440
and never removal under that 
specific rule, which is a tricky

448
00:22:05,440 --> 00:22:08,200
piece. 
It seems that way to me too. 

449
00:22:08,200 --> 00:22:10,320
As a non scientist I look at 
something like that and 

450
00:22:10,320 --> 00:22:15,400
obviously any sort of system 
boundary question is contested 

451
00:22:15,400 --> 00:22:19,760
because if you were extremely 
holistic, the entire planet is 

452
00:22:19,760 --> 00:22:22,160
part of the same system and you 
should include all of this. 

453
00:22:22,160 --> 00:22:24,120
But like that makes science 
probably impossible. 

454
00:22:24,120 --> 00:22:26,400
Like you need to, you need to 
truncate and you need to 

455
00:22:26,400 --> 00:22:28,160
simplify to like make models 
work. 

456
00:22:28,360 --> 00:22:30,600
Otherwise it would be the map in
the territory would be the same 

457
00:22:30,600 --> 00:22:32,000
thing. 
And then what's even the point 

458
00:22:32,000 --> 00:22:34,040
of having one? 
I don't know. 

459
00:22:34,280 --> 00:22:36,680
This is by open system. 
Carbon removal is so hard 

460
00:22:36,680 --> 00:22:39,560
because we're doing things out 
in a world where we can't put 

461
00:22:39,560 --> 00:22:41,640
our finger on the carbon that 
we're removing, and we need to 

462
00:22:42,040 --> 00:22:45,040
have some understanding of what 
happens to the carbon that we 

463
00:22:45,040 --> 00:22:47,120
just send into the broader earth
system. 

464
00:22:47,480 --> 00:22:49,080
And it's very hard to draw those
boundaries. 

465
00:22:49,080 --> 00:22:52,400
And we frankly don't have the 
models yet that are like really,

466
00:22:52,400 --> 00:22:54,800
really good that we feel very 
confident about that can trace 

467
00:22:54,800 --> 00:22:57,160
those carbon flows super 
reliably. 

468
00:22:57,160 --> 00:22:59,760
They're being developed and we 
need more data, and the data is 

469
00:22:59,760 --> 00:23:03,320
being developed as well. 
But this is like one of the 

470
00:23:03,320 --> 00:23:05,400
fundamental challenges with open
system carbon removal. 

471
00:23:05,560 --> 00:23:07,800
Where do you draw the system 
boundaries, and then how do you 

472
00:23:07,800 --> 00:23:09,920
simulate them and account for 
them and understand what's 

473
00:23:09,920 --> 00:23:11,720
happening in places that you 
can't actually make the 

474
00:23:11,720 --> 00:23:17,360
measurements in the first place?
Well look I am very smart so why

475
00:23:17,400 --> 00:23:20,440
would you just draw the boundary
around the rock itself? 

476
00:23:20,440 --> 00:23:23,960
Obviously the atmospheric 
relationship is very important 

477
00:23:23,960 --> 00:23:25,880
for understanding. 
Like does this actually exist or

478
00:23:25,880 --> 00:23:27,040
not? 
Because it changes the net 

479
00:23:27,040 --> 00:23:29,280
carbon removals that can be 
accounted for and would change 

480
00:23:29,480 --> 00:23:33,080
the math of seemingly everything
downstream of it in a very 

481
00:23:33,080 --> 00:23:35,600
radical way. 
Teach me as a non scientist? 

482
00:23:35,600 --> 00:23:38,720
Like why would you choose to 
define it so narrowly? 

483
00:23:39,680 --> 00:23:42,040
I don't think that you would. 
In the world of carbon removal, 

484
00:23:42,040 --> 00:23:44,240
you wouldn't. 
I don't think it makes sense. 

485
00:23:44,240 --> 00:23:47,920
The IPCC report in their 
Greenhouse Gas guy inventory 

486
00:23:47,920 --> 00:23:51,080
guidelines, It makes sense only 
because they're trying to 

487
00:23:51,120 --> 00:23:54,440
discretize the problem to make 
it easy to do in small chunks. 

488
00:23:54,440 --> 00:23:57,440
So they has the effect of 
spreading carbonate unfilled in 

489
00:23:57,440 --> 00:24:01,080
one place and then the effect of
interactions between the soil 

490
00:24:01,080 --> 00:24:02,840
and the atmosphere coming 
somewhere else. 

491
00:24:03,200 --> 00:24:05,120
And so they're saying, look, 
don't worry, you can account for

492
00:24:05,120 --> 00:24:06,960
it. 
But like maybe the person that's

493
00:24:06,960 --> 00:24:09,800
doing the inventory about 
spreading rocks on fields is not

494
00:24:09,800 --> 00:24:12,240
the same person doing the 
inventory about what's happening

495
00:24:12,240 --> 00:24:16,160
at that interface elsewhere. 
It's just somewhere else in this

496
00:24:16,160 --> 00:24:18,640
very dense volume of all of the 
different ways that you might 

497
00:24:19,000 --> 00:24:22,920
calculate your emissions. 
So it does exist, but at a 

498
00:24:22,920 --> 00:24:26,120
certain point, they just needed 
to discretize stuff to ideally 

499
00:24:26,120 --> 00:24:29,560
make these chunks simple. 
And that's what happened. 

500
00:24:29,800 --> 00:24:31,240
I don't know if it was the right
call or not. 

501
00:24:31,280 --> 00:24:35,280
It's hard to say, but as we're 
thinking about what I can say is

502
00:24:35,280 --> 00:24:38,840
that in this next round of 
updates to the greenhouse gas 

503
00:24:38,840 --> 00:24:43,400
inventories with ITC, CS, TFI or
task force on, on inventories, 

504
00:24:44,920 --> 00:24:47,600
they're thinking about adding 
carbon removal methods to these 

505
00:24:47,600 --> 00:24:51,040
methodologies and asking, well, 
what would, what rules would we 

506
00:24:51,040 --> 00:24:55,840
need in order to figure out like
national scale removal estimates

507
00:24:55,840 --> 00:25:00,680
from different in different, 
including open system carbon 

508
00:25:00,680 --> 00:25:03,880
removal approaches. 
And in that world, if, if 

509
00:25:03,880 --> 00:25:06,480
enhanced rock weathering is 
built into the, the next round, 

510
00:25:07,120 --> 00:25:10,840
we're talking about doing it in 
that other box, not in the box 

511
00:25:10,840 --> 00:25:13,160
about spreading rocks on fields,
but that other box that I've 

512
00:25:13,160 --> 00:25:16,160
been hinting at. 
So it, it, it has to live 

513
00:25:16,160 --> 00:25:18,800
somewhere. 
And the conversation right now 

514
00:25:18,800 --> 00:25:20,800
is to put it there, but it's 
really hard. 

515
00:25:20,800 --> 00:25:22,880
It's like. 
Yeah, I'm trying to think of 

516
00:25:22,880 --> 00:25:25,440
what the alternative is because 
even the way that I framed it 

517
00:25:25,440 --> 00:25:27,560
makes it sound like, well, 
obviously you wouldn't want to 

518
00:25:27,560 --> 00:25:31,160
discretize this and make it 
discreet in this like nice 

519
00:25:31,160 --> 00:25:33,440
little box way because that's 
not the whole story or you're 

520
00:25:33,440 --> 00:25:35,600
missing things that should 
actually be in relation to one 

521
00:25:35,600 --> 00:25:38,000
another. 
But I think if you didn't do 

522
00:25:38,000 --> 00:25:40,800
that, I imagine there's 
pathologies the other directions

523
00:25:40,800 --> 00:25:45,200
to where because you do not 
discretize, you have some larger

524
00:25:45,200 --> 00:25:48,280
amorphous system where the 
causality is confused and maybe 

525
00:25:48,280 --> 00:25:50,840
it's harder to do productive 
climate science in some other 

526
00:25:50,840 --> 00:25:52,440
way. 
Surely there are good reasons. 

527
00:25:52,440 --> 00:25:55,120
It's not just, you know, very 
well educated people who are 

528
00:25:55,120 --> 00:25:59,160
passionate about this subject 
are corrupt or foolish in some 

529
00:25:59,160 --> 00:26:00,840
way. 
Like, is there some other 

530
00:26:00,960 --> 00:26:03,760
corollary to this on the other 
side of go too far and then it's

531
00:26:03,760 --> 00:26:05,600
impossible to do good science or
something like that? 

532
00:26:06,360 --> 00:26:09,160
You can go too far in the 
direction of of just taking on 

533
00:26:09,160 --> 00:26:10,560
the whole system rather than 
discussing. 

534
00:26:10,560 --> 00:26:11,960
Is that the? 
Alternative to making things 

535
00:26:11,960 --> 00:26:14,160
more discreet is that you would 
have to have a much more 

536
00:26:14,160 --> 00:26:16,360
holistic model, but then that 
would make it, you know, much 

537
00:26:16,360 --> 00:26:19,520
more difficult to write a report
or to make sure that all of the 

538
00:26:19,520 --> 00:26:23,400
various bureaucratic levels of 
this report composition sign off

539
00:26:23,400 --> 00:26:25,480
it in the right ways. 
Do we just not understand the 

540
00:26:25,480 --> 00:26:28,560
relationship between all these 
discrete parts and that's why 

541
00:26:28,560 --> 00:26:31,080
it's not written in that way? 
Like why isn't the science done 

542
00:26:31,080 --> 00:26:34,440
in that way? 
The science of the IPCC or the 

543
00:26:34,440 --> 00:26:36,240
science of enhanced rock 
weathering? 

544
00:26:36,720 --> 00:26:38,600
I, I think both of those layers 
are important. 

