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FE4.8 - Ground Truthing
Episode 829th October 2022 • Future Ecologies • Future Ecologies
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Can we sequester our carbon and eat it too?

For the first time in 4 seasons, we're discussing natural climate solutions, and in particular, regenerative agriculture. Joining us is agrologist and fellow podcaster, Scott Gillespie (of Plants Dig Soil) to get into the nitty gritty of farming for soil carbon — its promise, possibility and feasibility.

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Transcripts

Introduction Voiceover:

You are listening to season four of

Introduction Voiceover:

Future Ecologies.

Mendel Skulski:

Okay, let's do it.

Adam Huggins:

Okay. I'm Adam.

Mendel Skulski:

Mendel.

Adam Huggins:

And this is future ecologies. And I'm here because

Adam Huggins:

Mendel invited me to be here to talk about natural climate

Adam Huggins:

solutions.

Mendel Skulski:

That's right.

Adam Huggins:

Which, which are...?

Mendel Skulski:

Which are, you know, a whole bunch of different

Mendel Skulski:

things. But they're basically all the ways that we can harness

Mendel Skulski:

natural ecosystems or natural processes to mitigate the

Mendel Skulski:

impacts of climate change.

Adam Huggins:

Yeah, basically non-technological solutions to

Adam Huggins:

sucking greenhouse gases out of the atmosphere.

Mendel Skulski:

Right.

Adam Huggins:

And this topic is all of the rage right now in

Adam Huggins:

climate circles, because well, because it's hopeful. And it

Adam Huggins:

promises to provide a way for us to restore ecosystems and to

Adam Huggins:

protect biodiversity and have benefits for human communities

Adam Huggins:

as well. All while sequestering lots of carbon.

Mendel Skulski:

Yeah, natural climate solutions are usually

Mendel Skulski:

pitched as this big win-win-win. And, you know, conveniently,

Mendel Skulski:

that pitch usually skips the part where governments or

Mendel Skulski:

industry have to reduce their own emissions.

Adam Huggins:

Yeah, it's always easier to promote and invest in

Adam Huggins:

something that doesn't require the powerful to make sacrifices.

Mendel Skulski:

Yeah. Although, you know, ideally, those

Mendel Skulski:

solutions are implemented in tandem with reductions in

Mendel Skulski:

greenhouse gases from human sources. It can't be either/or,

Mendel Skulski:

it's definitely a yes/and kind of situation.

Adam Huggins:

Yeah, we have to do all of it. And even though we

Adam Huggins:

did a whole set of seven episodes on the climate crisis a

Adam Huggins:

couple of years back —

Mendel Skulski:

— right, yeah. That's Scales of Change, for

Mendel Skulski:

newer listeners —

Adam Huggins:

we actually didn't talk much at all about natural

Adam Huggins:

climate solutions in that series. Did we even did we

Adam Huggins:

mention it?

Mendel Skulski:

No, I mean, it was supposed to be a series

Mendel Skulski:

about climate inaction. You know, and of course, we had to

Mendel Skulski:

sneak some action in there, too. But no, you're right. We really

Mendel Skulski:

didn't cover natural climate solutions. So we're here today

Mendel Skulski:

to redeem ourselves, and maybe generate some hate mail.

Adam Huggins:

Wait, wait, really?

Mendel Skulski:

Yeah.

Adam Huggins:

We don't want to do that.

Mendel Skulski:

No. You know, I just think that this is honestly

Mendel Skulski:

going to be one of the most controversial episodes we've

Mendel Skulski:

ever made.

Adam Huggins:

God, I hope not. I'm I'm actually really jazzed

Adam Huggins:

about natural climate solutions. And I'm so excited that I did a

Adam Huggins:

bunch of background research. I hope that's okay.

Mendel Skulski:

You're incorrigible. You're supposed to

Mendel Skulski:

be the blank slate for this one.

Adam Huggins:

It's hard for me to pretend to be the blank slate

Adam Huggins:

on the subject that I spent most of my time working on. Can I can

Adam Huggins:

I share with you what I found?

Mendel Skulski:

Sure.

Adam Huggins:

Okay, here we go. natural climate solutions tend

Adam Huggins:

to focus on enhancing the ability of natural processes to

Adam Huggins:

capture and store carbon in living biomass and in the soil.

Adam Huggins:

And also occasionally in rock, which we actually did talk a

Adam Huggins:

little bit about on Scales of Change. Anyway, we can sequester

Adam Huggins:

all this carbon by planting forests in places where they

Adam Huggins:

used to be, or where they could be — that's afforestation or

Adam Huggins:

reforestation. We could also protect and restore wetland

Adam Huggins:

ecosystems, and especially peatlands because they are so

Adam Huggins:

carbon rich.

Mendel Skulski:

Yeah.

Adam Huggins:

And finally, we can improve agricultural

Adam Huggins:

practices to store more carbon in crop and pasture lands.

Mendel Skulski:

Hey, guess what.

Adam Huggins:

What?

Mendel Skulski:

Today's episode is about that last one, storing

Mendel Skulski:

more carbon in agricultural soils.

Adam Huggins:

Nice. Okay. Well, in that case, one thing I

Adam Huggins:

learned about that is that there is huge potential for the

Adam Huggins:

agricultural approach. Like globally, but also in Canada

Adam Huggins:

specifically, I read a major study recently that was

Adam Huggins:

published earlier this year, and found that Canada currently

Adam Huggins:

stores about 20% of all global soil carbon.

Mendel Skulski:

Well, that's, that's actually more than I

Mendel Skulski:

expected. I mean, it is a huge country, but like a bunch of

Mendel Skulski:

that is in wetlands, right?

Adam Huggins:

Yeah, about a third of Canada's soil carbon is

Adam Huggins:

stored just in peatlands, which only cover about 12% of the land

Adam Huggins:

surface here. But you know, are a huge carbon sink. About half

Adam Huggins:

of that soil carbon is also in permafrost, you know,

Adam Huggins:

permanently frozen soils, which, as we've learned are a giant

Adam Huggins:

ticking climate time bomb.

Mendel Skulski:

Let's not go there.

Adam Huggins:

Let's not go there. But the rest is stored in

Adam Huggins:

other ecosystems. And just to put all of this in perspective,

Adam Huggins:

this is do that already estimated that over 20 gigatons

Adam Huggins:

of carbon are stored in living biomass in Canada,

Mendel Skulski:

Right, so like trees and shrubs and roots and

Mendel Skulski:

animals.

Adam Huggins:

Yep.

Mendel Skulski:

And by 20 gigatons you mean 20 billion

Mendel Skulski:

metric tons of carbon?

Adam Huggins:

Yeah, a gigaton is a billion tons, or about 10 to

Adam Huggins:

the 15th power of grams. A petagram, actually!

Mendel Skulski:

And that's a lot.

Adam Huggins:

Yeah, one gigaton of carbon is a lot. 20 bigatons

Adam Huggins:

is inconceivable. But um, you want to know how much is stored

Adam Huggins:

in the soil?

Mendel Skulski:

Hit me.

