C&EN Uncovered: Can altering ocean chemistry fight climate change?
Can climate catastrophe be stymied by tweaking seawater chemistry?
In this episode of C&EN Uncovered, host Craig Bettenhausen speaks with C&EN reporter Fionna Samuels about her recent C&EN cover story concerning Ocean Alkalinity Enhancement (OAE) as a method to combat climate change by increasing ocean alkalinity to absorb more CO2. Uncovered offers a deeper look at subjects from recent stories pulled from the pages of Chemical & Engineering News. Check out Fionna's story on engineering our oceans to mitigate the effects of Climate Change.
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Credits
Executive Producer: David Anderson
Host: Craig Bettenhausen
Reporter: Fionna Samuels
Video + Audio Producer: Jeremy Barr
Episode artwork: Michael Sswat
Music: Commercial Flow, Shutterstock
Contact Stereo Chemistry: Contact us on social media at @cenmag or email cenfeedback@acs.org.
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Transcript
1 00:00:00,000 --> 00:00:02,490 Craig Bettenhausen: Craig, welcome to CNN uncovered. I'm 2 00:00:02,490 --> 00:00:05,190 Craig Bettenhausen. CNN uncovered is a podcast series 3 00:00:05,190 --> 00:00:07,650 from Stereo Chemistry. In each episode, we'll take another look 4 00:00:07,650 --> 00:00:10,050 at a recent cover story in chemical and Engineering News, 5 00:00:10,050 --> 00:00:12,480 and hear from CNN reporters about striking moments from 6 00:00:12,480 --> 00:00:14,880 their reporting, their biggest takeaways, and what got left on 7 00:00:14,880 --> 00:00:16,890 the cutting room floor. This episode, we're looking at a 8 00:00:16,890 --> 00:00:19,830 recent cover story about a CO two abatement method called 9 00:00:19,830 --> 00:00:22,470 Ocean alkalinity enhancement that aims to use the world's 10 00:00:22,470 --> 00:00:25,440 oceans to remove more carbon from the atmosphere. Are Earth's 11 00:00:25,440 --> 00:00:27,840 vast oceans our biggest allies in the fight against greenhouse 12 00:00:27,840 --> 00:00:30,930 gasses. Can we augment the power of nature to keep our planet 13 00:00:30,930 --> 00:00:33,330 alive longer? We'll put a link to the story in today's show 14 00:00:33,330 --> 00:00:36,150 notes. I'm here with CNN assistant editor Fiona Samuels, 15 00:00:36,150 --> 00:00:37,650 who wrote the article. Hi Fiona. 16 00:00:37,860 --> 00:00:39,420 Fionna Samuels: Hi Craig. It's so nice to be here. 17 00:00:39,690 --> 00:00:40,440 Craig Bettenhausen: Yeah, good to have you. 18 00:00:44,020 --> 00:00:44,200 for 19 00:00:44,250 --> 00:00:46,710 So for anyone that hasn't had a chance to read the story yet, 20 00:00:46,740 --> 00:00:49,500 can you give a brief recap of what's in the article? Yeah, so 21 00:00:49,500 --> 00:00:53,640 basically, I reported on a few different experiments, field 22 00:00:53,640 --> 00:00:57,420 trials, specifically, that are happening around the world to 23 00:00:57,420 --> 00:01:02,580 look at how we can add alkaline substances to ocean water in 24 00:01:02,580 --> 00:01:05,790 order to help it draw down more carbon dioxide from the 25 00:01:05,790 --> 00:01:09,930 atmosphere. And all of this is in an effort to sort of stymie 26 00:01:09,960 --> 00:01:13,200 the worst effects of climate change. And how did you get 27 00:01:13,200 --> 00:01:16,110 interested in this topic? It actually started out looking at 28 00:01:16,140 --> 00:01:20,190 solar radiation modification, or solar geoengineering, which is 29 00:01:20,220 --> 00:01:22,830 putting stuff into the atmosphere to reflect sunlight 30 00:01:22,830 --> 00:01:27,660 back into space. But it turns out that there are almost no 31 00:01:27,690 --> 00:01:31,710 field trials happening in that space right now because it's so 32 00:01:31,740 --> 00:01:35,610 controversial, and the method is very questionable. But there is 33 00:01:35,610 --> 00:01:39,150 quite a few different things happening in the marine carbon 34 00:01:39,150 --> 00:01:42,870 dioxide removal space. So instead of reflecting sunlight 35 00:01:42,870 --> 00:01:46,140 to cool the planet, removing carbon dioxide to help cool the 36 00:01:46,140 --> 00:01:48,570 planet, interesting. So one of the things I had noticed in your 37 00:01:48,570 --> 00:01:51,660 story is this experiment called Loch Ness. Tell me about Loch 38 00:01:51,660 --> 00:01:54,780 Ness. The experiment not the Celtic sea monster or both. I'm 39 00:01:54,780 --> 00:01:55,380 flexible. 