FE4.8 - Ground Truthing

Summary

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.

Click here to read a transcription of this episode


Show Notes

This episode was produced by Scott Gillespie, Mendel Skulski, and Adam Huggins. Besides working as an agronomy / regenerative agriculture consultant, Scott hosts his own podcast: Plants Dig Soil.

Music by Patricia Wolf, Erik Tuttle, Thumbug, and Sunfish Moon Light

Special thanks to Kimberly Cornish, Nicole Tautges, Stephen Shafer, Emily Oldfield, and Sean Smukler for all their help!

✨ Future Ecologies is an independent production, and is supported by our community of listeners on Patreon. You can join them for as little as a dollar each month — at patreon.com/futureecologies 🌱



CITATIONS

Button, E., et al. (2022) Deep-C storage: Biological, chemical and physical strategies to enhance carbon stocks in agricultural subsoils, Soil Biology and Biochemistry, 170. doi:10.1016/j.soilbio.2022.108697

Georgiou, K. (2022) Global stocks and capacity of mineral-associated soil organic carbon, Nat Commun., 13(1):3797. doi:10.1038/s41467-022-31540-9.

Michaud, L. (2021) 2020 FCC farmland rental rates analysis, FCC-FAC, blog post

Minasny, B., McBratney, A. (2006). A Conditioned Latin Hypercube Method for Sampling in the Presence of Ancillary Information, Computers & Geosciences, 32. 1378-1388. doi:10.1016/j.cageo.2005.12.009

Oldfield, E. (2021) Study shows healthy soils protect corn yields and lower crop insurance payouts, Environmental Defense Fund, blog post

Oldfield, E. (2021) Quick action needed to achieve full mitigation potential of soil carbon credits, Environmental Defense Fund, blog post

Oldfield, E. (2022) How regional accounting can boost the integrity of the voluntary soil carbon market, Environmental Defense Fund, blog post

Paustian, K. et al (2020) Climate Mitigation Potential of Regenerative Agriculture is significant!, open letter in response to WRI blog post “Regenerative Agriculture: Good for Soil Health, but Limited Potential to Mitigate Climate Change”

Popkin, G. (2021) A Soil-Science Revolution Upends Plans to Fight Climate Change, Quanta Magazine

Ranganathan, J., Waite, R., Searchinger, T., Zionts, J. (2020) Regenerative Agriculture: Good for Soil Health, but Limited Potential to Mitigate Climate Change, World Resources Institute, blog post

Roesch-McNally, G., Basche, A., et al. (2018). The trouble with cover crops: Farmers’ experiences with overcoming barriers to adoption. Renewable Agriculture and Food Systems, 33(4), 322-333. doi:10.1017/S1742170517000096

Sanderman, J., et al. (2017) Soil carbon debt of 12,000 years of human land use, PNAS, 114 (36), 9575-9580. doi:10.1073/pnas.1706103114

Sanderman, J., et al. (2018) Correction for Sanderman et al., Soil carbon debt of 12,000 years of human land use, PNAS, 115 (7) E1700, doi:10.1073/pnas.1800925115

Searchinger, T., Ranganathan, J. (2018) Creating a Sustainable Food Future: A Menu of Solutions to Feed Nearly 10 Billion People by 2050, World Resources Institute, Synthesis report

Searchinger, T., Ranganathan, J. (2020) Further Explanation on the Potential Contribution of Soil Carbon Sequestration on Working Agricultural Lands to Climate Change Mitigation, World Resources Institute, blog post

Tautges, N., Chiartas, J., et al. (2019) Deep soil inventories reveal that impacts of cover crops and compost on soil carbon sequestration differ in surface and subsurface soils, Global Change Biology, 25(11), 3753-3766. https://doi.org/10.1111/gcb.14762

Waite, R., Rudee, A. (2020) 6 Ways the US Can Curb Climate Change and Grow More Food, World Resources Institute, blog post

Whetter, J. (2022) The true history of farming on the Prairies, The Narwhal


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Transcription

Introduction Voiceover  00:01

You are listening to season four of Future Ecologies.

Mendel Skulski  00:09

Okay, let's do it.

Adam Huggins  00:10

Okay. I'm Adam.

Mendel Skulski  00:12

Mendel.

Adam Huggins  00:13

And this is Future Ecologies. And I'm here because Mendel invited me to be here to talk about natural climate solutions.

Mendel Skulski  00:22

That's right.

Adam Huggins  00:23

Which, which are...?

Mendel Skulski  00:25

Which are, you know, a whole bunch of different things. But they're basically all ways that we can harness natural ecosystems or natural processes to mitigate the impacts of climate change.

Adam Huggins  00:39

Yeah, basically non-technological solutions to sucking greenhouse gases out of the atmosphere.

Mendel Skulski  00:45

Right.

Adam Huggins  00:45

And this topic is all of the rage right now in climate circles, because well, because it's hopeful. And it promises to provide a way for us to restore ecosystems and to protect biodiversity and have benefits for human communities as well. All while sequestering lots of carbon.

Mendel Skulski  01:06

Yeah, natural climate solutions are usually pitched as this big win-win-win. And, you know, conveniently, that pitch usually skips the part where governments or industry have to reduce their own emissions.

Adam Huggins  01:18

Yeah, it's always easier to promote and invest in something that doesn't require the powerful to make sacrifices.

Mendel Skulski  01:24

Yeah. Although, you know, ideally, those solutions are implemented in tandem with reductions in greenhouse gases from human sources. It can't be either/or, it's definitely a yes/and kind of situation.

Adam Huggins  01:38

 Yeah, we have to do all of it. And even though we did a whole set of seven episodes on the climate crisis a couple of years back —

Mendel Skulski  01:46

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

Adam Huggins  01:50

we actually didn't talk much at all about natural climate solutions in that series. Did we even did we mention it?