Adam Huggins:

Apparently, over 300 gigatons are stored in the

Adam Huggins:

top one meter of soil alone, here in Canada. And as much as

Adam Huggins:

260 more gigatons in the next meter down. So you know, 20

Adam Huggins:

gigatons in all of the living biomass in Canada, and over 15

Adam Huggins:

times that amount in the top one meter of soil alone.

Mendel Skulski:

Well, I have a statistic for you: the carbon

Mendel Skulski:

that used to be in the soil, and was lost due to agriculture over

Mendel Skulski:

the past 200 plus years.

Adam Huggins:

Oh, yeah? Lay it on me.

Mendel Skulski:

So this one is also an estimate, as are all

Mendel Skulski:

huge numbers. But worldwide, agriculture has released over

Mendel Skulski:

116 gigatons from the soil.

Adam Huggins:

Yeah... so there's lots of soil carbon in Canada.

Mendel Skulski:

Yeah. And lots of agricultural land in Canada.

Adam Huggins:

And it would follow then that this country

Adam Huggins:

probably accounts for a big chunk of those global soil

Adam Huggins:

losses.

Mendel Skulski:

Yeah. I mean, the areas that have been farmed

Mendel Skulski:

and grazed intensively in the past often have organic carbon

Mendel Skulski:

levels that are way, way below their ancient capacity. And you

Mendel Skulski:

can look all around the world, the places with the most intense

Mendel Skulski:

history of cultivation, are now the ones with the most degraded

Mendel Skulski:

soils

Adam Huggins:

And the least soil carbon.

Mendel Skulski:

Yeah. So today, we're not just talking about

Mendel Skulski:

keeping it in the ground, we're talking about putting it back.

Mendel Skulski:

From Future Ecologies, this is Ground Truthing.

Introduction Voiceover:

Broadcasting from the unseeded shared and

Introduction Voiceover:

asserted territories of the Musqueam, Squamish and

Introduction Voiceover:

Tsleil-Waututh, this is Future Ecologies: exploring the shape

Introduction Voiceover:

of our world, through ecology, design and sound.

Mendel Skulski:

Okay, so to sift through the story, I brought in

Mendel Skulski:

some help.

Scott Gillespie:

Hello!

Mendel Skulski:

Scott. Adam. Adam, Scott Gillespie.

Adam Huggins:

Hey, Scott, thanks for joining us.

Scott Gillespie:

Glad to be here.

Mendel Skulski:

So Scott is a professional agronomist in

Mendel Skulski:

southern Alberta, which is the traditional and present day home

Mendel Skulski:

of the people of the Blackfoot Confederacy.

Scott Gillespie:

Yeah.

Adam Huggins:

I've been to southern Alberta, but I don't

Adam Huggins:

think Future Ecologies has. Scott, would you help situate

Adam Huggins:

us?

Scott Gillespie:

Well as our local country singer, Corb Lund,

once put it:

we're East of the Rockies, and we're West of the

once put it:

rest. Right at the edge of what we call the prairies in Canada,

once put it:

or the plains in the United States: the great grasslands of

once put it:

North America.

Adam Huggins:

Well, for those of us who are even West-er, maybe

Adam Huggins:

you could tell us what it's like to be out there.

Scott Gillespie:

Yeah, well, as you can probably picture, trees

Scott Gillespie:

don't grow here naturally. It can be a place of intense winds

Scott Gillespie:

and extreme temperatures. Historically, it would have been

Scott Gillespie:

a pasture of huge herds of bison. And now it's been

Scott Gillespie:

converted to mostly agriculture in one form or another. So in my

Scott Gillespie:

area, which is in the south of the province, we live in what

Scott Gillespie:

the farmers here call the brown soil region.

Adam Huggins:

I love that. I love that you use the color of

Adam Huggins:

the soil to describe the character of the place that you

Adam Huggins:

live. What is it that makes the soils there Brown?

Scott Gillespie:

It's basically the fact that it's so dry here.

Scott Gillespie:

Over geological periods, we just don't get a lot of rain. So, not

Scott Gillespie:

a lot accumulates in the soil. As you go further north through

Scott Gillespie:

the province, you get more rainfall. And then you get into

Scott Gillespie:

what they call the dark brown soil, and then eventually you

Scott Gillespie:

get to the black soils, which are these beautiful rich soils —

Scott Gillespie:

that are full of organic material.

Adam Huggins:

Do I detect a bit of soil envy there in your

Adam Huggins:

voice, Scott?

Scott Gillespie:

Maybe a bit.

Mendel Skulski:

So Scott, maybe you should tell us what an

Mendel Skulski:

Agrologist is?

Scott Gillespie:

Okay. Well, the easiest way to think of it is if

Scott Gillespie:

you think of what a veterinarian does for animals, an Agrologist

Scott Gillespie:

does for plants and soils.

Mendel Skulski:

And you have your own podcast.

Scott Gillespie:

Yeah, Plants Dig Soil.

Mendel Skulski:

Where you help farmers practice something

Mendel Skulski:

called regenerative agriculture.

Scott Gillespie:

That's right.

Mendel Skulski:

And you know, I think we'll get into exactly

Mendel Skulski:

what that means later. But first, let's cover some basics.

Mendel Skulski:

Climate change is here. And it's happening faster and stronger

Mendel Skulski:

than almost anyone predicted. And as we all know, the main

Mendel Skulski:

molecular malefactor is of course...

Adam Huggins:

Carbon dioxide.

Scott Gillespie:

Yeah. And ultimately, the carbon causing

Scott Gillespie:

all these problems came from under our feet. The source of

Scott Gillespie:

the carbon that we hear the most about, and for good reason, is

Scott Gillespie:

fossil fuels. But it's not the only one. As you mentioned in

Scott Gillespie:

the intro, a significant chunk of human caused emissions came

Scott Gillespie:

from the soil itself.

Adam Huggins:

Right, yeah, living in the age of

Adam Huggins:

agriculture, we took — what... what was it, Mendel, 116?

Adam Huggins:

Yes.

Adam Huggins:

116 gigatons of carbon out of the soil. And that all went

Adam Huggins:

straight to the atmosphere.

Scott Gillespie:

Well, not quite, because it's not totally

Scott Gillespie:

clear how much of the carbon went back into the ocean, either

Scott Gillespie:

as dissolved carbon dioxide or unfortunately as dust from

Scott Gillespie:

topsoil erosion.

Adam Huggins:

Right... Yeah, erosion and ocean acidification.

Adam Huggins:

Neither of those are are good either.

Mendel Skulski:

No. But you know, together, we quantify

Mendel Skulski:

those losses and call them the "soil carbon debt": the carbon

Mendel Skulski:

that we owe back to the soil. You could basically say that we

Mendel Skulski:

cashed out millennia of carbon to grow our crops as quickly and

Mendel Skulski:

easily as we could.

Scott Gillespie:

Yeah. And there was even a belief among the

Scott Gillespie:

European colonists that with proper tillage, there was an

Scott Gillespie:

inexhaustible supply of plant nutrients — flowing up from the

Scott Gillespie:

deep. And because of a fluke of the climate, they happened to be

Scott Gillespie:

establishing these farms during a wet cycle, leading them to

Scott Gillespie:

think that plowing fields caused more rainfall.