40 00:01:56,490 --> 00:01:59,700 Fionna Samuels: So unlike the monster, I guess this experiment 41 00:01:59,700 --> 00:02:03,510 is real and it's officially happening. They just got the 42 00:02:03,510 --> 00:02:07,080 permit, finally approved with the EPA. It's being led by a 43 00:02:07,080 --> 00:02:10,620 researcher at Woods Hole Oceanographic Institute. His 44 00:02:10,620 --> 00:02:14,400 name is Dr Adam Subhas, and what they're doing is they are 45 00:02:14,400 --> 00:02:19,260 releasing a solution of sodium hydroxide into the water and 46 00:02:19,290 --> 00:02:23,970 looking at where that alkaline water goes, and measuring a 47 00:02:23,970 --> 00:02:26,610 whole bunch of different things to try to see if they can 48 00:02:26,610 --> 00:02:31,620 quantify how much carbon dioxide is absorbed by the water because 49 00:02:31,650 --> 00:02:35,040 of that increased alkalinity. Seems too simple to be 50 00:02:35,040 --> 00:02:38,220 intuitive. Can you explain how would dumping a bunch of lye 51 00:02:38,250 --> 00:02:40,680 into the water do anything about carbon dioxide in the 52 00:02:40,680 --> 00:02:43,650 atmosphere. Well, so carbon dioxide dissolves in water 53 00:02:43,650 --> 00:02:46,950 naturally. This is an ongoing geochemical process, and when 54 00:02:46,950 --> 00:02:50,160 the gas dissolves into the water, it quickly reacts to form 55 00:02:50,160 --> 00:02:53,460 carbonic acid, which then dissolves into different 56 00:02:53,460 --> 00:02:57,780 carbonate ions. And because it's an acid protons, so that's why 57 00:02:57,780 --> 00:03:01,110 we get ocean acidification. And it was really interesting 58 00:03:01,110 --> 00:03:04,320 because many of the researchers that I spoke to for this story 59 00:03:04,350 --> 00:03:10,080 started off as researchers of ocean acidification. So the pH 60 00:03:10,110 --> 00:03:13,830 plays a big role in how much carbon dioxide can be absorbed 61 00:03:13,860 --> 00:03:18,660 and then sequestered in ocean water. And by raising the pH or 62 00:03:18,660 --> 00:03:22,230 making it more alkaline, not only are you sort of combating 63 00:03:22,230 --> 00:03:25,800 that acidification that happens with carbon dioxide dissolution, 64 00:03:25,830 --> 00:03:29,340 but you're also making it so more carbon dioxide can be 65 00:03:29,340 --> 00:03:33,510 absorbed and then sequestered as carbonate ions and bicarbonate 66 00:03:33,540 --> 00:03:35,940 ions. It's a little bit like magic, to be honest. 67 00:03:37,830 --> 00:03:38,910 Craig Bettenhausen: And what kind of scales would this need 68 00:03:38,910 --> 00:03:41,160 to operate on to make an impact? 69 00:03:41,220 --> 00:03:43,080 Fionna Samuels: Well, that's a great question. So right now, 70 00:03:43,110 --> 00:03:47,820 humanity is releasing carbon dioxide on gigaton orders of 71 00:03:47,820 --> 00:03:51,840 magnitude. So that's 1 billion metric tons, and it's our annual 72 00:03:51,870 --> 00:03:56,280 emissions are close to 40 billion metric tons. Obviously 73 00:03:56,280 --> 00:03:59,670 we need to reduce emissions. That's number one. But there are 74 00:03:59,670 --> 00:04:03,930 certain sectors that can't be easily decarbonized. So 75 00:04:03,960 --> 00:04:07,710 aviation, agriculture, those cows are going to keep farting. 76 00:04:07,740 --> 00:04:12,540 So we need to do more than just radically decrease emissions. 77 00:04:12,570 --> 00:04:15,780 Scientists think we need to also start removing carbon dioxide 78 00:04:15,780 --> 00:04:19,800 from the atmosphere, but if we're thinking on gigaton scale 79 00:04:19,830 --> 00:04:24,390 of emissions, we want to probably remove gigatons of 80 00:04:24,420 --> 00:04:26,790 carbon dioxide. That would be great. We can't do that right 81 00:04:26,790 --> 00:04:31,590 now. We're not even to millions of metric tons. So one of the 82 00:04:31,590 --> 00:04:35,190 researchers, David Ho, had a really good analogy. He thinks 83 00:04:35,190 --> 00:04:38,700 of carbon removal like a time machine. So if you're thinking 84 00:04:38,700 --> 00:04:43,230 we're emitting 40 billion metric tons of carbon dioxide annually 85 00:04:43,260 --> 00:04:47,700 around the globe. And if we could remove 1 million metric 86 00:04:47,700 --> 00:04:50,910 tons with these carbon dioxide removal techniques, you would 87 00:04:50,910 --> 00:04:54,960 have had gone back 13 minutes in time. That's equivalent to 13 88 00:04:54,960 --> 00:04:59,970 minutes of carbon emissions. So the scale is huge, and. 89 00:05:00,000 --> 00:05:03,180 It's impossible to do it with carbon dioxide removal 90 00:05:03,180 --> 00:05:06,540 techniques alone. Emission reduction is absolutely vital. 