545
00:26:38,800 --> 00:26:42,160
I think the the IPCC is just 
like I've edited books and 

546
00:26:42,160 --> 00:26:44,440
anything where you have or made 
documentaries, anything when you

547
00:26:44,440 --> 00:26:48,320
have lots of stakeholders, 
everyone's got opinions on how 

548
00:26:48,320 --> 00:26:51,440
it should be and they often 
times will call each other names

549
00:26:51,440 --> 00:26:54,880
and it gets really nasty. 
I imagine being the stakeholder 

550
00:26:54,880 --> 00:27:00,240
manager of any IPCC report or 
any sufficiently numerous 

551
00:27:00,240 --> 00:27:03,960
co-author situations it gives 
you know, makes people go bald 

552
00:27:03,960 --> 00:27:06,400
probably. 
It sounds really, really hard. 

553
00:27:06,400 --> 00:27:07,520
I've been there. 
It's not fun. 

554
00:27:08,480 --> 00:27:10,960
So I imagine, like part of that 
is bureaucratic, political, 

555
00:27:10,960 --> 00:27:14,400
diplomatic, and I imagine like 
the enhanced weathering, part of

556
00:27:14,400 --> 00:27:18,160
this faces its own challenges 
between commercial interests and

557
00:27:18,160 --> 00:27:21,120
doing science on a time scale 
that's appropriate for companies

558
00:27:21,120 --> 00:27:22,280
that are funding this, that are 
for profit. 

559
00:27:22,960 --> 00:27:24,520
Basically any of these 
approaches probably have their 

560
00:27:24,520 --> 00:27:26,560
own pathologies that are 
inherent to them. 

561
00:27:27,040 --> 00:27:31,080
And I'm just wondering of the 
IPCC specifically, why do it in 

562
00:27:31,080 --> 00:27:35,160
this way that prioritizes what 
can be made discrete rather than

563
00:27:35,160 --> 00:27:38,160
something that is maybe truer 
and more holistic but was not 

564
00:27:38,160 --> 00:27:41,120
chosen? 
I don't know. 

565
00:27:42,640 --> 00:27:44,520
I wish I had. 
Miles, you're on a podcast. 

566
00:27:44,520 --> 00:27:48,680
Tyler, this is what we do. 
I mean, I, I, I kind of think it

567
00:27:48,680 --> 00:27:50,280
doesn't matter too much, to be 
honest. 

568
00:27:50,280 --> 00:27:53,440
I think that like it, the IPCC 
decision to draw the brat 

569
00:27:53,440 --> 00:27:54,920
boundaries where they did is one
thing. 

570
00:27:54,920 --> 00:27:56,600
And, and it's been 
misunderstood, frankly. 

571
00:27:56,600 --> 00:27:58,680
Like the the papers that have 
come out that tried to correct 

572
00:27:58,680 --> 00:28:01,720
the original statement include a
different set of boundaries. 

573
00:28:01,720 --> 00:28:06,480
And one of them like 
coincidentally ignores the quote

574
00:28:06,480 --> 00:28:08,600
UN quote ignores the carbon 
dioxide in the atmosphere 

575
00:28:08,600 --> 00:28:10,840
because they assume that all the
carbon dioxide that's taken up 

576
00:28:10,840 --> 00:28:13,920
is eventually re emitted. 
So it cancels out or whatever. 

577
00:28:14,160 --> 00:28:16,880
So by accident, they land in the
same exact boundary that the 

578
00:28:16,880 --> 00:28:19,480
IPCC wrote, but it's completely 
by accident. 

579
00:28:20,200 --> 00:28:24,200
So it's, you know, the boundary 
that they drew matters for the 

580
00:28:24,200 --> 00:28:26,720
purpose of like somebody 
deciding how much carbonate 

581
00:28:27,000 --> 00:28:29,840
emits carbon in their country 
that year. 

582
00:28:30,320 --> 00:28:34,720
It I don't think it matters for 
the purpose of like either way, 

583
00:28:35,200 --> 00:28:37,120
however they drew their 
boundary, I think they still 

584
00:28:37,120 --> 00:28:40,320
would have landed in a world 
where you have to account for 

585
00:28:40,320 --> 00:28:42,400
emissions of spreading carbonate
on fields. 

586
00:28:42,400 --> 00:28:45,080
And they probably they were 
thinking about emissions at the 

587
00:28:45,080 --> 00:28:46,760
time, not removals. 
So they probably would have 

588
00:28:46,760 --> 00:28:49,560
conservatively landed in a world
where there are where carbonate 

589
00:28:49,560 --> 00:28:52,520
is an emitting process. 
And that is that's the piece 

590
00:28:52,720 --> 00:28:55,840
that gave everyone talking about
enhanced silicate weathering the

591
00:28:55,840 --> 00:28:59,760
ability to say, look, if we stop
spreading carbonate, we'll avoid

592
00:28:59,760 --> 00:29:01,400
those emissions that are really 
pesky. 

593
00:29:02,200 --> 00:29:05,640
So I think that that that 
element is the, the, the tricky 

594
00:29:05,640 --> 00:29:07,920
piece, the fact that they're 
writing in emissions inventory 

595
00:29:07,920 --> 00:29:11,920
is kind of the the nature of why
we're in this world. 

596
00:29:13,640 --> 00:29:15,960
Back to the the narrative 
question here. 

597
00:29:16,240 --> 00:29:19,760
I had thought you were going to 
go for, I don't know, like if 

598
00:29:19,760 --> 00:29:22,400
you were in biomass sinking, you
would point to the Azola event 

599
00:29:22,400 --> 00:29:24,880
and be like, isn't that cool? 
Like that's what we're doing, 

600
00:29:24,880 --> 00:29:27,760
but smaller. 
And if you're involved in 

601
00:29:27,760 --> 00:29:30,840
silicate weathering, you would 
go to the Deccan traps or the 

602
00:29:30,840 --> 00:29:33,960
Siberian Traps and be like, 
look, this can change the entire

603
00:29:33,960 --> 00:29:36,360
climate of the planet in the 
largest way possible. 

604
00:29:36,880 --> 00:29:39,040
That's so cool. 
And if I was doing something 

605
00:29:39,040 --> 00:29:41,400
with cyanobacteria, I would be 
making the same case the other 

606
00:29:41,400 --> 00:29:43,160
direction. 
Like, you know, like those like 

607
00:29:43,160 --> 00:29:45,880
major, like biogeochemical 
things that happen. 

608
00:29:45,880 --> 00:29:49,200
Like, it's cool to be able to 
point to things that made eras 

609
00:29:49,200 --> 00:29:52,480
and epochs like, happen. 
So I thought you were going to 

610
00:29:52,480 --> 00:29:55,600
be talking about that. 
So apparently that's just for 

611
00:29:55,600 --> 00:29:58,520
people who like geological deep 
history stuff. 

612
00:29:59,600 --> 00:30:01,160
But it's not, it's definitely 
not. 

613
00:30:01,160 --> 00:30:02,960
Yeah, it's not just for those 
people. 

614
00:30:03,000 --> 00:30:03,680
I. 
Don't even know. 

615
00:30:04,320 --> 00:30:09,040
I, well, a couple of years ago 
at Carbon Plan, we put out an 

616
00:30:09,040 --> 00:30:11,720
article that the title is does 
enhanced rock weathering work? 

617
00:30:11,720 --> 00:30:14,400
Does enhanced weathering work? 
And the question that we were 

618
00:30:14,400 --> 00:30:16,120
asking is like, look, there's 
still a lot of science that 

619
00:30:16,120 --> 00:30:17,640
needs to be done. 
Do we have an answer to this 

620
00:30:17,640 --> 00:30:20,600
question of does it work or not?
And the response that we got 

621
00:30:20,880 --> 00:30:23,720
from a few folks was we know 
that it works. 

622
00:30:23,720 --> 00:30:27,080
It obviously works because 
enhanced weathering is the thing

623
00:30:27,080 --> 00:30:29,840
that has kept our planet 
habitable for billions of years 

624
00:30:29,840 --> 00:30:31,880
of time, not quote UN quote 
enhanced. 

625
00:30:31,880 --> 00:30:35,080
What I mean by that is that over
the course of geologic time 

626
00:30:35,080 --> 00:30:37,640
scales, when too many greenhouse
gases build up in the 

627
00:30:37,640 --> 00:30:41,400
atmosphere, the weathering of 
silicate rocks picks up and that

628
00:30:41,400 --> 00:30:44,320
scrubs that excess greenhouse 
gases out of the atmosphere. 

629
00:30:44,560 --> 00:30:48,040
And over the course of, you 
know, millions and billions of 

630
00:30:48,040 --> 00:30:50,560
years, This is why we still have
liquid water on our planet for 

631
00:30:50,560 --> 00:30:52,000
all of this time. 
We haven't boiled away the 

632
00:30:52,000 --> 00:30:54,000
oceans. 
And it's not like Venus where 

633
00:30:54,000 --> 00:30:56,960
you can melt lead on the surface
of the planet like we we live in

634
00:30:56,960 --> 00:31:00,560
a different world because this 
negative feedback exists that 

635
00:31:00,560 --> 00:31:03,960
prevents the over accumulation 
of greenhouse gases in the 

636
00:31:03,960 --> 00:31:05,920
atmosphere on very long time 
scales. 

637
00:31:06,400 --> 00:31:08,840
The thing is that that takes 
place on time scales of like 10s

638
00:31:08,840 --> 00:31:10,240
to hundreds of thousands of 
years. 

639
00:31:10,840 --> 00:31:15,640
And on those long time scales if
you weather like carbonate rock 

640
00:31:15,640 --> 00:31:18,960
for example, the carbonate that 
you weather ends up re 

641
00:31:18,960 --> 00:31:22,600
precipitating or reforming in 
the ocean where it locks up that

642
00:31:22,600 --> 00:31:26,520
carbon that you weathered on 
land permanently. 

643
00:31:26,520 --> 00:31:30,040
And so on long time scales, the 
effect is 0 of weathering 

644
00:31:30,040 --> 00:31:31,960
carbonate rock on carbon 
dioxide. 