Adam Huggins:

Wait, are you serious?

Scott Gillespie:

I'm serious.

Adam Huggins:

Does plowing cause rainfall?

Scott Gillespie:

No, it doesn't. But it all ended when the dry

Scott Gillespie:

cycle returned in the 1930s. So you might heard of the Dust

Bowl:

the topsoil was so depleted, it just simply blew

Bowl:

off the land.

Adam Huggins:

So here we are. And we're looking back at all of

Adam Huggins:

the damage caused by intensive agriculture and all of the

Adam Huggins:

carbon that's been released. And of course, the obvious question

Adam Huggins:

is, why don't we just put it back? Right? If if there's room

Adam Huggins:

in the ground for billions more tons of carbon, then

Adam Huggins:

theoretically, we could solve climate change and repay our

Adam Huggins:

weary soils at the same time. It's the obvious fix.

Mendel Skulski:

And that, plus the little wrinkle of feeding

Mendel Skulski:

the world —

Adam Huggins:

Right that, yeah, too

Mendel Skulski:

That's the dream of regenerative agriculture.

Mendel Skulski:

So regenerative agriculture means different things to

Mendel Skulski:

different people, at least in terms of what it looks like in

Mendel Skulski:

practice. But I think everyone would agree that the goal is

Mendel Skulski:

growing food, while simultaneously enriching, and

Mendel Skulski:

you know, that is returning carbon to the soil.

Adam Huggins:

Well, let's dig in. How does the carbon get into

Adam Huggins:

the soil? And how can we help?

Scott Gillespie:

Well, this is where things get more

Scott Gillespie:

complicated than we could ever cover in a single episode. So

Scott Gillespie:

let's just break it down to what we can understand at a couple

Scott Gillespie:

different levels.

Adam Huggins:

Sure. Yeah, that's par for the course for Future

Adam Huggins:

Ecologies.

Scott Gillespie:

So the first level is that there's only one

Scott Gillespie:

way to increase soil organic carbon: living growing plants.

Scott Gillespie:

So you could say, plants dig soil.

Adam Huggins:

Ya' could.

Scott Gillespie:

If you think about it, ultimately, the only

Scott Gillespie:

new carbon going into the soil is from the plants,

Adam Huggins:

Right. Primary production — classic ecology

Adam Huggins:

here. As opposed to animals and fungi, plants famously

Adam Huggins:

photosynthesize, and they use the sun's energy to turn carbon

Adam Huggins:

dioxide in the air into their own bodies. A thing, which, when

Adam Huggins:

I first learned, it, absolutely blew my mind because I thought

Adam Huggins:

they were building their bodies directly out of the soil. And it

Adam Huggins:

turns out, almost all of that is from the atmosphere. Totally

Adam Huggins:

freaking incredible.

Scott Gillespie:

And it's important to remember that those

Scott Gillespie:

bodies aren't just above ground where we can see them.

Scott Gillespie:

Generally, about a third of the mass of a plant, which is almost

Scott Gillespie:

all carbon is in its roots. So grasslands put more into their

Scott Gillespie:

roots, forests put more into the woody structures. But generally

Scott Gillespie:

30% is a good rule of thumb. So in a food system, there's a

Scott Gillespie:

portion that is harvested and exported off the land. Some of

Scott Gillespie:

that carbon will be eaten, and most of that will return to the

Scott Gillespie:

atmosphere with every human breath.

Adam Huggins:

But some of that harvest that you're talking

Adam Huggins:

about is is not going to make it into people's bodies and onto

Adam Huggins:

their tables. Because it's stuff like leaves and stems and husks

Adam Huggins:

and roots — stuff that we don't tend to eat as people, right?

Adam Huggins:

You have to grow a lot of plant material to get an ear of corn,

Scott Gillespie:

Right, and that carbon will get eaten by

Scott Gillespie:

something else. The first step is usually for grazing animals,

Scott Gillespie:

earthworms, or any other large critters of the soil to eat it.

Scott Gillespie:

And they break it down to a more manageable size for the main

decomposers:

fungi and bacteria.

Adam Huggins:

So you have the portion of the plant that we eat

Adam Huggins:

and respire, and you have the portion that, you know, passes

Adam Huggins:

through our bodies, of course. But everything else should be

Adam Huggins:

going back to the field that it was grown on, right?

Scott Gillespie:

So in theory, yes, but practically no. Most

Scott Gillespie:

food travels 1000s of kilometers, sometimes across

Scott Gillespie:

oceans. No one wants that back. If crop waste, food waste, or

Scott Gillespie:

humanure gets buried in landfill, you'll get a lot of

Scott Gillespie:

methaneÚ a greenhouse gas, it's 84 times worse than CO2. If

Scott Gillespie:

instead it gets composted, you'll still lose some of the

Scott Gillespie:

carbon to the air as those microbes eat and breathe. But

Scott Gillespie:

you can put a lot of it back onto the field.

Mendel Skulski:

Yeah, the problem is still that you need

Mendel Skulski:

to get it to a field, maybe not the original field that it grew

Mendel Skulski:

on. But any field nearby can benefit from this far better

Mendel Skulski:

than just putting it into a landfill. But the real trick is

Mendel Skulski:

getting that carbon to stay there.

Scott Gillespie:

Okay, then let's go to level two.

Mendel Skulski:

Level two!

Scott Gillespie:

The way the carbon from these plants

Scott Gillespie:

actually becomes part of the soil. As the plant grows, as

Scott Gillespie:

much as 25% of the carbon formed by photosynthesis is released as

Scott Gillespie:

a liquid by its roots. These liquids called root exudates —

Mendel Skulski:

Yeah, because they're exuding — roots exude

Scott Gillespie:

Yes. And these liquids feed the fungi and

Scott Gillespie:

exudates.

Scott Gillespie:

bacteria that live in the soil. Now, when I was in school, 20

Scott Gillespie:

years ago, it was thought that the roots were just leaky. Now

Scott Gillespie:

we know that they tune exactly what molecules they release:

Scott Gillespie:

they're trying to attract the fungi and bacteria that they

Scott Gillespie:

want hanging around the roots.

Adam Huggins:

That's so wild.

Scott Gillespie:

Now some of this liquid carbon will go right

Scott Gillespie:

back off as CO2 as the microbes use it for energy. But through a

Scott Gillespie:

complex series of symbiosis, this microbial ecosystem locks

Scott Gillespie:

in the carbon into clumps of solidified soil grains called

Scott Gillespie:

aggregates.

Adam Huggins:

Got it.

Scott Gillespie:

Now how long that carbon stays in the soil

Scott Gillespie:

depends on the stability of those aggregates, which may get

Scott Gillespie:

disturbed by earthworms, new roots moving through the soil,

Scott Gillespie:

tilling, droughts or floods.