91 00:05:06,660 --> 00:05:09,360 Craig Bettenhausen: So I can imagine getting sodium hydroxide 92 00:05:09,420 --> 00:05:12,120 on a laboratory scale. You can get it at the hardware store, 93 00:05:12,120 --> 00:05:15,360 but on that kind of scale, we're not just talking about that kind 94 00:05:15,360 --> 00:05:18,660 of material. Where are we going to get that much base 95 00:05:18,660 --> 00:05:20,600 equivalence, that much alkalinity? Yeah, 96 00:05:20,600 --> 00:05:22,520 Fionna Samuels: so now you're talking about sort of the life 97 00:05:22,520 --> 00:05:24,920 cycle of these sort of techniques. And there's actually 98 00:05:24,920 --> 00:05:27,440 a few different techniques. It's not just putting sodium 99 00:05:27,440 --> 00:05:30,800 hydroxide in the water. So with sodium hydroxide, the Loch Ness 100 00:05:30,800 --> 00:05:36,380 team is truly only interested in figuring out if ocean alkalinity 101 00:05:36,380 --> 00:05:39,560 enhancement is a viable solution, and so they're 102 00:05:39,560 --> 00:05:44,140 basically using the cleanest form of alkalinity in the sense 103 00:05:44,140 --> 00:05:47,440 that sodium hydroxide, they can be incredibly confident of what 104 00:05:47,440 --> 00:05:49,780 they're putting in the water. They can be very confident about 105 00:05:49,780 --> 00:05:53,140 the kinds of reactions that are happening. Sodium ions already 106 00:05:53,140 --> 00:05:56,680 exist in seawater. Hydroxide ions also exist in seawater, but 107 00:05:56,680 --> 00:06:02,460 obviously at a far lower abundance and the pH, they very 108 00:06:02,460 --> 00:06:06,120 well constrained how the pH will fluctuate after their release 109 00:06:06,180 --> 00:06:08,520 and at different timescales after the release. That's why 110 00:06:08,520 --> 00:06:12,120 they're using sodium hydroxide in the real world. You're right. 111 00:06:12,120 --> 00:06:16,620 Sodium hydroxide is not necessarily a viable way to 112 00:06:16,620 --> 00:06:19,320 increase the alkalinity of these bodies of water, because you 113 00:06:19,320 --> 00:06:22,640 would need vast amounts of it. And right now, a lot of sodium 114 00:06:22,640 --> 00:06:26,720 hydroxide is actually produced in chlorine chemical reactions, 115 00:06:26,720 --> 00:06:29,480 but we produce chlorine for other chemistry is happening 116 00:06:29,480 --> 00:06:33,740 anyway. Other researchers are looking at alkaline minerals. So 117 00:06:33,740 --> 00:06:38,000 like olivine is a big one, and that would come from mining 118 00:06:38,000 --> 00:06:41,620 minerals around the world. We humanity, different people are 119 00:06:41,620 --> 00:06:46,060 already sort of spreading these mined minerals on agricultural 120 00:06:46,060 --> 00:06:51,700 fields and elsewhere. So those sources of mineral alkalinity 121 00:06:51,700 --> 00:06:55,240 exist already, which is why these folks who are using 122 00:06:55,240 --> 00:06:58,780 minerals argue that that might be a better option. A third 123 00:06:58,780 --> 00:07:02,100 technique actually uses electrolysis to separate 124 00:07:02,160 --> 00:07:04,980 alkaline seawater from acidic seawater. But the problem with 125 00:07:04,980 --> 00:07:07,440 that is then you have a bunch of acid, and there's not a huge 126 00:07:07,440 --> 00:07:12,360 market for acid to change the pH of things. So you're right when 127 00:07:12,360 --> 00:07:16,200 it comes to scalability, the life cycle of these chemicals is 128 00:07:16,200 --> 00:07:19,380 very important to consider, where they're coming from, where 129 00:07:19,380 --> 00:07:22,340 the byproducts are going. If we're thinking about mining 130 00:07:22,340 --> 00:07:26,000 alkaline minerals, you need to think about if those mines are 131 00:07:26,000 --> 00:07:30,440 emitting more carbon than can be taken up by the ocean or other 132 00:07:30,440 --> 00:07:33,140 carbon dioxide removal techniques where the energy is 133 00:07:33,140 --> 00:07:36,560 coming from. All of this stuff is a big question mark. The 134 00:07:36,560 --> 00:07:40,160 field trials right now are really focused on whether or not 135 00:07:40,280 --> 00:07:44,680 the chemistry is workable from a standpoint of like we 136 00:07:44,800 --> 00:07:47,980 theoretically know that this should work, but does it in the 137 00:07:47,980 --> 00:07:48,700 real world. 