645
00:31:32,560 --> 00:31:36,160
And the effect of silicate rock 
is not zero because silicates 

646
00:31:36,160 --> 00:31:38,800
don't have carbon in them. 
So you weather a silicate rock 

647
00:31:38,800 --> 00:31:42,480
on a very long time scale, it 
forms carbonate in the ocean and

648
00:31:42,480 --> 00:31:45,920
that locks up the carbon in the 
carbonate that you form. 

649
00:31:46,440 --> 00:31:49,880
And that is the geologic 
mechanism of carbon removal that

650
00:31:49,880 --> 00:31:52,600
has kept our planet habitable 
more or less for for billions of

651
00:31:52,600 --> 00:31:53,880
years. 
And so when you're telling this 

652
00:31:53,880 --> 00:31:57,280
story about like does enhanced 
rock weathering work, it's very 

653
00:31:57,280 --> 00:32:01,600
easy to say, obviously it works.
We're here like we have 

654
00:32:01,600 --> 00:32:04,440
wonderful evidence that the 
planet has been inhabitable more

655
00:32:04,440 --> 00:32:06,280
or less for so long. 
Exactly. 

656
00:32:06,520 --> 00:32:09,160
But the the tricky thing about 
that story is that story too 

657
00:32:09,160 --> 00:32:12,560
makes it difficult to kind of 
weave in carbonates because that

658
00:32:12,560 --> 00:32:15,040
story is built around silicates.
It's what we call the silicate 

659
00:32:15,040 --> 00:32:17,320
weathering sheet back. 
Carbonate weathering on those 

660
00:32:17,320 --> 00:32:19,800
long time scales cancels out to 
the point that it really doesn't

661
00:32:19,800 --> 00:32:23,680
matter for carbon removal and it
does matter on short time 

662
00:32:23,680 --> 00:32:25,840
scales. 
But when we also, we often say 

663
00:32:25,840 --> 00:32:28,560
enhanced rock weathering just 
takes Earth's natural thermostat

664
00:32:28,560 --> 00:32:31,680
and speeds it up. 
That natural thermostat process 

665
00:32:31,680 --> 00:32:33,760
is the silicate weathering 
feedback. 

666
00:32:33,840 --> 00:32:36,560
And it's easy to make that case.
It's, it's a wonderful, 

667
00:32:36,560 --> 00:32:40,440
compelling story that like This 
is why our planet exists the way

668
00:32:40,440 --> 00:32:43,800
it does is silicate rocks. 
But that story doesn't extend to

669
00:32:43,800 --> 00:32:45,920
carbonates. 
And it's really hard to, you 

670
00:32:45,920 --> 00:32:49,000
know, tell such a nice story 
around carbonates because of 

671
00:32:49,000 --> 00:32:50,520
that. 
I've never heard anybody who's a

672
00:32:50,520 --> 00:32:54,200
proponent of enhanced carbonate 
weathering frame the problem in 

673
00:32:54,200 --> 00:32:57,440
this really nice simple way 
that, look, we're just speeding 

674
00:32:57,440 --> 00:33:00,880
up Earth's natural thermostat. 
But a lot of those folks talking

675
00:33:00,880 --> 00:33:02,840
about enhanced silicate 
weathering, that's like the 

676
00:33:02,840 --> 00:33:06,000
first line of the conversation 
is precisely that. 

677
00:33:06,120 --> 00:33:08,680
So the narrative in like a bunch
of subtle ways is really 

678
00:33:08,680 --> 00:33:11,760
difficult for carbonates to to 
expand on. 

679
00:33:12,440 --> 00:33:14,200
And that's that's maybe the 
second pillar of why the 

680
00:33:14,200 --> 00:33:16,840
silicate story is easy. 
The first pillar is, look, the 

681
00:33:16,840 --> 00:33:20,760
IPCC said a long time ago that 
carbonates emit carbon and that 

682
00:33:20,760 --> 00:33:23,360
that is maybe true in like the 
very specific way in which 

683
00:33:23,360 --> 00:33:26,360
they've drawn their box. 
But it's not true in the way 

684
00:33:26,360 --> 00:33:29,000
that it's like we care about 
carbon removal is like a broader

685
00:33:29,160 --> 00:33:31,440
process that accounts for what 
happens in the atmosphere. 

686
00:33:32,600 --> 00:33:36,120
It's easy to say, look, stopping
adding carbonate will avoid 

687
00:33:36,120 --> 00:33:38,080
those emissions. 
That's the prong number one. 

688
00:33:38,080 --> 00:33:41,280
I guess prong number 2 is like 
one of the most fundamental 

689
00:33:41,280 --> 00:33:43,280
stories of enhanced rock 
weathering as we're Speaking of 

690
00:33:43,280 --> 00:33:46,520
Earth's natural thermostat, and 
that narrative starts to break 

691
00:33:46,520 --> 00:33:48,680
down when you want to apply it 
to carbonate rocks. 

692
00:33:49,920 --> 00:33:51,920
Then there's a third prong we 
can get into, but we can stop 

693
00:33:51,920 --> 00:33:53,800
here if we want to take a moment
and dig deeper into that 

694
00:33:53,800 --> 00:33:56,560
narratives. 
Yeah, I'm in favor of a prong 

695
00:33:56,560 --> 00:34:02,080
break. 
Yeah, the the advantages and 

696
00:34:02,080 --> 00:34:04,880
disadvantages for the various 
mineral types here is is super 

697
00:34:04,880 --> 00:34:06,800
interesting. 
It also faces problems for 

698
00:34:06,800 --> 00:34:10,920
carbons because it is used for 
pH management and unlocking 

699
00:34:10,920 --> 00:34:14,360
micronutrients and on 
agricultural lands as AG lime. 

700
00:34:14,719 --> 00:34:17,120
So therefore like using 
carbonism this way may not 

701
00:34:17,120 --> 00:34:20,440
qualify as additional because no
one's putting silicate rock on 

702
00:34:20,560 --> 00:34:23,400
farm lands typically for. 
Ross, that's the third. 

703
00:34:23,400 --> 00:34:26,120
Trong, That's the third. 
Narrative. 

704
00:34:26,120 --> 00:34:29,880
Should that be in front? 
Of the Yeah, well, no, no, I 

705
00:34:29,880 --> 00:34:33,679
think those are distinct things 
because the, the idea that like 

706
00:34:33,880 --> 00:34:36,199
we're speeding up Earth's 
natural thermostat, that exists 

707
00:34:36,199 --> 00:34:38,920
regardless of how you decide to 
do the carbon removal. 

708
00:34:39,159 --> 00:34:41,840
But the, the question of like 
whether or not that carbon 

709
00:34:41,840 --> 00:34:46,239
removal is additional in that 
that question is a challenge in 

710
00:34:46,239 --> 00:34:48,880
the context of the carbon 
market, which is the way that 

711
00:34:48,880 --> 00:34:51,080
we're trying to do the carbon 
removal right now for enhanced 

712
00:34:51,080 --> 00:34:54,040
rock weathering. 
And so I think that the last 

713
00:34:54,040 --> 00:34:56,120
piece of like why? 
And then again, there are many 

714
00:34:56,120 --> 00:34:57,200
more, there are others are going
on. 

715
00:34:57,200 --> 00:34:59,360
These are the three things that 
float to the surface for me. 

716
00:34:59,960 --> 00:35:02,200
But the last piece for 
bicarbonates are difficult to 

717
00:35:02,200 --> 00:35:05,200
support narratively is that 
we're already doing it. 

718
00:35:05,200 --> 00:35:07,600
We're already spreading rock, 
carbonate rocks on fields for 

719
00:35:07,600 --> 00:35:09,760
agronomic purposes. 
When we're talking about 

720
00:35:09,760 --> 00:35:11,720
enhanced rock weathering, 
terrestrial enhanced rock 

721
00:35:11,720 --> 00:35:13,560
weathering, we're usually 
talking about spreading it on 

722
00:35:13,560 --> 00:35:16,520
agricultural fields. 
So is it any different? 

723
00:35:16,520 --> 00:35:18,600
Is it, are you doing something 
that wouldn't have happened 

724
00:35:18,600 --> 00:35:20,600
already if you're spreading 
carbonate rock? 

725
00:35:21,320 --> 00:35:24,240
The answer is, like, mostly 
probably, yeah, because we're 

726
00:35:24,240 --> 00:35:25,960
not spreading at carbonate rock 
everywhere. 

727
00:35:25,960 --> 00:35:28,520
It's a common enough practice, 
but it's not universal. 

728
00:35:28,760 --> 00:35:30,680
So you can find places where it 
would be new. 

729
00:35:30,960 --> 00:35:34,160
But we've talked to a number of 
buyers and other folks who want 

730
00:35:34,160 --> 00:35:36,760
to support enhanced rock 
weathering who say, well, I'm 

731
00:35:36,760 --> 00:35:39,720
just worried that it's hard to 
sell the story that what you're 

732
00:35:39,720 --> 00:35:41,880
doing is additional because we 
know that we're already 

733
00:35:41,880 --> 00:35:44,280
spreading carbonate rock. 
It's a little bit of like, like 

734
00:35:44,280 --> 00:35:47,320
showing up to a job interview 
and they're like, oh, I'm sorry,

735
00:35:47,320 --> 00:35:51,560
you have a lot of experience in 
this jobs like we can't, we 

736
00:35:51,560 --> 00:35:53,920
can't hire you. 
But this is one of the other 

737
00:35:53,920 --> 00:35:56,360
pieces like why it's hard, I 
think, narratively to support 

738
00:35:56,360 --> 00:35:57,880
carbonates. 
To be clear, like the same 

739
00:35:57,880 --> 00:36:01,440
problems apply to silicates. 
If you like, mathematically, if 

740
00:36:01,440 --> 00:36:04,360
you want to spread silicate 
rocks on a field that has been 

741
00:36:04,360 --> 00:36:08,640
limed or where carbonate has 
been used historically, you need

742
00:36:08,640 --> 00:36:10,720
to make sure that the silicate 
rock is doing something 

743
00:36:10,720 --> 00:36:13,040
additional relative to what the 
carbonate that you've 

744
00:36:13,040 --> 00:36:14,440
historically applied would have 
done. 