Scott Gillespie:

Now how much carbon gets into soil depends on a huge number of

factors:

the amount of rain, the proportion of sand to clay, the

factors:

slope, the health and the diversity of all those microbes.

factors:

But the most important by far is simply the amount of

factors:

photosynthesis happening in the first place. The more green

factors:

growing plants, the better.

Adam Huggins:

Well, so far, none of this sounds particularly

Adam Huggins:

controversial to me.

Mendel Skulski:

I would say we're still on firm ground.

Mendel Skulski:

That's all pretty settled, if over-simplified soil science.

Mendel Skulski:

But the debate really starts to heat up when you wade into the

Mendel Skulski:

question of "what should we do about it?"

Adam Huggins:

People arguing about climate policy? I can't

Adam Huggins:

believe it.

Mendel Skulski:

This isn't the classic case of climate deniers

Mendel Skulski:

versus the world.

Adam Huggins:

No?

Mendel Skulski:

No. And you know, wouldn't bother making

Mendel Skulski:

this episode, if it were. The people on both sides of this

Mendel Skulski:

debate really just want the same thing. And that's carbon

Mendel Skulski:

drawdown and food security. Where their opinions differ is

Mendel Skulski:

whether we can count on soil carbon sequestration to get us

Mendel Skulski:

there.

Scott Gillespie:

Ss in, should we pay farmers for adding carbon

Scott Gillespie:

to their soils?

Adam Huggins:

Oh, okay. So now we're talking, I think, about

Adam Huggins:

carbon credits. Which are, you know, market solutions for

Adam Huggins:

market problems. Am I right?

Mendel Skulski:

Yeah. Well, I'm actually still on the fence

Mendel Skulski:

about it. Because farming at scale is really expensive, and

Mendel Skulski:

the margins can be razor thin. You know, for a farmer, any

Mendel Skulski:

little change in behavior can mean tens of thousands of

Mendel Skulski:

dollars up front, without any guarantee of success at the end

Mendel Skulski:

of the season. So if we want to make our food system less

Mendel Skulski:

destructive, we need to find a way to help farmers make the

Mendel Skulski:

leap. But then again, if we're going to pay for that carbon, we

Mendel Skulski:

better be damn sure it's real.

Scott Gillespie:

And that's the root of the debate. Selling

Scott Gillespie:

carbon credits can lock farmers into complicated contracts that

Scott Gillespie:

may or may not make financial sense to them. It might give

Scott Gillespie:

polluters the excuse to continue their business as usual,

Scott Gillespie:

canceling out the climate benefits, or even worse, the

Scott Gillespie:

soil carbon backing those credits might not be there at

Scott Gillespie:

all.

Adam Huggins:

Wait, what do you — what do you mean?

Mendel Skulski:

Scott? Are you ready?

Scott Gillespie:

Yep.

Mendel Skulski:

Ring the bell, cuz we've got a list.

Adam Huggins:

Did I miss something? Like, do we have a

Adam Huggins:

segment called "Ring the bell, read a list"?

Mendel Skulski:

Just go with it.

Scott Gillespie:

Okay, so there's four things that are

Scott Gillespie:

good carbon credit has to represent: additionality,

Scott Gillespie:

non-reversal, lack of leakage, and permanence.

Scott Gillespie:

Additionality means that we want the carbon to be sequestered

Scott Gillespie:

because of the credit incentive. That is, it's additional to our

Scott Gillespie:

baseline.

Adam Huggins:

Right, the business as usual scenario. So

Adam Huggins:

for it to have any benefit to the climate, it has to go above

Adam Huggins:

and beyond the status quo.

Mendel Skulski:

Exactly. And then there's non-reversal, which

Mendel Skulski:

means that those credits also have to contend with that

Mendel Skulski:

temperamental flux that is soil carbon, either by a change in

Mendel Skulski:

farming practices or, you know, uncontrollable factors, like a

Mendel Skulski:

change in the climate.

Adam Huggins:

Can you imagine?

Mendel Skulski:

Right? It could cause that carbon to go from

Mendel Skulski:

being locked up in soil aggregates, to right back up in

Mendel Skulski:

the atmosphere.

Scott Gillespie:

Yeah now, farmers aren't generally on the

Scott Gillespie:

hook for reversals outside of their control. But it does raise

Scott Gillespie:

questions about what happens down the line. In Canada and the

Scott Gillespie:

United States, approximately one half of farmers rent the land

Scott Gillespie:

they farm on. They can't guarantee how the next tenant

Scott Gillespie:

will treat the soil.

Mendel Skulski:

No. And landlords and owner operators

Mendel Skulski:

might also feel conflicted about signing contracts. What if an

Mendel Skulski:

opportunity for a lucrative cash crop comes along, you know, five

Mendel Skulski:

or 10 years later, but the practices of farming it go

Mendel Skulski:

against the sequestering of carbon?

Adam Huggins:

Right, I'm starting to get a sense of how

Adam Huggins:

this could be complicated.

Scott Gillespie:

Well, then meet leakage. leakage is when a

Scott Gillespie:

climate positive action in one place causes a climate negative

Scott Gillespie:

effect somewhere else.

Mendel Skulski:

Say for instance, if (and this is a

Mendel Skulski:

contentious if) regenerative farming practices results in

Mendel Skulski:

lower food yields, than the market would put pressure on

Mendel Skulski:

other farmers to convert yet more land, perhaps by clearing a

Mendel Skulski:

productive forest or prairie.

Adam Huggins:

Yeah, nobody wants leakage. Now, not only would

Adam Huggins:

that be outside of the carbon farmers control, they might not

Adam Huggins:

even know about it, right? Like you're talking about a systemic

Adam Huggins:

pressure because of the price of food or or land.

Scott Gillespie:

Yeah, you've got it. And finally, there's

Scott Gillespie:

permanence.

Mendel Skulski:

So permanence is kind of related to reversal, but

Mendel Skulski:

it's about the time horizon. We've been talking about how

Mendel Skulski:

carbon naturally cycles through plants, the soil, the air. But

Mendel Skulski:

if our concern is reducing greenhouse gases, we really want

Mendel Skulski:

that carbon locked away for as long as possible. Ideally, on

Mendel Skulski:

geological timescales, like the fossil fuels it mostly came

Mendel Skulski:

from. In the world of carbon credits, that target is usually

Mendel Skulski:

set somewhat arbitrarily, at 100 years.

Scott Gillespie:

And outside of places like bogs —

Adam Huggins:

We love a bog

Scott Gillespie:

— it's just really hard to know where that

Scott Gillespie:

carbon will be in a century. Think about the land around you,

Scott Gillespie:

and what it looked like 100 years ago. I bet its quite a bit

Scott Gillespie:

different than what it looks like today.

Adam Huggins:

Yeah, so that's a lot that any legitimate soil

Adam Huggins:

carbon credit would have to account for.

Mendel Skulski:

Yeah, no kidding.

Adam Huggins:

So how do we actually do that? Like, how...

Adam Huggins:

how do you prove that any of that is working? That you have,

Adam Huggins:

let me see hold on... additional carbon, that is not reversing

Adam Huggins:

itself back into the atmosphere, and isn't leaking out somewhere,

Adam Huggins:

because it's permanent.