138 00:07:49,480 --> 00:07:51,520 Craig Bettenhausen: So that suggests the question, how are 139 00:07:51,520 --> 00:07:54,460 they going to tell what are they measuring to see if this 140 00:07:54,460 --> 00:07:56,320 Fionna Samuels: works? They're measuring a bunch of different 141 00:07:56,320 --> 00:07:59,920 things. So the Woods Hole folks are. They're throwing the whole 142 00:07:59,920 --> 00:08:03,000 instrument laboratory at the problem. They're going to be 143 00:08:03,240 --> 00:08:06,960 taking water in through the ship that they're driving and 144 00:08:06,960 --> 00:08:10,980 releasing the alkaline solution behind to sample for the 145 00:08:10,980 --> 00:08:14,400 pressures of oxygen and carbon dioxide dissolved in the water. 146 00:08:14,400 --> 00:08:17,820 They're also going to be looking at how the pH changes. They're 147 00:08:17,820 --> 00:08:21,260 going to be looking at total dissolved inorganic carbon, 148 00:08:21,260 --> 00:08:23,900 which is all those carbonate ions. They're going to be 149 00:08:23,900 --> 00:08:29,000 looking at changes in the marine life in the area. Of course, 150 00:08:29,000 --> 00:08:31,700 they're going to make sure that they're not, or they plan to 151 00:08:31,700 --> 00:08:35,300 make sure that they're not going to be dumping anything on a 152 00:08:35,300 --> 00:08:40,040 whale's head, right? But as long as there's not any big animals 153 00:08:40,040 --> 00:08:44,860 around the they're gonna dump this solution, and then they 154 00:08:44,860 --> 00:08:48,700 will be taking a plankton net and dragging the plankton net 155 00:08:48,700 --> 00:08:53,500 behind the boat to look at how these little, tiny marine plant, 156 00:08:53,500 --> 00:08:56,500 like creatures, plankton, is hard to find. Sorry, 157 00:08:56,680 --> 00:08:59,020 Craig Bettenhausen: yeah, things at the bottom of the food web, 158 00:08:59,020 --> 00:09:01,440 how the bottom of the food web? Yes, yes, they're 159 00:09:01,440 --> 00:09:03,840 Fionna Samuels: looking at how plankton, which is the bottom of 160 00:09:03,840 --> 00:09:07,020 the food web, will be affected by this experiment in the real 161 00:09:07,020 --> 00:09:09,540 world, because other researchers have already looked at how 162 00:09:09,540 --> 00:09:13,080 plankton are affected in microcosms and mesocosms, which 163 00:09:13,080 --> 00:09:15,540 are basically containers filled with seawater. 164 00:09:15,540 --> 00:09:17,280 Craig Bettenhausen: Yes, I liked in your story, you had this 165 00:09:17,280 --> 00:09:20,240 vocabulary where the mesocosms, and started right off with that, 166 00:09:20,240 --> 00:09:22,760 I immediately, I was like, I need to I'm in just so I can 167 00:09:22,760 --> 00:09:24,080 find out what that word means. 168 00:09:24,140 --> 00:09:26,060 Fionna Samuels: Yeah. So mesocosm is basically like a 169 00:09:26,060 --> 00:09:30,320 giant test tube, like 1000s of liters of water in a test in an 170 00:09:30,320 --> 00:09:33,920 enclosed container. And then the microcosms are smaller volumes 171 00:09:33,920 --> 00:09:36,500 of water, so more on the liter scale. And the nice thing about 172 00:09:36,500 --> 00:09:39,920 microcosms is that, because they're so small, you can 173 00:09:39,920 --> 00:09:42,640 standardize a bunch of experiments across the world, 174 00:09:42,640 --> 00:09:44,800 you can have a bunch of different labs doing a very 175 00:09:44,800 --> 00:09:48,040 similar experiment with different samples of water. So 176 00:09:48,040 --> 00:09:51,520 like you can go out and scoop ocean water off the coast of 177 00:09:51,580 --> 00:09:55,240 Maine or off the coast of Australia or off the coast of 178 00:09:55,360 --> 00:09:57,460 England, right? Like any of these places 179 00:09:57,520 --> 00:09:59,440 Craig Bettenhausen: and the mesocosms, these are in the 180 00:09:59,440 --> 00:10:02,520 water. But not the water can't pass from one side of