745
00:36:14,680 --> 00:36:16,880
But narratively, it's easier to 
say that this wouldn't have 

746
00:36:16,880 --> 00:36:19,600
happened because so few people 
are spreading silicate rocks on 

747
00:36:19,600 --> 00:36:23,160
their fields as it is, but more 
are spreading carbonates. 

748
00:36:24,320 --> 00:36:27,520
My understanding of the 
possibility for carbonates to 

749
00:36:27,520 --> 00:36:32,000
become additional is that since 
they are used primarily or 

750
00:36:32,000 --> 00:36:36,640
mostly primarily for pH 
management, but that too much 

751
00:36:36,640 --> 00:36:40,080
acidity or the wrong types of 
acidity caused the carbon to be 

752
00:36:40,080 --> 00:36:41,720
more emitted than it would 
otherwise be. 

753
00:36:41,720 --> 00:36:44,560
That's my understanding of the 
the chemical feedback here. 

754
00:36:44,760 --> 00:36:47,720
In which case the field that you
would be using for agronomic 

755
00:36:47,720 --> 00:36:49,880
benefits are potentially 
different from the ones that you

756
00:36:49,880 --> 00:36:51,440
would be using for the carbon 
removal benefits. 

757
00:36:51,600 --> 00:36:53,440
Is that true? 
Is my understanding correct? 

758
00:36:54,600 --> 00:36:57,120
When you say the field you would
be using for agronomic benefits,

759
00:36:57,120 --> 00:37:00,120
I I think maybe one way to think
about it is like the way that 

760
00:37:00,120 --> 00:37:02,960
you optimize how you're 
spreading rock is going to look 

761
00:37:02,960 --> 00:37:05,680
different for agronomic benefits
than it would for carbon removal

762
00:37:05,680 --> 00:37:07,520
benefits potentially in many 
cases. 

763
00:37:08,320 --> 00:37:10,720
What we know is that, like, in 
many cases, we're spreading 

764
00:37:10,720 --> 00:37:13,600
carbonate on fields already in a
way that is removing carbon from

765
00:37:13,600 --> 00:37:15,400
the atmosphere. 
And we're doing that 

766
00:37:15,400 --> 00:37:17,200
accidentally. 
Like we're not trying to remove 

767
00:37:17,200 --> 00:37:19,080
carbon from the atmosphere. 
But that raises exciting 

768
00:37:19,080 --> 00:37:21,560
questions about like, wow, what 
could we do if we were actually 

769
00:37:21,560 --> 00:37:23,960
trying to remove the carbon from
the atmosphere? 

770
00:37:24,600 --> 00:37:27,080
But you're bringing me to like, 
I think it's worthwhile taking a

771
00:37:27,080 --> 00:37:30,000
break here to say what are the 
differences between silicates 

772
00:37:30,080 --> 00:37:32,480
and carbonates? 
I mentioned upfront that like, 

773
00:37:32,480 --> 00:37:34,680
they're not like interchangeable
necessarily. 

774
00:37:34,680 --> 00:37:36,080
They have their own strengths 
and weaknesses. 

775
00:37:36,080 --> 00:37:37,520
And there are important 
differences. 

776
00:37:37,920 --> 00:37:40,840
And the two things that I think 
are the most important to focus 

777
00:37:40,840 --> 00:37:44,360
on are how fast they weather and
whether they have carbon in them

778
00:37:44,360 --> 00:37:47,400
or not. 
So carbonates, they tend to 

779
00:37:47,400 --> 00:37:51,080
weather really, really fast, 
often an order or two orders of 

780
00:37:51,080 --> 00:37:54,160
magnitude faster than a lot of 
silicate minerals do. 

781
00:37:54,840 --> 00:37:58,320
So they much, much faster. 
But they have carbon in them, 

782
00:37:58,320 --> 00:38:02,120
which means that that that 
limits how how effective and 

783
00:38:02,120 --> 00:38:04,400
efficient they are at removing 
carbon from the atmosphere 

784
00:38:04,640 --> 00:38:06,960
because that has to compete with
the carbon that's already in the

785
00:38:06,960 --> 00:38:10,480
rock when that rock dissolves. 
Silicates on the other hand, 

786
00:38:10,880 --> 00:38:14,440
pure silicate minerals don't 
have carbon in them and so they 

787
00:38:14,440 --> 00:38:16,600
tend to be more efficient at 
removing carbon from the 

788
00:38:16,600 --> 00:38:18,880
atmosphere, but they dissolve 
more slowly. 

789
00:38:19,080 --> 00:38:23,480
So often it it matters a lot 
more like how finely you grind 

790
00:38:23,480 --> 00:38:26,680
your silicate rock in order to 
increase how quickly that rock 

791
00:38:26,680 --> 00:38:29,600
is going to dissolve or weather.
Then it matters for carbonates. 

792
00:38:29,600 --> 00:38:31,760
But you have this trade off 
where carbonates go really quick

793
00:38:31,760 --> 00:38:33,160
but they have this carbon in 
them. 

794
00:38:33,240 --> 00:38:36,120
Silicates tend to go more 
slowly, but they don't have 

795
00:38:36,120 --> 00:38:39,240
carbon in them. 
And the issue with carbonates 

796
00:38:39,240 --> 00:38:42,960
having carbon in them is that if
you're in a really acidic field,

797
00:38:43,560 --> 00:38:46,680
it's very likely that you're not
going to be able to get your 

798
00:38:46,680 --> 00:38:48,720
carbon removal. 
And instead you might just admit

799
00:38:48,720 --> 00:38:51,440
that carbon that was in the rock
into the atmosphere. 

800
00:38:52,240 --> 00:38:54,400
Now, there are questions about 
like, you know, depending on 

801
00:38:54,400 --> 00:38:56,760
where you draw your boundary, 
that could be really bad for the

802
00:38:56,760 --> 00:38:59,560
climate or just a little bit bad
or maybe not that bad at all. 

803
00:38:59,560 --> 00:39:02,120
Maybe it's net zero, depending 
on how do you draw the system 

804
00:39:02,120 --> 00:39:04,520
boundary, which is really 
complicated and we don't need to

805
00:39:04,520 --> 00:39:09,400
get into, but it it it is one of
the concerns around like the 

806
00:39:09,400 --> 00:39:11,440
narrative of carbonates. 
It's like, look, there's a 

807
00:39:11,440 --> 00:39:13,880
potential that carbonates are 
emitting carbon to the 

808
00:39:13,880 --> 00:39:16,600
atmosphere and that creates this
risk. 

809
00:39:17,320 --> 00:39:23,000
I think in my mind, like that 
same potential sort exists for 

810
00:39:23,000 --> 00:39:24,720
silicates. 
If you expand the system to have

811
00:39:24,720 --> 00:39:28,240
very long it wide enough, like 
we're always trucking rock and 

812
00:39:28,240 --> 00:39:29,760
crushing rock and radiant to the
field. 

813
00:39:29,760 --> 00:39:32,520
And though that requires 
emissions, you could all that 

814
00:39:32,520 --> 00:39:35,720
like you need to outweigh those 
emissions when you spread rock 

815
00:39:35,720 --> 00:39:37,960
on your field. 
So just because you can have 

816
00:39:37,960 --> 00:39:42,360
emissions with carbonate that is
like downstream as what happens 

817
00:39:42,360 --> 00:39:44,800
with transporting the rock, 
doesn't mean that like you can 

818
00:39:44,800 --> 00:39:47,840
ignore the problem of emissions 
in a silicate deployment. 

819
00:39:47,840 --> 00:39:54,800
I don't know if that made sense.
I answered my previous question 

820
00:39:54,800 --> 00:39:59,080
to were yeah, field sufficiently
acidic or with certain kinds of 

821
00:39:59,080 --> 00:40:02,600
acidity? 
It might just negate the carbon 

822
00:40:02,600 --> 00:40:05,440
removal potential of carbonates 
because it doesn't play nice in 

823
00:40:05,440 --> 00:40:06,560
the kinds of ways that we need 
for. 

824
00:40:06,640 --> 00:40:09,160
There's like perfect 1 to 1 
overlap, which may help the 

825
00:40:09,160 --> 00:40:11,280
additionality story, but it's 
one of those things where it's 

826
00:40:11,520 --> 00:40:14,360
like the details matter, which 
is a hard thing to explain to 

827
00:40:14,560 --> 00:40:15,920
buyers. 
You typically want to be talking

828
00:40:15,920 --> 00:40:17,400
about. 
We're enhancing the natural 

829
00:40:17,400 --> 00:40:20,720
cycles of the earth. 
There's no fancy footwork here. 

830
00:40:20,720 --> 00:40:22,840
We're just purely natural, and 
natural is always good. 

831
00:40:22,840 --> 00:40:24,560
Don't you know, like a thumbs 
up? 

832
00:40:25,160 --> 00:40:28,440
This is also why silicate 
weathering tends to take place 

833
00:40:28,440 --> 00:40:30,720
in the tropics where there's 
more rainfall so that you can, 

834
00:40:30,880 --> 00:40:33,800
you can get around some of the 
issues of the slower weathering 

835
00:40:33,840 --> 00:40:37,200
rate because you have things 
that are, they'd be there 

836
00:40:37,200 --> 00:40:39,280
increase the surface area so 
much or they just have more 

837
00:40:39,280 --> 00:40:41,080
interaction with water and 
things like that. 

838
00:40:41,400 --> 00:40:43,920
And that's why people who are 
interested in carbonates are 

839
00:40:43,920 --> 00:40:45,920
more tolerant of temperate 
zones. 

840
00:40:45,920 --> 00:40:48,720
And it's, it's a latitudinal 
almost more than anything else. 