Mendel Skulski:

We'll get to that... after the break.

Mendel Skulski:

Hey, me again — here to tell you that this episode is sponsored

Mendel Skulski:

by... you.

Mendel Skulski:

You make Future Ecologies possible by sharing it with the

Mendel Skulski:

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Mendel Skulski:

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Mendel Skulski:

guest producers and 20 musicians, not even including

Mendel Skulski:

Adam and myself. I'm so proud that we can pay all of those

Mendel Skulski:

people for their work. And we can do so because of our

Mendel Skulski:

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And so I wanted to remind you that it's just us. No parent

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Mendel Skulski:

Okay, I'm Mendel. That's Adam.

Adam Huggins:

Hey.

Mendel Skulski:

We're joined by Scott.

Scott Gillespie:

Hello.

Mendel Skulski:

And today on Future Ecologies, we're talking

Mendel Skulski:

about the promise of soil carbon sequestration, or how we could

Mendel Skulski:

use food-producing land to fight climate change.

Scott Gillespie:

Well, I wouldn't say the promise, but

Scott Gillespie:

rather the possibility. And in practice, that might be a whole

Scott Gillespie:

lot different from the feasibility.

Adam Huggins:

Right. I mean, basically, I came here, super

Adam Huggins:

stoked to talk about natural climate solutions, and you guys

Adam Huggins:

are just raining on my parade.

Mendel Skulski:

Yes.

Adam Huggins:

So to recap, we know in theory that the soil

Adam Huggins:

could hold as much carbon, at least, as we've taken out of it

Adam Huggins:

since the agricultural revolution, which was how much

Adam Huggins:

again?

Mendel Skulski:

116 gigatons.

Adam Huggins:

Yeah, that's a lot. But because that carbon

Adam Huggins:

doesn't like to sit still — it likes to flow through plants and

Adam Huggins:

microbes, and then back up into the air, and it might even leak

Adam Huggins:

out somewhere else because of pressures on land use —

Adam Huggins:

actually, keeping it in the ground is a lot easier said than

Adam Huggins:

done.

Mendel Skulski:

Exactly. But that's not to say we can't do

Mendel Skulski:

it. Regenerative ag as it's practiced today is really just a

Mendel Skulski:

repackaging of different traditional agricultural

Mendel Skulski:

techniques from all around the world: Cover cropping,

Mendel Skulski:

composting, no till or low till, biochar, agroforestry matrix

Mendel Skulski:

planting, silvopasture... none of these are new ideas. And

Mendel Skulski:

they're all known to build soil and turn it dark and rich,

Mendel Skulski:

basically packed with organic carbon.

Scott Gillespie:

That's true. But proving it, and selling it

Scott Gillespie:

by the ton? That's another story. And it brings us into the

Scott Gillespie:

realm of MRV.

Adam Huggins:

We love a good acronym. What is MRV?

Scott Gillespie:

Measurement, reporting and verification.

Scott Gillespie:

Basically, accounting and auditing in the world of carbon

Scott Gillespie:

sequestration.

Adam Huggins:

Please tell me this didn't turn into an episode

Adam Huggins:

about accounting.

Mendel Skulski:

How about we just focus on that one key

aspect:

measurement. To know how much carbon any intervention

aspect:

helped add to the soil, first, you have to measure how much

aspect:

carbon is there already.

Adam Huggins:

Sure, yeah.

Mendel Skulski:

And that's not easy, or cheap.

Scott Gillespie:

Because so carbon is not a simple compound

Scott Gillespie:

to measure, like, say CO2. Organic chemistry is an entire

Scott Gillespie:

scientific discipline studying all the compounds that carbon

Scott Gillespie:

can make.

Adam Huggins:

Can I just say that was the best summary of

Adam Huggins:

organic chemistry that I've ever heard? Even after studying it

Adam Huggins:

for a couple years.

Scott Gillespie:

Well, thanks. So because carbon can take all

Scott Gillespie:

those different forms. And because soil is really variable,

Scott Gillespie:

and heterogeneous, on a landscape scale, carbon can be

Scott Gillespie:

incredibly patchy. So you need to sample enough points to get

Scott Gillespie:

good data. Sample too few, and you might be getting the wrong

Scott Gillespie:

picture. Sample too many, and you're just wasting time and

Scott Gillespie:

money.

Mendel Skulski:

And by sample, we mean physically going into

Mendel Skulski:

the field and getting a soil core. That is, like, drilling

Mendel Skulski:

out a tube of dirt, and then shipping it off to a lab to be

Mendel Skulski:

analyzed. Every single core is at least a few minutes of work.

Scott Gillespie:

Provided you don't hit a rock.

Mendel Skulski:

Yeah. Plus all the logistics and expenses

Mendel Skulski:

around the lab analysis.

Adam Huggins:

I mean, I've done soil sampling before and it's

Adam Huggins:

it's not that hard. But I've also only done it on like small

Adam Huggins:

areas of land.

Scott Gillespie:

Well consider that the Canadian Prairies alone

Scott Gillespie:

have 77 million acres of farmland. Most city blocks are

Scott Gillespie:

just a few acres in size.

Mendel Skulski:

Yeah, it really all adds up.

Adam Huggins:

Well, that's not great. Is that really the best

Adam Huggins:

option that we have?

Mendel Skulski:

There are a few promising new technologies. But

Mendel Skulski:

right now, none of them are ready for primetime. Some folks

Mendel Skulski:

are aiming to use satellites, you know, so called remote

Mendel Skulski:

sensing to measure soil carbon en mass. Some are using these

Mendel Skulski:

meteorological stations that are called eddy towers to calculate

Mendel Skulski:

the carbon flux at this landscape level. And then

Mendel Skulski:

there's others who are developing tools that can

Mendel Skulski:

measure the carbon right there in the field, instead of a soil

Mendel Skulski:

core — using a probe that basically detects the color of

Mendel Skulski:

the dirt.

Adam Huggins:

Right like brown, dark brown and black.

Scott Gillespie:

Exactly. Color can be a decent proxy for the

Scott Gillespie:

amount of organic carbon in the soil. And all of these tools

Scott Gillespie:

will be used to improve computational models so that we

Scott Gillespie:

can better predict what's happening to the carbon, and

Scott Gillespie:

then use the magic of statistics. So we don't need to

Scott Gillespie:

take as many physical samples.

Mendel Skulski:

Yeah, real magic. They've got incantations,

Mendel Skulski:

like regionalised variables and conditioned Latin Hypercube

Mendel Skulski:

sample design.

Adam Huggins:

That's real Arcana. It's almost like you

Adam Huggins:

want to explain a thing?

Mendel Skulski:

I don't.

Adam Huggins:

Okay, so you're saying that these techniques are

Adam Huggins:

good enough for the kinds of large estimates we've been

Adam Huggins:

throwing around in this episode so far, but not necessarily good

Adam Huggins:

enough to be sure that we are selling a certain amount of

Adam Huggins:

carbon when we're making carbon credits.