Mendel Skulski  01:58

No, I mean, it was supposed to be a series about climate inaction. You know, and of course, we had to sneak some action in there, too. But no, you're right. We really didn't cover natural climate solutions. So we're here today to redeem ourselves, and maybe generate some hate mail.

Adam Huggins  02:20

Wait, wait, really?

Mendel Skulski  02:22

Yeah.

Adam Huggins  02:23

We don't want to do that.

Mendel Skulski  02:24

No. You know, I just think that this is honestly going to be one of the most controversial episodes we've ever made.

Adam Huggins  02:31

God, I hope not. I'm I'm actually really jazzed about natural climate solutions. And I'm so excited that I did a bunch of background research. I hope that's okay.

Mendel Skulski  02:41

You're incorrigible. You're supposed to be the blank slate for this one.

Adam Huggins  02:45

It's hard for me to pretend to be the blank slate on the subject that I spent most of my time working on. Can I can I share with you what I found?

Mendel Skulski  02:56

Sure.

Adam Huggins  02:58

Okay, here we go. natural climate solutions tend to focus on enhancing the ability of natural processes to capture and store carbon in living biomass and in the soil. And also occasionally in rock, which we actually did talk a little bit about on Scales of Change. Anyway, we can sequester all this carbon by planting forests in places where they used to be, or where they could be — that's afforestation or reforestation. We could also protect and restore wetland ecosystems, and especially peatlands because they are so carbon rich.

Mendel Skulski  03:31

Yeah.

Adam Huggins  03:32

And finally, we can improve agricultural practices to store more carbon in crop and pasture lands.

Mendel Skulski  03:39

Hey, guess what.

Adam Huggins  03:40

What?

Mendel Skulski  03:41

Today's episode is about that last one, storing more carbon in agricultural soils.

Adam Huggins  03:47

Nice. Okay. Well, in that case, one thing I learned about that is that there is huge potential for the agricultural approach. Like globally, but also in Canada specifically, I read a major study recently that was published earlier this year, and found that Canada currently stores about 20% of all global soil carbon.

Mendel Skulski  04:14

Well, that's, that's actually more than I expected. I mean, it is a huge country, but like a bunch of that is in wetlands, right?

Adam Huggins  04:26

Yeah, about a third of Canada's soil carbon is stored just in peatlands, which only cover about 12% of the land surface here. But you know, are a huge carbon sink. About half of that soil carbon is also in permafrost, you know, permanently frozen soils, which, as we've learned are a giant ticking climate time bomb.

Mendel Skulski  04:49

Let's not go there.

Adam Huggins  04:51

Let's not go there. But the rest is stored in other ecosystems. And just to put all of this in perspective, this is do that already estimated that over 20 gigatons of carbon are stored in living biomass in Canada,

Mendel Skulski  05:06

Right, so like trees and shrubs and roots and animals.

Adam Huggins  05:10

Yep.

Mendel Skulski  05:11

And by 20 gigatons you mean 20 billion metric tons of carbon?

Adam Huggins  05:16

Yeah, a gigaton is a billion tons, or about 10 to the 15th power of grams. A petagram, actually!

Mendel Skulski  05:23

And that's a lot.

Adam Huggins  05:24

Yeah,  one gigaton of carbon is a lot. 20 bigatons is inconceivable. But um, you want to know how much is stored in the soil?

Mendel Skulski  05:32

Hit me.

Adam Huggins  05:33

Apparently, over 300 gigatons are stored in the top one meter of soil alone, here in Canada. And as much as 260 more gigatons in the next meter down. So you know, 20 gigatons in all of the living biomass in Canada, and over 15 times that amount in the top one meter of soil alone.

Mendel Skulski  05:57

Well, I have a statistic for you: the carbon that used to be in the soil, and was lost due to agriculture over the past 200 plus years.

Adam Huggins  06:08

Oh, yeah? Lay it on me.

Mendel Skulski  06:10

So this one is also an estimate, as are all huge numbers. But worldwide, agriculture has released over 116 gigatons from the soil.

Adam Huggins  06:23

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

Mendel Skulski  06:28

Yeah. And lots of agricultural land in Canada.

Adam Huggins  06:32

And it would follow then that this country probably accounts for a big chunk of those global soil losses.

Mendel Skulski  06:38

Yeah. I mean, the areas that have been farmed and grazed intensively in the past often have organic carbon levels that are way, way below their ancient capacity. And you can look all around the world, the places with the most intense history of cultivation, are now the ones with the most degraded soils

Adam Huggins  06:56

And the least soil carbon.

Mendel Skulski  06:58

Yeah. So today, we're not just talking about keeping it in the ground, we're talking about putting it back.

Mendel Skulski  07:06

From Future Ecologies, this is Ground Truthing.

Introduction Voiceover  07:12

Broadcasting from the unseeded shared and asserted territories of the Musqueam, Squamish and Tsleil-Waututh, this is Future Ecologies: exploring the shape of our world, through ecology, design and sound.

Mendel Skulski  07:57

Okay, so to sift through the story, I brought in some help.

Scott Gillespie  08:01

Hello!

Mendel Skulski  08:02

Scott. Adam. Adam, Scott Gillespie.

Adam Huggins  08:05

Hey, Scott, thanks for joining us.

Scott Gillespie  08:07

Glad to be here.

Mendel Skulski  08:08

So Scott is a professional agronomist in southern Alberta, which is the traditional and present day home of the people of the Blackfoot Confederacy.

Scott Gillespie  08:18

Yeah.

Adam Huggins  08:19

I've been to southern Alberta, but I don't think Future Ecologies has. Scott, would you help situate us?