this 181 00:10:02,580 --> 00:10:04,800 mesocosm out into the general correct 182 00:10:04,980 --> 00:10:07,620 Fionna Samuels: so the 1000 liter containers, the mesocosms, 183 00:10:07,680 --> 00:10:11,640 they are just containers in the ocean. The researchers flood the 184 00:10:11,640 --> 00:10:14,400 container, collect all this water and then make sure that if 185 00:10:14,400 --> 00:10:17,100 there are any fish or anything else accidentally get caught up, 186 00:10:17,100 --> 00:10:20,300 to remove the fish. Because that's too complex, they're 187 00:10:20,300 --> 00:10:23,360 really only interested in the plankton, the bottom of the food 188 00:10:23,360 --> 00:10:26,480 web at this point. Historically, the research so far has really 189 00:10:26,480 --> 00:10:29,360 only been interested at that level. Future research, though, 190 00:10:29,360 --> 00:10:32,840 might look at some fish larva, but yeah, and then that water is 191 00:10:32,840 --> 00:10:35,900 totally isolated from the surrounding water, so anything 192 00:10:35,900 --> 00:10:39,980 that's added to the mesocosm is contained within the mesocosm, 193 00:10:39,980 --> 00:10:43,060 and you don't worry about putting anything into the 194 00:10:43,060 --> 00:10:44,980 surrounding open water system. 195 00:10:44,980 --> 00:10:46,840 Craig Bettenhausen: Yeah. I wanted to ask about that because 196 00:10:46,840 --> 00:10:49,240 you encountered some critics, some people that aren't happy 197 00:10:49,240 --> 00:10:51,400 about this. Were they worried about the Loch Ness project 198 00:10:51,400 --> 00:10:54,280 specifically? Were they skeptical about ocean alkalinity 199 00:10:54,280 --> 00:10:56,560 enhancement, or were they against climate change 200 00:10:56,560 --> 00:10:58,660 mitigation as a whole effort? 201 00:10:58,780 --> 00:11:00,300 Fionna Samuels: Yeah, so I think, I think you're talking 202 00:11:00,300 --> 00:11:04,080 about James Carey, one of the sources in my story, yes, he was 203 00:11:04,140 --> 00:11:07,380 skeptical about Loch Ness specifically, but also about 204 00:11:07,380 --> 00:11:10,740 ocean alkalinity enhancement, more generally, Loch Ness, he's 205 00:11:10,740 --> 00:11:13,680 not totally convinced that they will be able to measure all the 206 00:11:13,680 --> 00:11:15,960 things that they want to measure, because it's just open 207 00:11:15,960 --> 00:11:19,320 water systems are incredibly complex, and so measuring 208 00:11:19,320 --> 00:11:23,720 anything in the open ocean is going to be very difficult. The 209 00:11:23,720 --> 00:11:28,040 Signal to Noise is very hard to tease out. So he was skeptical 210 00:11:28,040 --> 00:11:31,880 about that. But more broadly, I think he has concerns about 211 00:11:31,880 --> 00:11:35,840 scalability. And scalability is a big question in all of these 212 00:11:35,840 --> 00:11:40,420 things, because we are emitting so much carbon dioxide that it 213 00:11:40,420 --> 00:11:45,400 almost doesn't pay to do any of this before seriously figuring 214 00:11:45,400 --> 00:11:49,120 out ways to cut emissions. The scientists, of course, argue 215 00:11:49,120 --> 00:11:53,200 that we need to have a solid research based foundation to 216 00:11:53,380 --> 00:11:57,040 even have discussions about carbon dioxide removal on a 217 00:11:57,040 --> 00:12:00,840 grand scale. But others, of course, worry that focusing on 218 00:12:00,900 --> 00:12:04,800 research for future applications, sort of moves the 219 00:12:04,800 --> 00:12:08,640 goal post for the current needs of just emission reductions. 220 00:12:08,640 --> 00:12:09,000 Yeah, I run 221 00:12:09,000 --> 00:12:10,500 Craig Bettenhausen: into that debate a lot like I should be 222 00:12:10,500 --> 00:12:13,320 redoing this at all, and it's a lot of the same dynamics of a 223 00:12:13,320 --> 00:12:15,780 lot of people think we will need these carbon removal 224 00:12:15,780 --> 00:12:18,960 technologies a little bit down the line. But yeah, there's 225 00:12:19,140 --> 00:12:21,680 lower hanging fruit that we should be picking but it won't 226 00:12:21,680 --> 00:12:24,020 be ready then, if we don't start working on it. Now, it's a 227 00:12:24,020 --> 00:12:25,160 difficult balance. 