Scott Gillespie:

No. And there might be one more problem.

Mendel Skulski:

And it's a big one.

Mendel Skulski:

So the way soil carbon is measured, now, those samples are

Mendel Skulski:

usually taken from the top 30 centimeters —

Adam Huggins:

That's one foot for those of you who think like

Adam Huggins:

me.

Mendel Skulski:

And you know, that's because the deeper you

Mendel Skulski:

go, the more expensive and challenging it gets. Try pushing

Mendel Skulski:

a probe into the soil, you know, like you said, the top is kind

Mendel Skulski:

of easy. But the deeper you go, the more pressure it takes,

Mendel Skulski:

almost exponentially.

Scott Gillespie:

I've done a lot of soil sampling over the years.

Scott Gillespie:

And I can definitely attest to that. Soil sampling is typically

Scott Gillespie:

done with hydraulic probes mounted to pickup trucks, and

Scott Gillespie:

the force is enough to lift the truck or bend the probe if

Scott Gillespie:

you're not careful.

Adam Huggins:

Wow, okay. But why go deeper? Isn't the top foot of

Adam Huggins:

the soil where most of the roots and microbes are anyway?

Scott Gillespie:

That's mostly true, but some roots go two or

Scott Gillespie:

three times that deep. In the case of prairie grasses, 10

Scott Gillespie:

times or more. And of course, in other places, the subsoils can

Scott Gillespie:

and will be a completely different situation.

Mendel Skulski:

And there's a growing body of evidence that

Mendel Skulski:

when we only measure carbon sequestration in the topsoil,

Mendel Skulski:

we're only getting a little slice of the whole picture,

Adam Huggins:

Right — those estimates that we covered at the

Adam Huggins:

beginning of the episode, were all about how the deep soils are

Adam Huggins:

a big part of the carbon stocks for Canada.

Scott Gillespie:

But those were just estimates, not field by

Scott Gillespie:

field measurements. What Mendel is talking about is a particular

Scott Gillespie:

study that looked at how soil organic carbon accumulated with

Scott Gillespie:

and without cover cropping, and a variety of inputs like

Scott Gillespie:

chemical fertilizers and compost. What was important

Scott Gillespie:

about this study is that it was long term, most studies only

Scott Gillespie:

last the length of a grad student's degree, which is about

Scott Gillespie:

two to four years,

Adam Huggins:

Not exactly the timescale of soil formation.

Adam Huggins:

That would be a PhD.

Scott Gillespie:

No, but we can do a little better. In this

Scott Gillespie:

study, soil samples had been taken over 19 years. And various

Scott Gillespie:

combinations of cover crops, irrigation, synthetic

Scott Gillespie:

fertilization, and compost were kept consistent over that time.

Scott Gillespie:

Unlike your typical 30-centimeter cores, these ones

Scott Gillespie:

went two meters down, with five sample points over that depth.

Adam Huggins:

That's uh... that's hardcore? Hard... deep

Adam Huggins:

core? Anyway, deep cores, long duration, different field

Adam Huggins:

variables, I'm with you.

Scott Gillespie:

So when no inputs were added to the system,

Scott Gillespie:

and no cover crops were planted, carbon in the topsoil is

Scott Gillespie:

decreased. Exporting food off the land meant that the microbes

Scott Gillespie:

needed to break apart their savings of long term carbon for

Scott Gillespie:

nutrients.

Adam Huggins:

As you'd expect.

Scott Gillespie:

Now, you remember how we talked about

Scott Gillespie:

that to build organic matter, we need more plants growing. Cover

Scott Gillespie:

crops are a way to achieve this in a farming system by growing

Scott Gillespie:

something in the shoulder season. Before and after the

Scott Gillespie:

cash crop. It's one of the key practices in regenerative

Scott Gillespie:

systems, because it helps to build the soil.

Adam Huggins:

Right. Yeah, I do this in my garden, too.

Scott Gillespie:

Yeah, so when winter cover crops were added to

Scott Gillespie:

the conventional system — as in a system that uses synthetic

Scott Gillespie:

fertilizers and pesticides — in this particular study, the top

Scott Gillespie:

soil saw a statistically significant increase in soil

Scott Gillespie:

organic carbon.

Adam Huggins:

So far, so good.

Scott Gillespie:

But the rest of the soil down to meters had a

Scott Gillespie:

statistically significant decrease in carbon. When looking

Scott Gillespie:

across the whole profile. They saw not only less sequestration,

Scott Gillespie:

but net positive emissions on the fields with cover crops.

Adam Huggins:

Wait, what?

Mendel Skulski:

Scary, right? That means what we typically

Mendel Skulski:

perceive as carbon sequestration might actually just be carbon

Mendel Skulski:

concentration in the top layer of the soil. And because of how

Mendel Skulski:

much more massive the subsoil is, there may still be

Mendel Skulski:

significant net carbon losses overall.

Adam Huggins:

So what you're saying is that when we're just

Adam Huggins:

measuring the first foot or so of the soil, we might fool

Adam Huggins:

ourselves into thinking that we're sequestering carbon, when

Adam Huggins:

in reality, it could be the exact opposite.

Scott Gillespie:

You got it. But just to be clear, having this

Scott Gillespie:

carbon concentrated near the surface isn't bad. That

Scott Gillespie:

particular crop system was doing this naturally. And so there's

Scott Gillespie:

probably a reason why it wants to carbon there. After all,

Scott Gillespie:

that's where most of the roots are. That's where the moisture

Scott Gillespie:

is. And that's where the microbes live. So it's good for

Scott Gillespie:

the farmer, just not so good if you think you're sequestering

Scott Gillespie:

carbon.

Adam Huggins:

What about adding compost? Like to the study,

Adam Huggins:

consider what happens if you're adding compost to the fields.

Scott Gillespie:

In that case, the carbon did increase overall.

Scott Gillespie:

But zooming out, that's essentially the result of

Scott Gillespie:

leakage from somewhere else. If that compost didn't go back to

Scott Gillespie:

the field that produced it, you've just transferred carbon

Scott Gillespie:

from one area to the other.

Mendel Skulski:

Basically more like carbon import, rather than

Mendel Skulski:

carbon sequestration.

Adam Huggins:

Yeah, that's a pretty sobering study. Thank you

Adam Huggins:

for, you know, hitting me with it three quarters of the way to

Adam Huggins:

this episode. So I guess, you know, what that makes me think

Adam Huggins:

is that when we're talking about, you know, trying to sell

Adam Huggins:

that carbon or allowing it to be used as an offset for big

Adam Huggins:

industrial emitters, there's a real risk here that that's a

Adam Huggins:

wasted investment, or it can actually actively make things

Adam Huggins:

worse.

Mendel Skulski:

Yeah. What it really means is that we still

Mendel Skulski:

have so much left to learn about the dynamics of deep soil. And

Mendel Skulski:

then we need to factor that into our models. And so this is

Mendel Skulski:

really where the problem lies. There's, there's a lot of hype,

Mendel Skulski:

because of models that show big changes. But you dig a little

Mendel Skulski:

deeper, and you see that most of them only go down 30

Mendel Skulski:

centimeters, and sometimes less. As of right now, they can't say

Mendel Skulski:

what happened in the subsoil. They can only say what happened

Mendel Skulski:

near the surface.