Scott Gillespie  08:25

Well as our local country singer, Corb Lund, once put it: we're East of the Rockies, and we're West of the rest. Right at the edge of what we call the prairies in Canada, or the plains in the United States: the great grasslands of North America.

Adam Huggins  08:37

Well, for those of us who are even West-er, maybe you could tell us what it's like to be out there.

Scott Gillespie  08:43

Yeah, well, as you can probably picture, trees don't grow here naturally. It can be a place of intense winds and extreme temperatures. Historically, it would have been a pasture of huge herds of bison. And now it's been converted to mostly agriculture in one form or another. So in my area, which is in the south of the province, we live in what the farmers here call the brown soil region.

Adam Huggins  09:07

I love that. I love that you use the color of the soil to describe the character of the place that you live. What is it that makes the soils there Brown?

Scott Gillespie  09:17

It's basically the fact that it's so dry here. Over geological periods, we just don't get a lot of rain. So, not a lot accumulates in the soil. As you go further north through the province, you get more rainfall. And then you get into what they call the dark brown soil, and then eventually you get to the black soils, which are these beautiful rich soils — that are full of organic material.

Adam Huggins  09:40

Do I detect a bit of soil envy there in your voice, Scott?

Scott Gillespie  09:43

Maybe a bit.

Mendel Skulski  09:45

So Scott, maybe you should tell us what an Agrologist is?

Scott Gillespie  09:49

Okay. Well, the easiest way to think of it is if you think of what a veterinarian does for animals, an Agrologist does for plants and soils.

Mendel Skulski  09:57

And you have your own podcast.

Scott Gillespie  09:59

Yeah, Plants Dig Soil.

Mendel Skulski  10:00

Where you help farmers practice something called regenerative agriculture.

Scott Gillespie  10:05

That's right.

Mendel Skulski  10:07

And you know, I think we'll get into exactly what that means later. But first, let's cover some basics. Climate change is here. And it's happening faster and stronger than almost anyone predicted. And as we all know, the main molecular malefactor is of course...

Adam Huggins  10:26

Carbon dioxide.

Scott Gillespie  10:27

Yeah. And ultimately, the carbon causing all these problems came from under our feet. The source of the carbon that we hear the most about, and for good reason, is fossil fuels. But it's not the only one. As you mentioned in the intro, a significant chunk of human caused emissions came from the soil itself.

Adam Huggins  10:46

Right, yeah, living in the age of agriculture, we took — what... what was it, Mendel, 116?

Adam Huggins  10:52

Yes.

Adam Huggins  10:53

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

Scott Gillespie  10:58

Well, not quite, because it's not totally clear how much of the carbon went back into the ocean, either as dissolved carbon dioxide or unfortunately as dust from topsoil erosion.

Adam Huggins  11:11

Right... Yeah, erosion and ocean acidification. Neither of those are are good either.

Mendel Skulski  11:16

No. But you know, together, we quantify those losses and call them the "soil carbon debt": the carbon that we owe back to the soil. You could basically say that we cashed out millennia of carbon to grow our crops as quickly and easily as we could.

Scott Gillespie  11:34

Yeah. And there was even a belief among the European colonists that with proper tillage, there was an inexhaustible supply of plant nutrients — flowing up from the deep. And because of a fluke of the climate, they happened to be establishing these farms during a wet cycle, leading them to think that plowing fields caused more rainfall.

Adam Huggins  11:55

Wait, are you serious?

Scott Gillespie  11:56

I'm serious.

Adam Huggins  11:57

Does plowing cause rainfall?

Scott Gillespie  11:59

No, it doesn't. But it all ended when the dry cycle returned in the 1930s. So you might heard of the Dust Bowl: the topsoil was so depleted, it just simply blew off the land.

Adam Huggins  12:13

So here we are. And we're looking back at all of the damage caused by intensive agriculture and all of the carbon that's been released. And of course, the obvious question is, why don't we just put it back? Right? If if there's room in the ground for billions more tons of carbon, then theoretically, we could solve climate change and repay our weary soils at the same time. It's the obvious fix.

Mendel Skulski  12:39

And that, plus the little wrinkle of feeding the world —

Adam Huggins  12:42

Right that, yeah, too

Mendel Skulski  12:44

That's the dream of regenerative agriculture.

Mendel Skulski  12:57

So regenerative agriculture means different things to different people, at least in terms of what it looks like in practice. But I think everyone would agree that the goal is growing food, while simultaneously enriching, and you know, that is returning carbon to the soil.

Adam Huggins  13:15

Well, let's dig in. How does the carbon get into the soil? And how can we help?

Scott Gillespie  13:22

Well, this is where things get more complicated than we could ever cover in a single episode. So let's just break it down to what we can understand at a couple different levels.

Adam Huggins  13:30

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

Scott Gillespie  13:33

So the first level is that there's only one way to increase soil organic carbon: living growing plants. So you could say, plants dig soil.

Adam Huggins  13:44

Ya' could.

Scott Gillespie  13:45

If you think about it, ultimately, the only new carbon going into the soil is from the plants,

Adam Huggins  13:51

Right. Primary production — classic ecology here. As opposed to animals and fungi, plants famously photosynthesize, and they use the sun's energy to turn carbon dioxide in the air into their own bodies. A thing, which, when I first learned, it, absolutely blew my mind because I thought they were building their bodies directly out of the soil. And it turns out, almost all of that is from the atmosphere. Totally freaking incredible.

Scott Gillespie  14:19

And it's important to remember that those bodies aren't just above ground where we can see them. Generally, about a third of the mass of a plant, which is almost all carbon is in its roots. So grasslands put more into their roots, forests put more into the woody structures. But generally 30% is a good rule of thumb. So in a food system, there's a portion that is harvested and exported off the land. Some of that carbon will be eaten, and most of that will return to the atmosphere with every human breath.