228 00:12:25,160 --> 00:12:26,720 Fionna Samuels: Yeah, definitely. And again, all the 229 00:12:26,720 --> 00:12:30,560 researchers that I talked to were not interested in selling 230 00:12:30,560 --> 00:12:34,340 carbon credits and they weren't interested in trying to make 231 00:12:34,340 --> 00:12:38,300 this a commercial sort of opportunity. They're really just 232 00:12:38,300 --> 00:12:43,060 wondering, Will this work, and the models that climate 233 00:12:43,060 --> 00:12:46,900 scientists have run suggest that ocean alkalinity enhancement and 234 00:12:46,900 --> 00:12:50,380 other carbon dioxide removal techniques could be incredibly 235 00:12:50,380 --> 00:12:53,920 valuable, worthwhile pursuits in the fight against climate 236 00:12:53,920 --> 00:12:58,060 change. But without doing these experiments in the real world, 237 00:12:58,060 --> 00:13:01,920 in field trials, there's just a big question mark about whether 238 00:13:01,920 --> 00:13:05,040 the real world is too complicated for this to work. 239 00:13:05,040 --> 00:13:06,840 Craig Bettenhausen: I'm gonna reveal my chemist background and 240 00:13:06,840 --> 00:13:09,180 say I'm curious about at the lab scale, though. I mean, is there 241 00:13:09,180 --> 00:13:12,600 solid proof at the liter scale that making the solution more 242 00:13:12,600 --> 00:13:15,960 basic will cause carbon dioxide to dissolve into it? Do we have 243 00:13:15,960 --> 00:13:17,460 that basis? Really solid? 244 00:13:17,460 --> 00:13:20,120 Fionna Samuels: Yeah, they figured that out. They are 245 00:13:20,120 --> 00:13:23,960 confident that carbon dioxide will dissolve into water more 246 00:13:23,960 --> 00:13:27,140 readily if the water is more basic, which is actually part of 247 00:13:27,140 --> 00:13:31,040 the reason why the oceans are so powerful already. So the oceans 248 00:13:31,040 --> 00:13:34,280 are absorbing vast amounts of carbon dioxide every year, and 249 00:13:34,280 --> 00:13:40,240 that's because their sort of inherent pH is around 8.3 which 250 00:13:40,240 --> 00:13:44,260 is quite basic compared to other bodies of water. In fact, tap 251 00:13:44,260 --> 00:13:48,220 water is often more acidic than that, and sodium hydroxide is 252 00:13:48,220 --> 00:13:52,720 often used in municipal water treatment plants in order to 253 00:13:52,720 --> 00:13:57,340 change the pH which helps prevent corrosion from pipes. So 254 00:13:57,340 --> 00:14:00,520 you know, humans are already doing pH modification on our 255 00:14:00,520 --> 00:14:05,580 drinking water and the ocean is already super basic. It's just a 256 00:14:05,580 --> 00:14:08,760 question of whether or not we can see these effects in the 257 00:14:08,760 --> 00:14:11,220 real world, because the ocean is so huge. 258 00:14:11,340 --> 00:14:13,320 Craig Bettenhausen: Yeah. Are there any other characters from 259 00:14:13,320 --> 00:14:15,960 your interviews that you wanted to bring in but didn't quite 260 00:14:15,960 --> 00:14:17,760 Fionna Samuels: fit? That's a good question. Yeah, the section 261 00:14:17,760 --> 00:14:21,140 that ended up not going into the piece was really about how the 262 00:14:21,140 --> 00:14:23,660 researchers are communicating with the public about their 263 00:14:23,660 --> 00:14:27,260 work, which was more of like a social sciences kind of 264 00:14:27,320 --> 00:14:30,740 discussion. And those folks were all great, and there are some 265 00:14:30,740 --> 00:14:33,860 really fabulous social science research happening in this 266 00:14:33,860 --> 00:14:37,700 space, and really important takeaways, like you need to talk 267 00:14:37,700 --> 00:14:41,860 to stakeholders before starting your experiment, which seems 268 00:14:41,860 --> 00:14:45,700 really obvious, but sometimes scientists are so excited to, 269 00:14:46,000 --> 00:14:48,460 you know, go out and start collecting data that it might 270 00:14:48,460 --> 00:14:52,360 not occur to them that the people living in these areas 271 00:14:52,420 --> 00:14:57,760 will feel very betrayed, almost, if this kind of science happens 272 00:14:57,760 --> 00:15:00,840 without any of their input. And so it's incredible. Incredibly 273 00:15:00,840 --> 00:15:04,320 important to have the local communities involved in the 274 00:15:04,800 --> 00:15:08,700 whole scientific process from even before applications for 275 00:15:08,700 --> 00:15:09,960 permits are submitted. And 276 00:15:09,960 --> 00:15:11,760 Craig