Scott Gillespie:

Yeah. And maybe eventually we'll develop an

Scott Gillespie:

understanding of how to lock huge climate shifting amounts of

Scott Gillespie:

carbon down into those deep soils, and find them at the same

Scott Gillespie:

time. And do it on a timescale that is much faster than how

Scott Gillespie:

long it took for those soils to form. But for now, we really

Scott Gillespie:

can't count on it.

Adam Huggins:

Well, thanks, you two, for a hopeful and uplifting

Adam Huggins:

episode. There's nothing I love more than pouring cold water on

Adam Huggins:

a natural climate solution. That's what I'm here for.

Mendel Skulski:

Yeah, yeah, I would say it's our pleasure.

Mendel Skulski:

But, you know...

Adam Huggins:

So, um, I guess to ask, you know, the obvious

Adam Huggins:

question, what now? We're, as a society, kind of banking on the

Adam Huggins:

soil being a part of our climate solution, and especially

Adam Huggins:

agricultural lands. Does this mean that we just give up on

Adam Huggins:

that dream? Do we give up on regenerative agriculture?

Mendel Skulski:

No, no, I don't think we should. Regenerative ag

Mendel Skulski:

can do a whole world of good — especially now, especially

Mendel Skulski:

during climate disruption. But, you know, in order to realize

Mendel Skulski:

that, we, I think we have to expand our focus right? Out from

Mendel Skulski:

just carbon and from carbon markets.

Scott Gillespie:

Yeah, if all we care about is carbon, we're

Scott Gillespie:

gonna miss the forest for the trees.

Adam Huggins:

It's funny you saying that coming from a place

Adam Huggins:

with no trees at all.

Scott Gillespie:

Okay, then how about missing the prairie for

Scott Gillespie:

the grasses?

Mendel Skulski:

or the roots for the exudates?

Adam Huggins:

That's acceptable.

Scott Gillespie:

Anyhow, one thing is indisputable,

Scott Gillespie:

regenerative farming is still a good thing. All those

Scott Gillespie:

regenerative practices can make a soil system more resilient to

Scott Gillespie:

climate extremes, helping water filter in slowly to manage big

Scott Gillespie:

rains, holding on to it longer to last through droughts, and

Scott Gillespie:

just generally increasing resistance to pests and erosion.

Scott Gillespie:

What farmer wouldn't want that?

Adam Huggins:

I mean, I want that I want that on my land.

Adam Huggins:

And there's a bunch of other natural climate solutions for

Adam Huggins:

agricultural lands that I think do have a more guaranteed

Adam Huggins:

delivery in terms of carbon sequestration. I'm talking about

Adam Huggins:

planting more trees on agricultural lands as riparian

Adam Huggins:

buffers, or as hedgerows, or as silvopasture, or agroforestry,

Adam Huggins:

right? Getting that woody biomass in there. That's going

Adam Huggins:

to do a world of good in some places, in other places, just

Adam Huggins:

doing leguminous cover crops to help reduce the amount of

Adam Huggins:

nitrogen fertilizer that's applied to the land is a huge

Adam Huggins:

benefit. Because a bunch of the nitrogen fertilizer that people

Adam Huggins:

apply ends up in the atmosphere as nitrous oxide, which is a

Adam Huggins:

greenhouse gas that's 300 times as potent as carbon dioxide. So

Adam Huggins:

there is a whole suite of practices that are still

Adam Huggins:

beneficial for the soil and for the farmer and for the climate.

Mendel Skulski:

Yeah, yeah, I think all of these things add up

Mendel Skulski:

to huge benefits in water quality and ecosystem health in

Mendel Skulski:

general. And, you know, hopefully still, food

Mendel Skulski:

production. And, you know, practically speaking some of

Mendel Skulski:

those regenerative practices —they might feel more within

Mendel Skulski:

reach, like winter cover cropping or reducing tillage to

Mendel Skulski:

the minimum. Others would mean a pretty complete reimagining of

Mendel Skulski:

how we plant and harvest at scale, and what those fields

Mendel Skulski:

look like, like what you just described. But with agricultural

Mendel Skulski:

systems and practices so deeply ingrained, you know, I really

Mendel Skulski:

think that farmers need help to try something new,

Adam Huggins:

And podcasters of the world are here to provide

Adam Huggins:

it.

Mendel Skulski:

Yeah, I mean, podcasters, and governments and

Mendel Skulski:

people who eat food, right?

Adam Huggins:

Yeah, I am a podcast. I'm not a government.

Adam Huggins:

But I am a person who eats food, I think we are all people who

Adam Huggins:

eat. And so we all play some part in our food systems. One

Adam Huggins:

thing I have learned farming is that every farm is different.

Adam Huggins:

And so I guess the regenerative practices that are going to make

Adam Huggins:

sense in one place will be different, depending on the

Adam Huggins:

farm. What do you think the farmers in your area need,

Adam Huggins:

Scott, in order to be able to embrace regenerative practices?

Adam Huggins:

What are you seeing?

Scott Gillespie:

To me, I think the most critical thing is that

Scott Gillespie:

there has to be some type of economic reason to do it.

Adam Huggins:

Like a carbon credit?

Scott Gillespie:

Well, I had hopes in the carbon credit...

Scott Gillespie:

until I did so much research on this, that it doesn't look like

Scott Gillespie:

that's going to be a viable solution. So it needs to be

Scott Gillespie:

something else. Even just incentives to start to get over

Scott Gillespie:

that initial hump in adoption would be a critical thing.

Scott Gillespie:

Realistically, it's going to have to be something that's

Scott Gillespie:

going to make economic sense to the farm. And as an example, in

Scott Gillespie:

the United States, where cover crops have really taken off is

Scott Gillespie:

where they had weeds that were resistant to the herbicides and

Scott Gillespie:

their costs were just getting out of control. When they were

Scott Gillespie:

able to integrate the cover crops in they're able to bring

Scott Gillespie:

their cost down. So whether you're farming at a small scale,

Scott Gillespie:

like a market garden, or up to thousands and thousands of

Scott Gillespie:

acres, it comes down to economics.

Mendel Skulski:

Yeah. And that's something that doesn't have to

Mendel Skulski:

come from the potentially greenwashing and, you know,

Mendel Skulski:

supposedly outcome based world of carbon offsets.

Scott Gillespie:

Yeah, there's things like crop insurance, low

Scott Gillespie:

interest loan programs, or just straight up cash incentives for

Scott Gillespie:

regenerative practices — that can help farmers close the gap

Scott Gillespie:

between doing good for their soil, making a living, and

Scott Gillespie:

putting food on all our tables. And I'm happy to say there's all

Scott Gillespie:

sorts of these programs starting to crop up.

Adam Huggins:

You made a pun, Scott. That's delightful. That's

Adam Huggins:

usually my job here. What kinds of regenerative practices are

Adam Huggins:

you seeing being implemented in the prairies where you live?