Adam Huggins  14:51

But some of that harvest that you're talking about is is not going to make it into people's bodies and onto their tables. Because it's stuff like leaves and stems and husks and roots — stuff that we don't tend to eat as people, right? You have to grow a lot of plant material to get an ear of corn,

Scott Gillespie  15:08

Right, and that carbon will get eaten by something else. The first step is usually for grazing animals, earthworms, or any other large critters of the soil to eat it. And they break it down to a more manageable size for the main decomposers: fungi and bacteria.

Adam Huggins  15:24

So you have the portion of the plant that we eat and respire, and you have the portion that, you know, passes through our bodies, of course. But everything else should be going back to the field that it was grown on, right?

Scott Gillespie  15:42

So in theory, yes, but practically no. Most food travels 1000s of kilometers, sometimes across oceans. No one wants that back. If crop waste, food waste, or humanure gets buried in landfill, you'll get a lot of methaneÚ a greenhouse gas, it's 84 times worse than CO2. If instead it gets composted, you'll still lose some of the carbon to the air as those microbes eat and breathe. But you can put a lot of it back onto the field.

Mendel Skulski  16:12

Yeah, the problem is still that you need to get it to a field, maybe not the original field that it grew on. But any field nearby can benefit from this far better than just putting it into a landfill. But the real trick is getting that carbon to stay there.

Scott Gillespie  16:29

Okay, then let's go to level two.

Mendel Skulski  16:30

Level two!

Scott Gillespie  16:32

The way the carbon from these plants actually becomes part of the soil. As the plant grows, as much as 25% of the carbon formed by photosynthesis is released as a liquid by its roots. These liquids called root exudates —

Mendel Skulski  16:48

Yeah, because they're exuding — roots exude exudates.

Scott Gillespie  16:52

Yes. And these liquids feed the fungi and bacteria that live in the soil. Now, when I was in school, 20 years ago, it was thought that the roots were just leaky. Now we know that they tune exactly what molecules they release: they're trying to attract the fungi and bacteria that they want hanging around the roots.

Adam Huggins  17:12

That's so wild.

Scott Gillespie  17:13

Now some of this liquid carbon will go right back off as CO2 as the microbes use it for energy. But through a complex series of symbiosis, this microbial ecosystem locks in the carbon into clumps of solidified soil grains called aggregates.

Adam Huggins  17:29

Got it.

Scott Gillespie  17:29

Now how long that carbon stays in the soil depends on the stability of those aggregates, which may get disturbed by earthworms, new roots moving through the soil, tilling, droughts or floods.

Scott Gillespie  17:43

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 slope, the health and the diversity of all those microbes. But the most important by far is simply the amount of photosynthesis happening in the first place. The more green growing plants, the better.

Adam Huggins  18:06

Well, so far, none of this sounds particularly controversial to me.

Mendel Skulski  18:12

I would say we're still on firm ground. That's all pretty settled, if over-simplified soil science. But the debate really starts to heat up when you wade into the question of "what should we do about it?"

Adam Huggins  18:26

People arguing about climate policy? I can't believe it.

Mendel Skulski  18:29

This isn't the classic case of climate deniers versus the world.

Adam Huggins  18:33

No?

Mendel Skulski  18:34

No. And you know, wouldn't bother making this episode, if it were. The people on both sides of this debate really just want the same thing. And that's carbon drawdown and food security. Where their opinions differ is whether we can count on soil carbon sequestration to get us there.

Scott Gillespie  18:52

Ss in, should we pay farmers for adding carbon to their soils?

Adam Huggins  18:56

Oh, okay. So now we're talking, I think, about carbon credits. Which are, you know, market solutions for market problems. Am I right?

Mendel Skulski  19:08

Yeah. Well, I'm actually still on the fence about it. Because farming at scale is really expensive, and the margins can be razor thin. You know, for a farmer, any little change in behavior can mean tens of thousands of dollars up front, without any guarantee of success at the end of the season. So if we want to make our food system less destructive, we need to find a way to help farmers make the leap. But then again, if we're going to pay for that carbon, we better be damn sure it's real.

Scott Gillespie  19:39

And that's the root of the debate. Selling carbon credits can lock farmers into complicated contracts that may or may not make financial sense to them. It might give polluters the excuse to continue their business as usual, canceling out the climate benefits, or even worse, the soil carbon backing those credits might not be there at all.

Adam Huggins  20:00

Wait, what do you — what do you mean?

Mendel Skulski  20:02

Scott? Are you ready?

Scott Gillespie  20:03

Yep.

Mendel Skulski  20:04

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

Adam Huggins  20:08

Did I miss something? Like, do we have a segment called "Ring the bell, read a list"?

Mendel Skulski  20:13

Just go with it.

Scott Gillespie  20:14

Okay, so there's four things that are good carbon credit has to represent: additionality, non-reversal, lack of leakage, and permanence.

Scott Gillespie  20:25

Additionality means that we want the carbon to be sequestered because of the credit incentive. That is, it's additional to our baseline.

Adam Huggins  20:34

Right, the business as usual scenario. So for it to have any benefit to the climate, it has to go above and beyond the status quo.

Mendel Skulski  20:42

Exactly. And then there's non-reversal, which means that those credits also have to contend with that temperamental flux that is soil carbon, either by a change in farming practices or, you know, uncontrollable factors, like a change in the climate.

Adam Huggins  20:59

Can you imagine?

Mendel Skulski  21:01

Right? It could cause that carbon to go from being locked up in soil aggregates, to right back up in the atmosphere.

