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:

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Mendel Skulski:

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Mendel Skulski:

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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