Scott Gillespie:

Well, the huge shift over the last quite a few

Scott Gillespie:

decades has been going to no till or at least minimum

Scott Gillespie:

tillage. So plowing is very rare in the prairies. And very

Scott Gillespie:

similar to cover crops, it is showing similar patterns of

carbon concentration:

in that we do get more carbon in the upper

carbon concentration:

levels, but not as much in the deeper levels. However, just

carbon concentration:

because that happens, doesn't mean that it's not a good

carbon concentration:

practice for the farmer. They're seeing a lot of benefits from

carbon concentration:

it.

Adam Huggins:

Yeah. So some incentivization is important.

Adam Huggins:

Like stepping back from this question about carbon credits,

Adam Huggins:

what occurs to me is that this whole question of how much

Adam Huggins:

carbon is being sequestered, and how do we measure that, and how

Adam Huggins:

permanent is that... it's a lot of complexity and noise that

Adam Huggins:

we've kind of, like, shoved into what could otherwise be a very

Adam Huggins:

simple conversation. Which is that we know that as a society,

Adam Huggins:

we are emitting too much carbon. We should be making the people

Adam Huggins:

that are emitting all that carbon pay. And then we should

Adam Huggins:

be taking that money and incentivizing the practices that

Adam Huggins:

we want to see on farms and elsewhere. And we don't

Adam Huggins:

necessarily have to quantify that as stringently as we are,

Adam Huggins:

if we're not counting on the slimmest of margins for climate

Adam Huggins:

recovery. If we aren't trying to, you know, finely balance the

Adam Huggins:

amount that we're emitting versus the amount that we're

Adam Huggins:

sequestering, right? If the general idea is "emit less,

Adam Huggins:

sequester more", then we need to reduce emission, which we we

Adam Huggins:

definitely know how to do that. And then incentivize practices

Adam Huggins:

that we know will eventually sequester carbon, even if we

Adam Huggins:

don't know exactly how much or over what kind of timespan

Adam Huggins:

that's going to happen. Do you know what I mean?

Mendel Skulski:

Yeah, I mean, you're saying like, not on a

Mendel Skulski:

gram by gram, or or ton by ton basis, but just to tax polluters

Mendel Skulski:

and use that to subsidize regenerative agriculture or

Mendel Skulski:

agriculture in general.

Adam Huggins:

Yeah, I mean, farming is already heavily

Adam Huggins:

subsidized. It's a question of shifting those subsidies to

Adam Huggins:

actually support the kinds of practices that we want to see as

Adam Huggins:

as a society, I think.

Mendel Skulski:

Totally. And, you know, while we do that, I

Mendel Skulski:

think we just need to get comfortable with the fact that

Mendel Skulski:

we're still learning. We're learning that there's a lot more

Mendel Skulski:

left to learn — about soil especially.

Scott Gillespie:

Yeah.

Mendel Skulski:

We know now that plowing doesn't make it rain,

Mendel Skulski:

that soil nutrients don't just spontaneously appear, and that

Mendel Skulski:

plants build their bodies from the air and not the ground.

Adam Huggins:

Yeah.

Mendel Skulski:

But despite how far we've come, we're really

Mendel Skulski:

still just at the beginning of a soil science revolution. And

Mendel Skulski:

we're overturning notions that have been in place for decades,

Mendel Skulski:

you could say some recalcitrant ideas. At some level, we know

Mendel Skulski:

it's possible to put a lot of carbon back in the soil, because

Mendel Skulski:

it was there once. But now we also know that there's a lot of

Mendel Skulski:

work to be done before soil carbon can be the silver bullet

Mendel Skulski:

we've been hoping for.

Mendel Skulski:

But that doesn't mean we just wait around in the meantime. We

Mendel Skulski:

already have the tools we need to change how we farm and how we

Mendel Skulski:

eat, to rebuild the soil in the places where it's the most

Mendel Skulski:

degraded, and to do whatever we can to regrow a livable planet.

Adam Huggins:

Okay, so if I understand you to correctly, the

Adam Huggins:

regenerative practices that we've been discussing this whole

Adam Huggins:

episode are good for the soil, they're good for farmers, and

Adam Huggins:

they're very likely good for the climate, at least in the long

Adam Huggins:

term. But we don't yet have the deep understanding of soil

Adam Huggins:

processes required for us to confidently predict and quantify

Adam Huggins:

those benefits, at least, enough to think that we can start

Adam Huggins:

selling them to each other or to people who are going to use them

Adam Huggins:

as an excuse to pollute, maybe. Is that right?

Mendel Skulski:

Yeah, that's about it.

Scott Gillespie:

And to close things out, I just wanted to

Scott Gillespie:

paraphrase a paper on overcoming the barriers to adoption of

Scott Gillespie:

cover cropping, since I think it also applies to all sorts of

Scott Gillespie:

regenerative practices. It's easy for individual farmers to

Scott Gillespie:

feel powerless to do what they think is right. But the

Scott Gillespie:

decisions of farmers are a form of embedded agency. One farmer

Scott Gillespie:

alone may not be able to do much, but just by doing it, they

Scott Gillespie:

will help another farmer to see a different way. Farm by farm,

Scott Gillespie:

field by field, those decisions aggregate — like grains of soil

Scott Gillespie:

— into watershed scale effects.

Mendel Skulski:

Future Ecologies is an independent production. In

Mendel Skulski:

this episode, you heard Scott Gillespie, Adam Huggins, and

Mendel Skulski:

myself, Mendel Skulski,

Scott Gillespie:

But we had lots and lots of help on the

Scott Gillespie:

background. From Kimberly Cornish, Nicole Tautges, Stephen

Scott Gillespie:

Shafer, Emily Oldfield, and Sean Smukler. Thanks.

Mendel Skulski:

Mix and sound design was by me, with music by

Mendel Skulski:

Patricia Wolf, Erik Tuttle, Thumbug, and Sunfish Moon Light.

Scott Gillespie:

A full list of credits and citations can be

Scott Gillespie:

found at futureecologies.net

Mendel Skulski:

where you'll also find the rest of our

Mendel Skulski:

episodes and a way to get in touch. We always love hearing

Mendel Skulski:

from you.

Adam Huggins:

Even if it's hate mail?

Mendel Skulski:

I guess we'll find out. Thanks as ever to all

Mendel Skulski:

of our supporting listeners on Patreon. This show simply

Mendel Skulski:

wouldn't be possible without you. To be a part of our

Mendel Skulski:

incredible community, head to futureecologies.net/patrons

Adam Huggins:

Thanks to the Sitka foundation for helping to

Adam Huggins:

support our fourth season. And to everybody else, if you can't

Adam Huggins:

help the show out with your money, you can still definitely

Adam Huggins:

help out with your words. Share your favorite episode with

Adam Huggins:

somebody you love, or just the next person that you meet — who

Adam Huggins:

you might also find that you eventually love. We really

Adam Huggins:

appreciate it.

Scott Gillespie:

Is that it?

Mendel Skulski:

That's it. Thanks for listening

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