Scott Gillespie  21:08

Yeah now, farmers aren't generally on the hook for reversals outside of their control. But it does raise questions about what happens down the line. In Canada and the United States, approximately one half of farmers rent the land they farm on. They can't guarantee how the next tenant will treat the soil.

Mendel Skulski  21:25

No. And landlords and owner operators might also feel conflicted about signing contracts. What if an opportunity for a lucrative cash crop comes along, you know, five or 10 years later, but the practices of farming it go against the sequestering of carbon?

Adam Huggins  21:41

Right, I'm starting to get a sense of how this could be complicated.

Scott Gillespie  21:44

Well, then meet leakage. leakage is when a climate positive action in one place causes a climate negative effect somewhere else.

Mendel Skulski  21:54

Say for instance, if (and this is a contentious if) regenerative farming practices results in lower food yields, than the market would put pressure on other farmers to convert yet more land, perhaps by clearing a productive forest or prairie.

Adam Huggins  22:10

Yeah, nobody wants leakage. Now, not only would that be outside of the carbon farmers control, they might not even know about it, right? Like you're talking about a systemic pressure because of the price of food or or land.

Scott Gillespie  22:24

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

Mendel Skulski  22:28

So permanence is kind of related to reversal, but it's about the time horizon. We've been talking about how carbon naturally cycles through plants, the soil, the air. But if our concern is reducing greenhouse gases, we really want that carbon locked away for as long as possible. Ideally, on geological timescales, like the fossil fuels it mostly came from. In the world of carbon credits, that target is usually set somewhat arbitrarily, at 100 years.

Scott Gillespie  22:57

And outside of places like bogs —

Adam Huggins  22:59

We love a bog

Scott Gillespie  22:59

— it's just really hard to know where that carbon will be in a century. Think about the land around you, and what it looked like 100 years ago. I bet its quite a bit different than what it looks like today.

Adam Huggins  23:13

Yeah, so that's a lot that any legitimate soil carbon credit would have to account for.

Mendel Skulski  23:21

Yeah, no kidding.

Adam Huggins  23:22

So how do we actually do that? Like, how... how do you prove that any of that is working? That you have, let me see hold on... additional carbon, that is not reversing itself back into the atmosphere, and isn't leaking out somewhere, because it's permanent.

Mendel Skulski  23:45

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

Mendel Skulski  24:03

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

Mendel Skulski  24:09

You make Future Ecologies possible by sharing it with the people that need to hear it, and encouraging them to support it on Patreon. So far this season, we've had the help of three guest producers and 20 musicians, not even including Adam and myself. I'm so proud that we can pay all of those people for their work. And we can do so because of our supporters on Patreon. Plus, I can usually make rent and get groceries.

Mendel Skulski  24:39

If you like this show, it's because we spend an incredible amount of time and effort on every episode. At least months, sometimes years. You don't get to hear all the drafts and revisions that go into each one, and hopefully you don't even notice that they're there. We just want you to come with us on a journey into an idea — and to let sound help tell the story, not get in the way.

Mendel Skulski  25:05

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Mendel Skulski  25:58

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

Adam Huggins  26:00

Hey.

Mendel Skulski  26:01

We're joined by Scott.

Scott Gillespie  26:02

Hello.

Mendel Skulski  26:02

And today on Future Ecologies, we're talking about the promise of soil carbon sequestration, or how we could use food-producing land to fight climate change.

Scott Gillespie  26:13

Well, I wouldn't say the promise, but rather the possibility. And in practice, that might be a whole lot different from the feasibility.

Adam Huggins  26:21

Right. I mean, basically, I came here, super stoked to talk about natural climate solutions, and you guys are just raining on my parade.

Mendel Skulski  26:29

Yes.

Adam Huggins  26:30

So to recap, we know in theory that the soil could hold as much carbon, at least, as we've taken out of it since the agricultural revolution, which was how much again?

Mendel Skulski  26:42

116 gigatons.

Adam Huggins  26:44

Yeah, that's a lot. But because that carbon doesn't like to sit still — it likes to flow through plants and microbes, and then back up into the air, and it might even leak out somewhere else because of pressures on land use — actually, keeping it in the ground is a lot easier said than done.

Mendel Skulski  27:00

Exactly. But that's not to say we can't do it. Regenerative ag as it's practiced today is really just a repackaging of different traditional agricultural techniques from all around the world: Cover cropping, composting, no till or low till, biochar, agroforestry matrix planting, silvopasture... none of these are new ideas. And they're all known to build soil and turn it dark and rich, basically packed with organic carbon.

Scott Gillespie  27:31

That's true. But proving it, and selling it by the ton? That's another story. And it brings us into the realm of MRV.

Adam Huggins  27:40

We love a good acronym. What is MRV?

Scott Gillespie  27:43

Measurement, reporting and verification. Basically, accounting and auditing in the world of carbon sequestration.

Adam Huggins  27:51

Please tell me this didn't turn into an episode about accounting.

Mendel Skulski  27:54

How about we just focus on that one key aspect: measurement. To know how much carbon any intervention helped add to the soil, first, you have to measure how much carbon is there already.

Adam Huggins  28:06

Sure, yeah.

Mendel Skulski  28:07

And that's not easy, or cheap.

Scott Gillespie  28:09

Because so carbon is not a simple compound to measure, like, say CO2. Organic chemistry is an entire scientific discipline studying all the compounds that carbon can make.

Adam Huggins  28:20

Can I just say that was the best summary of organic chemistry that I've ever heard? Even after studying it for a couple years.

Scott Gillespie  28:25

Well, thanks. So because carbon can take all those different forms. And because soil is really variable, and heterogeneous, on a landscape scale, carbon can be incredibly patchy. So you need to sample enough points to get good data. Sample too few, and you might be getting the wrong picture. Sample too many, and you're just wasting time and money.