841
00:40:48,720 --> 00:40:51,560
I want to think about who's 
involved in and the people I 

842
00:40:51,560 --> 00:40:53,800
have in mind. 
Depends on where they're doing 

843
00:40:53,800 --> 00:40:56,360
business, basically. 
It does. 

844
00:40:56,400 --> 00:40:59,120
I think one thing we over index 
on a little bit is the idea that

845
00:40:59,120 --> 00:41:01,080
carbonates don't work in acidic 
soils. 

846
00:41:01,280 --> 00:41:04,160
And it's true that like in 
really acidic soils, spreading 

847
00:41:04,160 --> 00:41:06,360
carbonate probably emits carbon 
to the atmosphere and we don't 

848
00:41:06,360 --> 00:41:09,360
want to do that. 
But the fact of adding rock to 

849
00:41:09,360 --> 00:41:12,600
soil changes the pH conditions 
of that soil itself. 

850
00:41:12,920 --> 00:41:16,280
So over time, you could totally 
add the rock amendments that 

851
00:41:16,280 --> 00:41:19,640
makes the soil amenable to 
continued carbonate carbon 

852
00:41:19,640 --> 00:41:22,560
removal, even if today that soil
is really acidic. 

853
00:41:23,000 --> 00:41:26,200
And so it, it where we are now 
doesn't necessarily we don't 

854
00:41:26,200 --> 00:41:28,120
have to draw firm boundaries 
around where it works and where 

855
00:41:28,120 --> 00:41:30,000
it doesn't. 
And carbonates more so than 

856
00:41:30,240 --> 00:41:32,240
silicates, at least in the 
models that I've been running 

857
00:41:32,520 --> 00:41:35,840
are much more responsive to 
increases in rainfall or water 

858
00:41:35,840 --> 00:41:38,960
infiltration in the soil. 
So one of the tricky things for 

859
00:41:38,960 --> 00:41:42,160
the the real, again, like the 
mega nerds out there is that in 

860
00:41:42,160 --> 00:41:44,480
the models that we've been 
running, this hasn't really been

861
00:41:44,480 --> 00:41:46,800
super well validated in shield 
studies yet. 

862
00:41:47,160 --> 00:41:50,040
In the models even running 
carbonate has a little bit of an

863
00:41:50,040 --> 00:41:52,120
upper limit. 
So you can only add so much rock

864
00:41:52,120 --> 00:41:54,960
before it saturates and you 
don't get more carbon removal 

865
00:41:54,960 --> 00:41:58,040
for more rock. 
And you can overcome that upper 

866
00:41:58,040 --> 00:41:59,760
limit by dumping more water on 
it. 

867
00:41:59,760 --> 00:42:01,880
It's very, it really likes 
having more water. 

868
00:42:02,120 --> 00:42:04,720
Carbonates do. 
And so if you have a, a soil 

869
00:42:04,720 --> 00:42:07,160
that's not too acidic and it's 
it's well watered, carbonates 

870
00:42:07,160 --> 00:42:08,760
are going to be very happy 
there. 

871
00:42:09,120 --> 00:42:12,040
Silicates don't seem to have 
that same like saturation limit,

872
00:42:12,280 --> 00:42:13,840
at least in the models that 
we've been running. 

873
00:42:13,840 --> 00:42:16,200
So you can add more and more 
rock and you tend to get more 

874
00:42:16,200 --> 00:42:19,440
and more carbon removal. 
The question though, is like, 

875
00:42:19,520 --> 00:42:21,400
how much rock can you actually 
spread on a field? 

876
00:42:21,600 --> 00:42:25,320
And does that additional rock? 
Like is that an amount that's 

877
00:42:25,320 --> 00:42:28,160
reasonable for what farmers are 
going to be comfortable adding 

878
00:42:28,160 --> 00:42:30,480
on their field? 
Or, you know, one of the big 

879
00:42:30,600 --> 00:42:33,440
questions is how many times can 
you drive a spreader over a 

880
00:42:33,440 --> 00:42:36,280
field before you've compacted 
the soil too much that you're 

881
00:42:36,280 --> 00:42:38,400
not happy with the outcome? 
So there, there are limits and 

882
00:42:38,400 --> 00:42:41,000
how much Rock You can spread 
already that are built into the 

883
00:42:41,000 --> 00:42:42,840
system. 
But carbonates also have this 

884
00:42:42,840 --> 00:42:44,800
limit where they tend to 
saturate quicker. 

885
00:42:45,200 --> 00:42:48,520
And so there there's all of 
these questions around like 

886
00:42:48,520 --> 00:42:50,320
which rock is better? 
There's no simple answer to 

887
00:42:50,320 --> 00:42:53,200
that, but it seems that they 
they sit different niches. 

888
00:42:54,040 --> 00:42:55,720
OK. 
So we've heard the the silicon 

889
00:42:55,720 --> 00:43:00,200
story that has been sort of the 
canonical position for a long 

890
00:43:00,200 --> 00:43:02,680
time. 
We've heard some of the changes 

891
00:43:02,680 --> 00:43:05,840
that come from carbonate 
research and maybe how that can 

892
00:43:05,840 --> 00:43:08,960
play a role here or can also be 
a part of carbon removal in ways

893
00:43:08,960 --> 00:43:12,760
that previously it was not. 
Make the case back if you're 

894
00:43:12,760 --> 00:43:15,320
working in silicates or thinking
about silicates, for why 

895
00:43:15,520 --> 00:43:19,640
silicates are still the way to 
go and carbonates are not nearly

896
00:43:20,840 --> 00:43:22,880
as rosy as you paint a picture 
of Tyler. 

897
00:43:22,880 --> 00:43:24,800
You actually aren't. 
You've actually disabused me of 

898
00:43:24,800 --> 00:43:26,880
several assumptions that I've 
made during this conversation. 

899
00:43:26,880 --> 00:43:29,600
But try and set the record clear
for why silicates still. 

900
00:43:30,640 --> 00:43:33,040
Yeah. 
So I think to be really clear, 

901
00:43:33,560 --> 00:43:36,560
carbonates aren't like 
inherently better and silicates 

902
00:43:36,560 --> 00:43:38,040
aren't also inherently better 
like these are. 

903
00:43:38,040 --> 00:43:40,200
There really are just different 
strengths and weaknesses here. 

904
00:43:40,200 --> 00:43:42,960
And one of the issues is we 
don't know it as much about 

905
00:43:42,960 --> 00:43:46,440
carbonates because the research 
has coalesced around silicates. 

906
00:43:46,840 --> 00:43:48,760
The papers that look at 
carbonates tell us that it 

907
00:43:48,760 --> 00:43:50,080
could, they could be really 
promising. 

908
00:43:50,520 --> 00:43:53,400
But one thing that is nice about
silicates is that you don't have

909
00:43:53,400 --> 00:43:56,320
to worry about emitting fossil 
carbon to the atmosphere. 

910
00:43:56,720 --> 00:43:59,520
A tricky bit of that is you need
to really know what your rock is

911
00:43:59,520 --> 00:44:02,400
because you can have carbonate 
that is cementing inside of a 

912
00:44:02,400 --> 00:44:04,640
silicate rock. 
And if you don't know that it's 

913
00:44:04,640 --> 00:44:06,640
there, I know it really 
shouldn't. 

914
00:44:07,080 --> 00:44:09,520
But if you don't know that it's 
there, you might you might think

915
00:44:09,520 --> 00:44:11,320
that it's delicate weathering 
when it's actually carbonate 

916
00:44:11,320 --> 00:44:13,560
weathering and that that's a big
issue that we need to deal with 

917
00:44:13,560 --> 00:44:15,240
and. 
Like in the various mineral 

918
00:44:15,240 --> 00:44:17,760
compositions of the the queries 
that people are are drawing 

919
00:44:17,760 --> 00:44:20,520
from, is that a common thing or 
is that just like in Wyoming in 

920
00:44:20,520 --> 00:44:24,240
one particular place? 
I think it's relatively common. 

921
00:44:24,240 --> 00:44:27,520
It's definitely not unheard of. 
And one of the things is it's 

922
00:44:27,520 --> 00:44:29,920
often in a small enough amount 
that it might be hard to detect 

923
00:44:29,920 --> 00:44:32,880
with like course resolution, 
mineralogical analysis. 

924
00:44:33,920 --> 00:44:36,960
But it, it is when you have 
carbonate in your rock, it's the

925
00:44:36,960 --> 00:44:38,160
first thing that's going to 
dissolve. 

926
00:44:38,320 --> 00:44:41,720
And so you, if you're measuring 
a really rapid pulse of 

927
00:44:41,720 --> 00:44:45,800
weathering, you might be, it 
might be worthwhile just double 

928
00:44:45,800 --> 00:44:47,560
checking that you don't have 
carbonate in your rock. 

929
00:44:47,880 --> 00:44:50,320
Because if you think that it's 
carbonate rather than, or you 

930
00:44:50,320 --> 00:44:52,480
think that it's silicate rather 
than carbonate or use the use 

931
00:44:52,480 --> 00:44:55,240
the wrong assumptions about the 
efficiency of carbon removal. 

932
00:44:55,240 --> 00:44:58,640
Essentially, because as we said,
carbonate has carbon in it and 

933
00:44:58,640 --> 00:45:02,400
silicates don't. 
But the silicates have, you 

934
00:45:02,400 --> 00:45:04,960
know, they, they don't have 
carbon in them, which is really 

935
00:45:04,960 --> 00:45:06,560
nice. 
You can, when you grind them up 

936
00:45:06,560 --> 00:45:08,680
really finely, they do weather 
faster. 

937
00:45:08,680 --> 00:45:11,520
And much the same way that like 
if you crush your ice before you

938
00:45:11,520 --> 00:45:13,440
put it in a drink, it's going to
dissolve faster. 