Mendel Skulski  28:46

And by sample, we mean physically going into the field and getting a soil core. That is, like, drilling out a tube of dirt, and then shipping it off to a lab to be analyzed. Every single core is at least a few minutes of work.

Scott Gillespie  29:00

Provided you don't hit a rock.

Mendel Skulski  29:02

Yeah. Plus all the logistics and expenses around the lab analysis.

Adam Huggins  29:06

I mean, I've done soil sampling before and it's it's not that hard. But I've also only done it on like small areas of land.

Scott Gillespie  29:15

Well consider that the Canadian Prairies alone have 77 million acres of farmland. Most city blocks are just a few acres in size.

Mendel Skulski  29:23

Yeah, it really all adds up.

Adam Huggins  29:24

Well, that's not great. Is that really the best option that we have?

Mendel Skulski  29:29

There are a few promising new technologies. But right now, none of them are ready for primetime. Some folks are aiming to use satellites, you know, so called remote sensing to measure soil carbon en mass. Some are using these meteorological stations that are called eddy towers to calculate the carbon flux at this landscape level. And then there's others who are developing tools that can measure the carbon right there in the field, instead of a soil core — using a probe that basically detects the color of the dirt.

Adam Huggins  30:00

Right like brown, dark brown and black.

Scott Gillespie  30:03

Exactly. Color can be a decent proxy for the amount of organic carbon in the soil. And all of these tools will be used to improve computational models so that we can better predict what's happening to the carbon, and then use the magic of statistics. So we don't need to take as many physical samples.

Mendel Skulski  30:19

Yeah, real magic. They've got incantations, like regionalised variables and conditioned Latin Hypercube sample design.

Adam Huggins  30:29

That's real Arcana. It's almost like you want to explain a thing?

Mendel Skulski  30:32

I don't.

Adam Huggins  30:33

Okay, so you're saying that these techniques are good enough for the kinds of large estimates we've been throwing around in this episode so far, but not necessarily good enough to be sure that we are selling a certain amount of carbon when we're making carbon credits.

Scott Gillespie  30:48

No. And there might be one more problem.

Mendel Skulski  30:51

And it's a big one.

Mendel Skulski  30:57

So the way soil carbon is measured, now, those samples are usually taken from the top 30 centimeters —

Adam Huggins  31:04

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

Mendel Skulski  31:08

And you know, that's because the deeper you go, the more expensive and challenging it gets. Try pushing a probe into the soil, you know, like you said, the top is kind of easy. But the deeper you go, the more pressure it takes, almost exponentially.

Scott Gillespie  31:23

I've done a lot of soil sampling over the years. And I can definitely attest to that. Soil sampling is typically done with hydraulic probes mounted to pickup trucks, and the force is enough to lift the truck or bend the probe if you're not careful.

Adam Huggins  31:36

Wow, okay. But why go deeper? Isn't the top foot of the soil where most of the roots and microbes are anyway?

Scott Gillespie  31:45

That's mostly true, but some roots go two or three times that deep. In the case of prairie grasses, 10 times or more. And of course, in other places, the subsoils can and will be a completely different situation.

Mendel Skulski  31:59

And there's a growing body of evidence that when we only measure carbon sequestration in the topsoil, we're only getting a little slice of the whole picture,

Adam Huggins  32:07

Right — those estimates that we covered at the beginning of the episode, were all about how the deep soils are a big part of the carbon stocks for Canada.

Scott Gillespie  32:17

But those were just estimates, not field by field measurements. What Mendel is talking about is a particular study that looked at how soil organic carbon accumulated with and without cover cropping, and a variety of inputs like chemical fertilizers and compost. What was important about this study is that it was long term, most studies only last the length of a grad student's degree, which is about two to four years,

Adam Huggins  32:41

Not exactly the timescale of soil formation. That would be a PhD.

Scott Gillespie  32:45

No, but we can do a little better. In this study, soil samples had been taken over 19 years. And various combinations of cover crops, irrigation, synthetic fertilization, and compost were kept consistent over that time. Unlike your typical 30-centimeter cores, these ones went two meters down, with five sample points over that depth.

Adam Huggins  33:08

That's uh... that's hardcore? Hard... deep core? Anyway, deep cores, long duration, different field variables, I'm with you.

Scott Gillespie  33:18

So when no inputs were added to the system, and no cover crops were planted, carbon in the topsoil is decreased. Exporting food off the land meant that the microbes needed to break apart their savings of long term carbon for nutrients.

Adam Huggins  33:32

As you'd expect.

Scott Gillespie  33:33

Now, you remember how we talked about that to build organic matter, we need more plants growing. Cover crops are a way to achieve this in a farming system by growing something in the shoulder season. Before and after the cash crop. It's one of the key practices in regenerative systems, because it helps to build the soil.

Adam Huggins  33:51

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

Scott Gillespie  33:54

Yeah, so when winter cover crops were added to the conventional system — as in a system that uses synthetic fertilizers and pesticides — in this particular study, the top soil saw a statistically significant increase in soil organic carbon.

Adam Huggins  34:09

So far, so good.

Scott Gillespie  34:10

But the rest of the soil down to meters had a statistically significant decrease in carbon. When looking across the whole profile. They saw not only less sequestration, but net positive emissions on the fields with cover crops.

Adam Huggins  34:26

Wait, what?

Mendel Skulski  34:27

Scary, right? That means what we typically perceive as carbon sequestration might actually just be carbon concentration in the top layer of the soil. And because of how much more massive the subsoil is, there may still be significant net carbon losses overall.

Adam Huggins  34:44

So what you're saying is that when we're just measuring the first foot or so of the soil, we might fool ourselves into thinking that we're sequestering carbon, when in reality, it could be the exact opposite.