939
00:45:14,160 --> 00:45:16,320
It's by like when you go to a 
fancy cocktail bar, they give 

940
00:45:16,320 --> 00:45:19,160
you a really big ice cube so 
that weather dissolves very 

941
00:45:19,160 --> 00:45:20,960
slowly. 
It's the same kind of principle.

942
00:45:22,440 --> 00:45:25,360
And we know a lot more about 
silicates now because we've been

943
00:45:25,360 --> 00:45:28,160
doing it for, so we've been 
researching it for a while. 

944
00:45:29,040 --> 00:45:31,800
I think there are still a lot of
open questions around silicates,

945
00:45:32,160 --> 00:45:35,320
but we know more there. 
One additional thing that I 

946
00:45:35,320 --> 00:45:38,480
think if enhanced weathering 
folks are listening to this, 

947
00:45:38,800 --> 00:45:41,200
they might be screaming at the 
like, oh, they're definitely. 

948
00:45:41,280 --> 00:45:43,040
Doing that. 
Right now, yeah, they might be 

949
00:45:43,040 --> 00:45:45,440
screaming at their at their 
phones or laptops or whatever 

950
00:45:45,440 --> 00:45:48,000
saying like no ion exchange, 
Matt, you're not talking about 

951
00:45:48,000 --> 00:45:51,920
ion exchange processes, which is
another issue that is really in 

952
00:45:51,920 --> 00:45:54,840
the weeds. 
But the key take away is that 

953
00:45:54,840 --> 00:45:57,600
when you start doing enhanced 
rock weathering at a place that 

954
00:45:57,600 --> 00:46:01,440
you haven't been amending with 
rock in the past or amending 

955
00:46:01,440 --> 00:46:05,280
very minimally, one of the first
things that happens is that when

956
00:46:05,280 --> 00:46:09,160
the rock dissolves the stuff, 
the cations, which is the thing 

957
00:46:09,160 --> 00:46:12,040
that removes the carbon from the
atmosphere by charge balance, 

958
00:46:12,520 --> 00:46:16,040
those cations knock off acidity 
from the absorb to the soil. 

959
00:46:16,440 --> 00:46:20,000
And that acidity limits how much
carbon is removed from the 

960
00:46:20,000 --> 00:46:22,440
atmosphere because you, you 
neutralize that acidity, which 

961
00:46:22,440 --> 00:46:26,160
is not carbon dependent first. 
And then later you do the carbon

962
00:46:26,160 --> 00:46:29,640
removal. 
And when you're adding silicate 

963
00:46:29,640 --> 00:46:33,320
rocks, neutralizing that acidity
means that you just don't do 

964
00:46:33,320 --> 00:46:36,240
carbon removal that much. 
You you kind of hit zero. 

965
00:46:36,720 --> 00:46:38,880
But when you're doing it with 
carbonate rocks and neutralizing

966
00:46:38,880 --> 00:46:41,560
that initial acidity means that 
you're emitting carbon to the 

967
00:46:41,560 --> 00:46:44,280
atmosphere. 
So that is also narratively a 

968
00:46:44,280 --> 00:46:49,160
really difficult story to tell. 
However, like what what we need 

969
00:46:49,160 --> 00:46:51,920
to keep in mind is that it takes
emissions to transport rocks to 

970
00:46:51,920 --> 00:46:54,080
your field. 
So if you're hitting zero carbon

971
00:46:54,080 --> 00:46:57,160
removal with a silicate rock, 
you're net emitting. 

972
00:46:57,240 --> 00:47:00,080
The process as a whole is net 
emitting because you have to use

973
00:47:00,080 --> 00:47:02,720
emissions to grind the rock up 
and to transport it to your 

974
00:47:02,720 --> 00:47:05,000
field. 
And the question becomes, is it 

975
00:47:05,000 --> 00:47:09,240
more net emitting than your 
carbonate rock counterparts? 

976
00:47:09,640 --> 00:47:12,280
And will that lag before you 
kind of neutralize all that 

977
00:47:12,280 --> 00:47:15,200
acidity be shorter or longer 
than if you were using 

978
00:47:15,200 --> 00:47:18,040
carbonates? 
So the ion exchange component, 

979
00:47:18,120 --> 00:47:19,640
it looks really good for 
silicates. 

980
00:47:19,960 --> 00:47:22,480
It also because you're not 
emitting carbon when you're 

981
00:47:22,560 --> 00:47:27,120
neutralizing that initial pool 
of acidity, but also you're 

982
00:47:27,120 --> 00:47:29,520
still emitting carbon through 
your upstream processes. 

983
00:47:29,520 --> 00:47:32,200
And we haven't had done, I don't
think any analysis yet has 

984
00:47:32,200 --> 00:47:34,480
factored that in. 
We're looking at that right now.

985
00:47:34,480 --> 00:47:36,640
I don't it's too early to have 
like clear answers. 

986
00:47:36,960 --> 00:47:39,880
And the answers are going to be 
really dependent on how you run 

987
00:47:39,880 --> 00:47:41,840
the model like because we 
there's a lot of tunable 

988
00:47:41,840 --> 00:47:44,360
parameters here. 
So there's no universal answer 

989
00:47:44,360 --> 00:47:46,960
to this question. 
One thing that I've heard is 

990
00:47:46,960 --> 00:47:51,040
that, well, I also just know it 
from touching things like basalt

991
00:47:51,040 --> 00:47:55,280
versus limestone, where 
limestone is just so much softer

992
00:47:55,560 --> 00:47:59,680
and basaltic rock and silicates 
are harder and like the amount 

993
00:47:59,680 --> 00:48:02,560
of grinding and energy to grind 
is much greater for silicates. 

994
00:48:02,560 --> 00:48:04,920
Is that broadly true? 
That is true. 

995
00:48:05,520 --> 00:48:07,600
All of our estimates of how much
energy it takes tells us 

996
00:48:07,600 --> 00:48:10,680
silicates are harder to grind 
up, but also like the grinding 

997
00:48:10,680 --> 00:48:13,240
emissions are thought to be 
relatively like a smaller 

998
00:48:13,240 --> 00:48:15,360
component of all of the upstream
emissions. 

999
00:48:16,200 --> 00:48:18,560
So in my models and in the 
simulations I've been running, 

1000
00:48:18,560 --> 00:48:20,760
like the big thing that matters 
is how are you transporting the 

1001
00:48:20,760 --> 00:48:22,400
rock? 
Are you using a truck, a barge? 

1002
00:48:22,400 --> 00:48:25,600
And how far are you moving it? 
And the grinding emissions are, 

1003
00:48:25,600 --> 00:48:27,200
you know, a smaller fraction of 
that. 

1004
00:48:27,480 --> 00:48:29,280
So it's not, it's not a make or 
break. 

1005
00:48:29,280 --> 00:48:31,840
What is kind of more of a make 
or break is that in my 

1006
00:48:31,840 --> 00:48:35,240
simulations at least, and a few 
others that I've seen, in order 

1007
00:48:35,240 --> 00:48:38,040
to achieve the same carbon 
removal, you need more silicate 

1008
00:48:38,040 --> 00:48:40,440
rock because it weathers more 
slowly. 

1009
00:48:40,440 --> 00:48:43,200
So any given year, if you want 
to do X amount of carbon 

1010
00:48:43,200 --> 00:48:45,560
removal, you probably need more 
silicates than you do 

1011
00:48:45,560 --> 00:48:47,560
carbonates. 
And that means you're 

1012
00:48:47,560 --> 00:48:49,840
transporting more rock and 
you're grinding more rock to 

1013
00:48:49,840 --> 00:48:52,560
make all of that work, which 
carries with it that emissions 

1014
00:48:52,560 --> 00:48:54,840
burden. 
So you're kind of you have to 

1015
00:48:54,840 --> 00:48:57,080
chase that emissions burden as 
you add more and more rock 

1016
00:48:57,080 --> 00:48:59,080
essentially to make those things
kind of balance out. 

1017
00:49:00,600 --> 00:49:04,800
Tyler, I have friends who are on
both sides of this one where 

1018
00:49:04,800 --> 00:49:08,800
some people I know are extreme 
partisans of the carbonate 

1019
00:49:09,320 --> 00:49:11,920
insurgency. 
I guess you could say I probably

1020
00:49:11,920 --> 00:49:13,160
shouldn't characterize it that 
way. 

1021
00:49:13,600 --> 00:49:16,520
I'm, you know, friends with many
people who are doing business in

1022
00:49:16,520 --> 00:49:21,000
silicates and to me it doesn't 
necessarily seem like this has 

1023
00:49:21,000 --> 00:49:24,920
to be business make or break. 
I can imagine that they're like 

1024
00:49:24,920 --> 00:49:27,680
one of the the business models. 
I think is is so clever in 

1025
00:49:27,680 --> 00:49:30,600
carbon removal is Charm's 
ability to do bio oil and 

1026
00:49:30,600 --> 00:49:33,240
biochar depending on the 
feedstock and the relative 

1027
00:49:33,240 --> 00:49:35,080
values of those products and 
being able to split the 

1028
00:49:35,080 --> 00:49:36,440
difference. 
How I think it's like such a 

1029
00:49:36,440 --> 00:49:39,400
smart idea. 
Is there not an opportunity for 

1030
00:49:40,280 --> 00:49:44,040
enhanced weathering project 
developers to say like in this 

1031
00:49:44,040 --> 00:49:48,360
geography with we have a quarry 
over here for great carbonate 

1032
00:49:48,360 --> 00:49:50,400
rock in the field that we're 
going to put it on as a great 

1033
00:49:50,400 --> 00:49:53,040
fit for it? 
Like does it have to be so 

1034
00:49:53,600 --> 00:49:55,800
contested a ground? 
I feel like in different 

1035
00:49:55,800 --> 00:49:59,320
circumstances, different types 
of rocks can make the LCA and 

1036
00:49:59,320 --> 00:50:02,040
system boundaries work in ways 
that still be commercially 

1037
00:50:02,040 --> 00:50:03,760
viable. 
I don't know that project 

1038
00:50:03,760 --> 00:50:06,240
developers in enhanced 
weathering have to be silicate 

1039
00:50:06,240 --> 00:50:09,240
or carbonate exclusive. 
They could probably be good at 

1040
00:50:09,240 --> 00:50:11,320
both of these things. 
Or maybe you just need too many 

1041
00:50:11,320 --> 00:50:14,360
geochemists on staff to figure 
out the rock types. 

1042
00:50:14,360 --> 00:50:16,320
By the way, does that how it 
works with like you get some 

1043
00:50:16,320 --> 00:50:18,600
geochemists here, like I only do
carbonate, I only do silicate 

1044
00:50:18,600 --> 00:50:20,240
stuff? 
Or could there not be productive

1045
00:50:20,240 --> 00:50:21,920
overlap here? 
There's a lot of productive 

1046
00:50:21,920 --> 00:50:23,720
overlap. 
There's no reason, yeah, no 

1047
00:50:23,720 --> 00:50:25,280
reason that you need to do just 
one. 

1048
00:50:25,280 --> 00:50:27,400
I think that the reason that 
there's tension right now is 

1049
00:50:27,400 --> 00:50:30,280
precisely the fact that there is
this divergent between where 

1050
00:50:30,280 --> 00:50:32,880
investment is going and where 
the evidence is that like, hey, 

1051
00:50:32,880 --> 00:50:35,320
look, carbonates could do really
well, especially in certain 

1052
00:50:35,320 --> 00:50:37,880
environments. 
And so it feels like there has 

1053
00:50:37,880 --> 00:50:39,840
to be tension because you're 
fighting for silicate money, 

1054
00:50:39,840 --> 00:50:43,160
money that's going to silicate 
deployments when we could just 

1055
00:50:43,160 --> 00:50:46,200
be in, you know, putting in 
research and development money 

1056
00:50:46,200 --> 00:50:48,920
into both. 
I think like the thing that 

1057
00:50:48,920 --> 00:50:51,200
brings them together. 
Also, companies are thinking 

1058
00:50:51,200 --> 00:50:54,840
about maybe I do both. 
Maybe I do one rock type for my 

1059
00:50:54,840 --> 00:50:57,800
early stage, or I'm trying to 
neutralize that initial pool of 

1060
00:50:57,800 --> 00:50:59,600
acidity and then I transition to
a nut. 

1061
00:50:59,600 --> 00:51:02,320
Like there are ways to optimize 
here that we're just starting to

1062
00:51:02,320 --> 00:51:05,480
scratch the surface of, but it's
not super common to be in a 

1063
00:51:05,480 --> 00:51:08,760
place where you have access to 
both types of rock that you can 

1064
00:51:08,760 --> 00:51:11,600
ship to your field. 
It's just too disparate and too.

1065
00:51:11,600 --> 00:51:13,360
Formal, exactly. 
Yeah, Yeah. 

1066
00:51:13,360 --> 00:51:16,040
So it's not, that's not super 
not often in like direct local 

1067
00:51:16,040 --> 00:51:18,920
competition. 
But I think one of the 

1068
00:51:18,920 --> 00:51:20,960
challenges is that like 
regardless of where you go, 

1069
00:51:20,960 --> 00:51:25,040
whether silicates or carbonates 
it, what appears to be the case.

1070
00:51:25,040 --> 00:51:28,440
What we're learning right now is
that the way that we've built 

1071
00:51:28,440 --> 00:51:31,880
out the market so far, we're 
going to be restricting some 

1072
00:51:31,880 --> 00:51:34,800
potentially good projects from 
happening, whether that's 

1073
00:51:34,800 --> 00:51:38,400
because you are in like a really
noisy quote UN quote noisy 

1074
00:51:38,400 --> 00:51:39,840
field. 
So it's hard to detect the 

1075
00:51:39,840 --> 00:51:42,280
carbon removal signal with 
measurements, whether that's 

1076
00:51:42,280 --> 00:51:44,800
because maybe you're using a 
rock feedstock that doesn't have

1077
00:51:44,800 --> 00:51:47,720
the right tracer elements in it 
that you need to do the type of 

1078
00:51:47,720 --> 00:51:50,760
measurement that you want to do,
even if that rock weather is 

1079
00:51:50,760 --> 00:51:52,960
really shast and can do really 
good, but it's just hard to do 

1080
00:51:52,960 --> 00:51:56,600
the measurement that way. 
Or maybe, you know, you're in 

1081
00:51:56,680 --> 00:51:59,360
like a region that historically 
farmers have been spreading 

1082
00:51:59,360 --> 00:52:01,440
carbonate and so it's hard to 
demonstrate that what you're 

1083
00:52:01,440 --> 00:52:03,640
doing is new above what would 
have happened already. 

1084
00:52:03,640 --> 00:52:06,240
There's a whole bunch of reasons
why the way that we're doing 

1085
00:52:06,240 --> 00:52:08,840
things are potentially limiting 
really good projects. 

1086
00:52:09,360 --> 00:52:12,320
And that is creating this like 
push toward thinking about, OK, 

1087
00:52:12,320 --> 00:52:14,640
what are other ways we can 
support enhanced rock weather. 

1088
00:52:14,640 --> 00:52:17,880
And, and there's increasingly a 
push toward thinking about 

1089
00:52:17,880 --> 00:52:22,360
policy mechanisms like subsidies
and pay for practice models that

1090
00:52:22,600 --> 00:52:26,160
are really exciting because they
could let you sidestep some of 

1091
00:52:26,160 --> 00:52:28,720
the constraints of the market 
and and potentially support 

1092
00:52:28,720 --> 00:52:31,520
projects that just aren't viable
in the market to help enhance 

1093
00:52:31,520 --> 00:52:33,320
weathering reach that broader 
potential. 

1094
00:52:34,880 --> 00:52:37,280
But I think like a really tricky
thing with that, that in 

1095
00:52:37,280 --> 00:52:39,800
something that we have to think 
about with any path dependence 

1096
00:52:39,800 --> 00:52:42,880
question is that if you are on a
path, you have the destination, 

1097
00:52:42,880 --> 00:52:46,480
a goal, a place you want to go. 
In theory, adding policy 

1098
00:52:46,480 --> 00:52:50,920
mechanisms will expand how much 
types of enhanced weathering we 

1099
00:52:50,920 --> 00:52:53,560
can do. 
But in practice, at a certain 

1100
00:52:53,560 --> 00:52:56,440
point, like if you have a 
subsidy for spreading rocks on 

1101
00:52:56,440 --> 00:52:59,680
fields everywhere at every 
country, that raises questions 

1102
00:52:59,680 --> 00:53:01,760
about how much of the carbon 
removal that you're doing in the

1103
00:53:01,760 --> 00:53:04,120
market is actually additional 
relative to what would have 

1104
00:53:04,120 --> 00:53:06,400
happened without the market 
practice. 

1105
00:53:06,600 --> 00:53:09,320
So what we're doing right now is
we're seeing this push for more 

1106
00:53:09,320 --> 00:53:11,840
policy mechanisms. 
But at a certain point, if 

1107
00:53:11,840 --> 00:53:15,640
that's very successful, you can 
imagine a class between how we 

1108
00:53:15,640 --> 00:53:18,200
do, whether we do enhanced 
lettering in one way or in 

1109
00:53:18,200 --> 00:53:21,120
another way. 
And there's no, I don't think 

1110
00:53:21,120 --> 00:53:22,520
there's a simple answer to that 
either. 

1111
00:53:22,520 --> 00:53:25,320
But whether you're working with 
silicates or carbonates, what 

1112
00:53:25,320 --> 00:53:27,920
we're seeing is that the market,
the way the market has developed

1113
00:53:27,920 --> 00:53:30,480
so far, it's likely that 
potentially good projects are 

1114
00:53:30,480 --> 00:53:33,440
going to be left on the table 
from that decision alone. 

1115
00:53:34,000 --> 00:53:37,200
And it's hard to open the door 
to other things at scale, I 

1116
00:53:37,200 --> 00:53:40,040
think. 
But I think we used to be very 

1117
00:53:40,040 --> 00:53:42,520
clear, I think that we would be 
a mistake not to be exploring 

1118
00:53:42,520 --> 00:53:44,280
policy mechanisms. 
I just don't think that they're 

1119
00:53:44,280 --> 00:53:46,320
a silver bullet for the problems
that we're seeing right now in 

1120
00:53:46,320 --> 00:53:48,640
the market. 
Yeah, they're all good points. 

1121
00:53:49,440 --> 00:53:53,800
I love questions like this that 
touch upon the political economy

1122
00:53:54,040 --> 00:54:01,920
of decision making where like 
you can see this and how much 

1123
00:54:01,920 --> 00:54:05,120
permanence is necessary to 
qualify as durable carbon 

1124
00:54:05,120 --> 00:54:07,000
removal. 
And if you happen to work at a 

1125
00:54:07,000 --> 00:54:09,360
dot company, you probably think 
it's longer than someone who 

1126
00:54:09,360 --> 00:54:12,560
works at a biochar company. 
And you might not even know that

1127
00:54:12,840 --> 00:54:15,640
part of the reason why you think
that is because you know that 

1128
00:54:15,640 --> 00:54:19,120
you will harm your rivals and 
help your potential allies or 

1129
00:54:19,120 --> 00:54:21,520
your own business by thinking 
this. 

1130
00:54:22,160 --> 00:54:25,200
I think that's what makes this 
really difficult here too, is, 

1131
00:54:25,200 --> 00:54:30,120
you know, that once companies 
have money coming in, that is a 

1132
00:54:30,240 --> 00:54:32,960
downstream of important design 
decisions, like for registry 

1133
00:54:32,960 --> 00:54:37,280
says that oh, this process is 
actually at best net zero and is

1134
00:54:37,280 --> 00:54:40,200
not carbon removal. 
That has an enormous impact. 