Scott Gillespie  34:58

You got it. But just to be clear, having this carbon concentrated near the surface isn't bad. That particular crop system was doing this naturally. And so there's probably a reason why it wants to carbon there. After all, that's where most of the roots are. That's where the moisture is. And that's where the microbes live. So it's good for the farmer, just not so good if you think you're sequestering carbon.

Adam Huggins  35:21

What about adding compost? Like to the study, consider what happens if you're adding compost to the fields.

Scott Gillespie  35:27

In that case, the carbon did increase overall. But zooming out, that's essentially the result of leakage from somewhere else. If that compost didn't go back to the field that produced it, you've just transferred carbon from one area to the other.

Mendel Skulski  35:41

Basically more like carbon import, rather than carbon sequestration.

Adam Huggins  35:45

Yeah, that's a pretty sobering study. Thank you for, you know, hitting me with it three quarters of the way to this episode. So I guess, you know, what that makes me think is that when we're talking about, you know, trying to sell that carbon or allowing it to be used as an offset for big industrial emitters, there's a real risk here that that's a wasted investment, or it can actually actively make things worse.

Mendel Skulski  36:13

Yeah. What it really means is that we still have so much left to learn about the dynamics of deep soil. And then we need to factor that into our models. And so this is really where the problem lies. There's, there's a lot of hype, because of models that show big changes. But you dig a little deeper, and you see that most of them only go down 30 centimeters, and sometimes less. As of right now, they can't say what happened in the subsoil. They can only say what happened near the surface.

Scott Gillespie  36:41

Yeah. And maybe eventually we'll develop an understanding of how to lock huge climate shifting amounts of carbon down into those deep soils, and find them at the same time. And do it on a timescale that is much faster than how long it took for those soils to form. But for now, we really can't count on it.

Adam Huggins  37:10

Well, thanks, you two, for a hopeful and uplifting episode. There's nothing I love more than pouring cold water on a natural climate solution. That's what I'm here for.

Mendel Skulski  37:22

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

Adam Huggins  37:26

So, um, I guess to ask, you know, the obvious question, what now? We're, as a society, kind of banking on the soil being a part of our climate solution, and especially agricultural lands. Does this mean that we just give up on that dream? Do we give up on regenerative agriculture?

Mendel Skulski  37:48

No, no, I don't think we should. Regenerative ag can do a whole world of good — especially now, especially during climate disruption. But, you know, in order to realize that, we, I think we have to expand our focus right? Out from just carbon and from carbon markets.

Scott Gillespie  38:08

Yeah, if all we care about is carbon, we're gonna miss the forest for the trees.

Adam Huggins  38:13

It's funny you saying that coming from a place with no trees at all.

Scott Gillespie  38:18

Okay, then how about missing the prairie for the grasses?

Mendel Skulski  38:22

or the roots for the exudates?

Adam Huggins  38:24

That's acceptable.

Scott Gillespie  38:26

Anyhow, one thing is indisputable, regenerative farming is still a good thing. All those regenerative practices can make a soil system more resilient to climate extremes, helping water filter in slowly to manage big rains, holding on to it longer to last through droughts, and just generally increasing resistance to pests and erosion. What farmer wouldn't want that?

Adam Huggins  38:49

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

Adam Huggins  38:52

And there's a bunch of other natural climate solutions for agricultural lands that I think do have a more guaranteed delivery in terms of carbon sequestration. I'm talking about planting more trees on agricultural lands as riparian buffers, or as hedgerows, or as silvopasture, or agroforestry, right? Getting that woody biomass in there. That's going to do a world of good in some places, in other places, just doing leguminous cover crops to help reduce the amount of nitrogen fertilizer that's applied to the land is a huge benefit. Because a bunch of the nitrogen fertilizer that people apply ends up in the atmosphere as nitrous oxide, which is a greenhouse gas that's 300 times as potent as carbon dioxide. So there is a whole suite of practices that are still beneficial for the soil and for the farmer and for the climate.

Mendel Skulski  39:46

Yeah, yeah, I think all of these things add up to huge benefits in water quality and ecosystem health in general. And, you know, hopefully still, food production. And, you know, practically speaking some of those regenerative practices —they might feel more within reach, like winter cover cropping or reducing tillage to the minimum. Others would mean a pretty complete reimagining of how we plant and harvest at scale, and what those fields look like, like what you just described. But with agricultural systems and practices so deeply ingrained, you know, I really think that farmers need help to try something new,

Adam Huggins  40:23

And podcasters of the world are here to provide it.

Mendel Skulski  40:27

Yeah, I mean, podcasters, and governments and people who eat food, right?

Adam Huggins  40:32

Yeah, I am a podcast. I'm not a government. But I am a person who eats food, I think we are all people who eat. And so we all play some part in our food systems. One thing I have learned farming is that every farm is different. And so I guess the regenerative practices that are going to make sense in one place will be different, depending on the farm. What do you think the farmers in your area need, Scott, in order to be able to embrace regenerative practices? What are you seeing?

Scott Gillespie  41:02

To me, I think the most critical thing is that there has to be some type of economic reason to do it.

Adam Huggins  41:09

Like a carbon credit?

Scott Gillespie  41:10

Well, I had hopes in the carbon credit... until I did so much research on this, that it doesn't look like that's going to be a viable solution. So it needs to be something else. Even just incentives to start to get over that initial hump in adoption would be a critical thing. Realistically, it's going to have to be something that's going to make economic sense to the farm. And as an example, in the United States, where cover crops have really taken off is where they had weeds that were resistant to the herbicides and their costs were just getting out of control. When they were able to integrate the cover crops in they're able to bring their cost down. So whether you're farming at a small scale, like a market garden, or up to thousands and thousands of acres, it comes down to economics.