1135
00:54:40,200 --> 00:54:43,160
And once you lock that in as oh,
this is actually carbon removal,

1136
00:54:43,160 --> 00:54:46,600
given how we've developed the 
system boundary changing that 

1137
00:54:46,600 --> 00:54:48,000
becomes politically very 
difficult. 

1138
00:54:48,000 --> 00:54:50,680
That registry might lose 
business, they might get sued. 

1139
00:54:50,840 --> 00:54:53,520
The project developers are often
backed by powerful venture 

1140
00:54:53,520 --> 00:54:56,680
capitalists who have connections
and, you know, wealth beyond 

1141
00:54:56,680 --> 00:54:58,760
many. 
And these decisions are no 

1142
00:54:58,760 --> 00:55:00,720
longer purely about the science 
or something else. 

1143
00:55:00,720 --> 00:55:01,960
It's all about political 
economy. 

1144
00:55:01,960 --> 00:55:06,000
And whose feathers can you 
effectively rustle and get away 

1145
00:55:06,000 --> 00:55:08,080
with it, even on the name of 
science? 

1146
00:55:08,840 --> 00:55:12,120
Gosh, I'm like, stressing myself
even talking about this, Tyler. 

1147
00:55:13,440 --> 00:55:15,840
But yeah, how are we supposed to
make good decisions given that 

1148
00:55:15,840 --> 00:55:19,560
those pressures exist for us? 
I think that like what where 

1149
00:55:19,560 --> 00:55:21,480
you're getting, where you're 
bringing my brain to is that 

1150
00:55:21,480 --> 00:55:24,160
like this is not a problem 
that's ever going to go away in 

1151
00:55:24,160 --> 00:55:27,920
carbon removal. 
How could it in enhanced 

1152
00:55:27,920 --> 00:55:30,200
weathering? 
Like I think what and across the

1153
00:55:30,200 --> 00:55:32,480
board, what we probably need is 
flexibility and foresight, 

1154
00:55:32,520 --> 00:55:34,200
right? 
You need the flexibility to 

1155
00:55:34,200 --> 00:55:38,440
build rules in such a way that 
don't make everything like that,

1156
00:55:38,440 --> 00:55:40,840
that don't rule out a bunch of 
viable projects and need the 

1157
00:55:40,840 --> 00:55:43,800
foresight to start investing in 
stuff before there's even like a

1158
00:55:43,800 --> 00:55:48,120
clear space or place for it in 
the market more broadly, or any 

1159
00:55:48,120 --> 00:55:50,920
kind of clear policy or broader 
support for that activity. 

1160
00:55:51,680 --> 00:55:54,320
And that's because like, as you 
mentioned, there's a bunch of 

1161
00:55:54,320 --> 00:55:57,240
things that just don't work now.
But we're not building carbon 

1162
00:55:57,240 --> 00:55:59,640
removal for like right now 
necessarily. 

1163
00:55:59,840 --> 00:56:02,640
We're building carbon removal 
for a decarbonized world. 

1164
00:56:02,640 --> 00:56:05,520
If you want carbon removal to, 
to balance hard to abate 

1165
00:56:05,520 --> 00:56:08,480
emissions and to, to neutralize 
legacy emissions, those are 

1166
00:56:08,480 --> 00:56:11,000
things that at least I think 
it's going to be very hard to 

1167
00:56:11,000 --> 00:56:13,480
accomplish that without mostly 
decarbonizing already. 

1168
00:56:13,480 --> 00:56:16,600
So if we're building out carbon 
removal infrastructure to be at 

1169
00:56:16,600 --> 00:56:19,800
scale in a decarbonized world, I
mean, we have path dependence 

1170
00:56:19,800 --> 00:56:22,800
problems built in because right 
now one of the biggest 

1171
00:56:22,800 --> 00:56:25,080
constraints on what carbon 
removal works and what carbon 

1172
00:56:25,080 --> 00:56:28,320
removal doesn't are the 
emissions of the non 

1173
00:56:28,320 --> 00:56:31,200
decarbonized sectors, right? 
So we're going to have to keep 

1174
00:56:31,200 --> 00:56:33,240
having this conversation over 
and over again. 

1175
00:56:33,400 --> 00:56:35,680
And the evolution of carbon 
removal over time is going to 

1176
00:56:35,680 --> 00:56:38,360
follow this like really used to 
queue in this path that just 

1177
00:56:38,680 --> 00:56:42,000
tracks whatever decarbonization 
is doing that might unlock new 

1178
00:56:42,000 --> 00:56:44,080
types of things that don't make 
any sense right now. 

1179
00:56:45,040 --> 00:56:48,640
And I think it's really hard to 
build things in a way that makes

1180
00:56:48,640 --> 00:56:51,840
it super easy for those things 
to reach their potential quickly

1181
00:56:52,080 --> 00:56:55,600
as decarbonization progresses, 
as new things become possible. 

1182
00:56:56,080 --> 00:56:58,480
Like, I don't know what the 
right answer is, but it's hard 

1183
00:56:58,480 --> 00:57:01,520
to build in flexibility early on
because it requires a lot of 

1184
00:57:01,520 --> 00:57:04,480
resources to build something 
that is flexible. 

1185
00:57:04,480 --> 00:57:05,800
You need to talk to a lot of 
experts. 

1186
00:57:05,800 --> 00:57:07,080
You need to do a lot of 
research. 

1187
00:57:07,280 --> 00:57:10,200
It's very easy to write rules 
and build infrastructure in a 

1188
00:57:10,200 --> 00:57:12,920
very defined way. 
And I just don't know how to 

1189
00:57:12,920 --> 00:57:18,280
balance like the need to, to 
build something at all with the 

1190
00:57:18,280 --> 00:57:20,880
need to build something that 
that we know needs to be 

1191
00:57:20,880 --> 00:57:22,880
flexible because this problem 
isn't going away. 

1192
00:57:22,880 --> 00:57:25,240
And it's not limited to enhance 
weathering. 

1193
00:57:28,200 --> 00:57:29,840
In some cases. 
I think there's like a story 

1194
00:57:29,840 --> 00:57:32,920
element to it. 
Like like, you know, if you're 

1195
00:57:32,920 --> 00:57:35,960
learning physics, you don't, you
don't start with like tensor 

1196
00:57:35,960 --> 00:57:39,440
calculus and relativity, right? 
You start with like spherical 

1197
00:57:39,440 --> 00:57:43,040
cows and frictionless planes. 
And that's kind of what's 

1198
00:57:43,040 --> 00:57:44,720
happening in enhanced rock 
weathering right now. 

1199
00:57:44,720 --> 00:57:47,320
We have a really nice story 
around silicates and silicates I

1200
00:57:47,320 --> 00:57:49,400
think are a simpler story to 
tell. 

1201
00:57:49,720 --> 00:57:52,080
But at a certain point you need 
to have room to like build the 

1202
00:57:52,080 --> 00:57:54,560
narrative out and learn more and
move on and expand our 

1203
00:57:54,560 --> 00:57:56,120
definition of enhanced rock 
weathering. 

1204
00:57:56,560 --> 00:58:00,440
And that narrative piece feels 
like kind of the first thing 

1205
00:58:00,440 --> 00:58:05,240
that needs to be solved in order
to build in flexibility into how

1206
00:58:05,560 --> 00:58:07,600
these different pathways evolve.
Like you need to be able to tell

1207
00:58:07,600 --> 00:58:10,240
a good story about why we want 
to go a different direction. 

1208
00:58:11,720 --> 00:58:13,360
And it's hard to tell those 
stories. 

1209
00:58:14,240 --> 00:58:17,040
For sure it is, and if you're 
able to do it, it's a lot of 

1210
00:58:17,040 --> 00:58:19,800
power one can wield by being an 
effective storyteller in this 

1211
00:58:19,800 --> 00:58:20,640
way. 
Totally. 

1212
00:58:21,440 --> 00:58:23,640
Oh. 
Tyler, thanks for teaching me 

1213
00:58:23,760 --> 00:58:26,600
science all the time. 
Like whenever we hang out, I 

1214
00:58:26,600 --> 00:58:28,880
just buttonhole you. 
I'm like, all right, what about 

1215
00:58:28,880 --> 00:58:33,240
this getting free, free 
explanations of scientific 

1216
00:58:33,240 --> 00:58:34,800
papers? 
I appreciate you. 

1217
00:58:34,920 --> 00:58:36,480
Oh, I feel like it goes both 
ways. 

1218
00:58:36,480 --> 00:58:38,840
I always appreciate when you're 
like, oh, well, this philosopher

1219
00:58:38,840 --> 00:58:41,200
says this one specific thing 
that's relevant to the way that 

1220
00:58:41,200 --> 00:58:43,720
we're progressing and carbon 
removal in this way. 

1221
00:58:44,720 --> 00:58:47,120
I my reading list has gotten so 
much longer through 

1222
00:58:47,120 --> 00:58:49,160
conversations with you and I do 
appreciate that. 

1223
00:58:50,760 --> 00:58:53,440
Complimentary skills, I think. 
Yeah, it's my pleasure. 

1224
00:58:53,560 --> 00:58:55,680
Thanks for coming back on. 
We should definitely do some 

1225
00:58:55,680 --> 00:58:57,240
more of this. 
Links to everything are in the 

1226
00:58:57,240 --> 00:58:59,600
show notes if you're listening, 
and we reference a bunch of 

1227
00:58:59,600 --> 00:59:02,800
different papers. 
Tyler sent me papers that help 

1228
00:59:02,880 --> 00:59:05,640
prep for this show that I'll put
links to in the show notes if 

1229
00:59:05,640 --> 00:59:09,000
you want more detail on this. 
Thanks again for being on Tyler.

1230
00:59:09,600 --> 00:59:10,800
Thank you Ross, it was a lot of 
fun.