Mendel Skulski  42:03

Yeah. And that's something that doesn't have to come from the potentially greenwashing and, you know, supposedly outcome based world of carbon offsets.

Scott Gillespie  42:12

Yeah, there's things like crop insurance, low interest loan programs, or just straight up cash incentives for regenerative practices — that can help farmers close the gap between doing good for their soil, making a living, and putting food on all our tables. And I'm happy to say there's all sorts of these programs starting to crop up.

Adam Huggins  42:32

You made a pun, Scott. That's delightful. That's usually my job here. What kinds of regenerative practices are you seeing being implemented in the prairies where you live?

Scott Gillespie  42:44

Well, the huge shift over the last quite a few decades has been going to no till or at least minimum tillage. So plowing is very rare in the prairies. And very similar to cover crops, it is showing similar patterns of carbon concentration: in that we do get more carbon in the upper levels, but not as much in the deeper levels. However, just because that happens, doesn't mean that it's not a good practice for the farmer. They're seeing a lot of benefits from it.

Adam Huggins  43:14

Yeah. So some incentivization is important. Like stepping back from this question about carbon credits, what occurs to me is that this whole question of how much carbon is being sequestered, and how do we measure that, and how permanent is that... it's a lot of complexity and noise that we've kind of, like, shoved into what could otherwise be a very simple conversation. Which is that we know that as a society, we are emitting too much carbon. We should be making the people that are emitting all that carbon pay. And then we should be taking that money and incentivizing the practices that we want to see on farms and elsewhere. And we don't necessarily have to quantify that as stringently as we are, if we're not counting on the slimmest of margins for climate recovery. If we aren't trying to, you know, finely balance the amount that we're emitting versus the amount that we're sequestering, right? If the general idea is "emit less, sequester more", then we need to reduce emission, which we we definitely know how to do that. And then incentivize practices that we know will eventually sequester carbon, even if we don't know exactly how much or over what kind of timespan that's going to happen. Do you know what I mean?

Mendel Skulski  44:36

Yeah, I mean, you're saying like, not on a gram by gram, or or ton by ton basis, but just to tax polluters and use that to subsidize regenerative agriculture or agriculture in general.

Adam Huggins  44:51

Yeah, I mean, farming is already heavily subsidized. It's a question of shifting those subsidies to actually support the kinds of practices that we want to see as as a society, I think.

Mendel Skulski  45:01

Totally. And, you know, while we do that, I think we just need to get comfortable with the fact that we're still learning. We're learning that there's a lot more left to learn — about soil especially.

Scott Gillespie  45:13

Yeah.

Mendel Skulski  45:14

We know now that plowing doesn't make it rain, that soil nutrients don't just spontaneously appear, and that plants build their bodies from the air and not the ground.

Adam Huggins  45:26

Yeah.

Mendel Skulski  45:27

But despite how far we've come, we're really still just at the beginning of a soil science revolution. And we're overturning notions that have been in place for decades, you could say some recalcitrant ideas. At some level, we know it's possible to put a lot of carbon back in the soil, because it was there once. But now we also know that there's a lot of work to be done before soil carbon can be the silver bullet we've been hoping for.

Mendel Skulski  45:56

But that doesn't mean we just wait around in the meantime. We already have the tools we need to change how we farm and how we eat, to rebuild the soil in the places where it's the most degraded, and to do whatever we can to regrow a livable planet.

Adam Huggins  46:19

Okay, so if I understand you to correctly, the regenerative practices that we've been discussing this whole episode are good for the soil, they're good for farmers, and they're very likely good for the climate, at least in the long term. But we don't yet have the deep understanding of soil processes required for us to confidently predict and quantify those benefits, at least, enough to think that we can start selling them to each other or to people who are going to use them as an excuse to pollute, maybe. Is that right?

Mendel Skulski  46:54

Yeah, that's about it.

Scott Gillespie  46:56

And to close things out, I just wanted to paraphrase a paper on overcoming the barriers to adoption of cover cropping, since I think it also applies to all sorts of regenerative practices. It's easy for individual farmers to feel powerless to do what they think is right. But the decisions of farmers are a form of embedded agency. One farmer alone may not be able to do much, but just by doing it, they will help another farmer to see a different way. Farm by farm, field by field, those decisions aggregate — like grains of soil — into watershed scale effects.

Mendel Skulski  47:53

Future Ecologies is an independent production. In this episode, you heard Scott Gillespie, Adam Huggins, and myself, Mendel Skulski,

Scott Gillespie  48:02

But we had lots and lots of help on the background. From Kimberly Cornish, Nicole Tautges, Stephen Shafer, Emily Oldfield, and Sean Smukler. Thanks.

Mendel Skulski  48:14

Mix and sound design was by me, with music by Patricia Wolf, Erik Tuttle, Thumbug, and Sunfish Moon Light.

Scott Gillespie  48:25

A full list of credits and citations can be found at futureecologies.net

Mendel Skulski  48:31

where you'll also find the rest of our episodes and a way to get in touch. We always love hearing from you.

Adam Huggins  48:37

Even if it's hate mail?

Mendel Skulski  48:39

I guess we'll find out. Thanks as ever to all of our supporting listeners on Patreon. This show simply wouldn't be possible without you. To be a part of our incredible community, head to futureecologies.net/patrons

Adam Huggins  48:54

Thanks to the Sitka foundation for helping to support our fourth season. And to everybody else, if you can't help the show out with your money, you can still definitely help out with your words. Share your favorite episode with somebody you love, or just the next person that you meet — who you might also find that you eventually love. We really appreciate it.

Scott Gillespie  49:16

Is that it?

Mendel Skulski  49:18

That's it. Thanks for listening