Bettenhausen: so, I mean, how was the community responding 277 00:15:11,760 --> 00:15:14,160 to the Loch Ness experiment? I mean, they had your person that 278 00:15:14,160 --> 00:15:16,560 was opposed to it because they didn't think it was going 279 00:15:16,560 --> 00:15:18,420 Fionna Samuels: to work, yeah. So there have been some vocal 280 00:15:18,420 --> 00:15:21,440 opponents in the local community, but it also seems 281 00:15:21,440 --> 00:15:25,820 like there was potentially less I mean, there was some reporting 282 00:15:25,880 --> 00:15:28,880 that there are local community members who are still not 283 00:15:28,880 --> 00:15:32,660 convinced that it's a good idea to put stuff into the water. But 284 00:15:32,660 --> 00:15:37,400 there were also the Loch Ness researchers did take lots of 285 00:15:37,460 --> 00:15:41,740 conversations into account and change some of their 286 00:15:41,740 --> 00:15:45,460 experimental design based on what the local fishing community 287 00:15:45,460 --> 00:15:49,120 said and other stakeholders wanted from the experiment. 288 00:15:49,120 --> 00:15:50,740 Craig Bettenhausen: Yes, I guess this is happening out of Cape 289 00:15:50,740 --> 00:15:53,440 Cod, and that is not an area known for a lot of community 290 00:15:53,440 --> 00:15:56,140 activism. It's not a quiet sit back and let everything happen 291 00:15:56,140 --> 00:15:57,340 to them, kind of a place, yeah, 292 00:15:57,700 --> 00:15:59,500 Fionna Samuels: the most important thing with all of 293 00:15:59,500 --> 00:16:03,900 these environmental field trials is to engage community members 294 00:16:03,960 --> 00:16:08,100 early and for the entire time that you're doing the 295 00:16:08,100 --> 00:16:11,940 experiment, and do more than it goes beyond just educating 296 00:16:11,940 --> 00:16:15,900 people. It actually requires that they are involved in the 297 00:16:15,900 --> 00:16:17,880 decision making process. So Cape Cod is not the 298 00:16:17,880 --> 00:16:19,320 Craig Bettenhausen: only place that they're looking at this 299 00:16:19,320 --> 00:16:22,280 kind of thing. There are some other experiments probing this 300 00:16:22,280 --> 00:16:24,680 idea of ocean alkalinity enhancement. 301 00:16:24,680 --> 00:16:26,540 Fionna Samuels: Yeah. So the other experiment that I talked 302 00:16:26,540 --> 00:16:29,480 about in the piece was really, really small scale, tiny scale 303 00:16:29,480 --> 00:16:32,720 off the coast of Australia. They're putting minerals down in 304 00:16:32,720 --> 00:16:36,560 the sediment in the water to just see how worms and other 305 00:16:36,560 --> 00:16:40,040 creatures that live down there will respond their results this 306 00:16:40,040 --> 00:16:43,960 really recent. It was our winter, their summer, but they 307 00:16:43,960 --> 00:16:47,020 just recently finished that project, and they told me that 308 00:16:47,020 --> 00:16:50,380 their results are promising. The worms don't seem to care. But 309 00:16:50,380 --> 00:16:54,340 the scale at which they were doing it is so small compared to 310 00:16:54,340 --> 00:16:56,080 what will need to happen. There 311 00:16:56,080 --> 00:16:58,060 Craig Bettenhausen: are scale where they're like swimming down 312 00:16:58,060 --> 00:16:59,920 there with a single vial. They're 313 00:16:59,920 --> 00:17:02,580 Fionna Samuels: swimming down with a single vial, opening it 314 00:17:02,580 --> 00:17:07,200 up, pouring it and then watching for a few weeks, taking samples 315 00:17:07,200 --> 00:17:10,620 every few weeks, and then taking up sediment samples. Obviously, 316 00:17:10,620 --> 00:17:14,460 that's such a small scale that that's not what any sort of real 317 00:17:14,460 --> 00:17:18,000 world application will look like. We do actually have 318 00:17:18,000 --> 00:17:21,140 examples of real world mineral applications. So there's a 319 00:17:21,140 --> 00:17:25,880 company called Vesta that has done some olivine trials where 320 00:17:25,880 --> 00:17:29,420 they've put huge amounts of crushed olivine sand along, I 321 00:17:29,420 --> 00:17:32,780 think it was the coast of New Jersey, and off the coast as 322 00:17:32,780 --> 00:17:37,280 well, obviously, tons and tons of crushed rock is a lot 323 00:17:37,280 --> 00:17:40,720 different than a tiny little bio of crushed rock. And they're 324 00:17:40,720 --> 00:17:44,800 interested in figuring out some kind of carbon credit, some way 325 00:17:44,800 --> 00:17:48,400 of making this technique profitable. If there's any 326 00:17:48,400 --> 00:17:51,220 future in these sorts of techniques, there should be 327 00:17:51,220 --> 00:17:56,020 small scale, very safe field trials before actually 328 00:17:56,080 --> 00:17:59,500 approaching anything that looks like what we would need to 329 00:17:59,740 --> 00:18:02,940 combat climate change in a real way, which is unfortunate. It's 330 00:18:02,940 --> 00:18:06,780 like such a bummer, right? Like, the best solution is for 331 00:18:06,780 --> 00:18:10,080 everyone to bike to work and go from there, 332 00:18:10,200 --> 00:18:12,900 Craig Bettenhausen: stop eating so much meat. Compost. Yeah, oh 333 00:18:12,900 --> 00:18:13,320 God. 334 00:18:13,920 --> 00:18:16,800 Fionna Samuels: There's this carbon dioxide removal technique 335 00:18:16,860 --> 00:18:21,200 where you use electricity to take carbon dioxide out of 336 00:18:21,200 --> 00:18:24,740 seawater and pretty much, and then you put that carbon dioxide 337 00:18:24,800 --> 00:18:28,160 into the ground, you inject it into some sort of geologic 338 00:18:28,160 --> 00:18:31,640 formation, pretty much everyone thought that that was a very 339 00:18:31,640 --> 00:18:36,620 silly approach, because the ocean is one of the most stable 340 00:18:36,740 --> 00:18:40,180 places for carbon dioxide to Live. Carbon dioxide is 341 00:18:40,180 --> 00:18:44,020 sequestered into carbonate, which is all of those sorts of 342 00:18:44,020 --> 00:18:47,620 ions that are in the ocean will stay in the ocean as carbonate 343 00:18:47,680 --> 00:18:53,560 for 10,000 years. So it's silly to take stable carbon dioxide 344 00:18:53,620 --> 00:18:56,680 out of the ocean to put somewhere else, because the 345 00:18:56,680 --> 00:19:00,480 ocean is a really good home for it. So 346 00:19:00,480 --> 00:19:02,100 Craig Bettenhausen: in June, actually, I'm going to visit a 347 00:19:02,100 --> 00:19:04,740 pilot rig in New York City, where a startup is testing a 348 00:19:04,740 --> 00:19:07,020 system like the enhanced ocean alkalinity that you're 349 00:19:07,020 --> 00:19:09,600 describing. They're going to add reactive alkaline minerals to 350 00:19:09,600 --> 00:19:12,120 remove CO two this time from the East River in New York, instead 351 00:19:12,120 --> 00:19:14,280 of the ocean. What should I ask them? What should I be looking 352 00:19:14,280 --> 00:19:14,940 for? What 353 00:19:16,320 --> 00:19:18,240 Fionna Samuels: you should ask them, how they're measuring how 354 00:19:18,240 --> 00:19:21,140 much carbon dioxide is being removed from the air, how 355 00:19:21,140 --> 00:19:23,540 they're measuring carbon dioxide uptake. All 356 00:19:23,000 --> 00:19:25,100 Craig Bettenhausen: right, so is there anything else to me 357 00:19:25,100 --> 00:19:27,080 reporting that you wish you could have fit in somehow? 358 00:19:27,170 --> 00:19:30,110 Fionna Samuels: The one thing that I didn't emphasize, and I 359 00:19:30,110 --> 00:19:33,620 would like to have emphasized, is that a big piece of all this 360 00:19:33,620 --> 00:19:37,250 research is what the researchers called monitoring, reporting and 361 00:19:37,250 --> 00:19:41,510 verification, and that goes into sort of figuring out if this is 362 00:19:41,510 --> 00:19:44,630 a usable technology for something like carbon credits. 363 00:19:44,660 --> 00:19:48,230 And what that means is that you need to be able to monitor how 364 00:19:48,230 --> 00:19:51,710 much carbon dioxide is removed. You need to be able to report 365 00:19:51,710 --> 00:19:54,770 it, which is a whole different sort of infrastructure that's 366 00:19:54,770 --> 00:19:58,250 separate from the science. And then you need to verify it so 367 00:19:58,250 --> 00:20:01,880 other people need to be able to come in. And measure the same 368 00:20:01,880 --> 00:20:05,570 thing that you measured. And a lot of this research right now 369 00:20:05,600 --> 00:20:08,960 depends on modeling. There are very few field trials, although 370 00:20:08,990 --> 00:20:12,980 it's a growing field so there will likely be more field trials 371 00:20:12,980 --> 00:20:16,130 in the near future, but monitoring carbon dioxide 372 00:20:16,130 --> 00:20:18,200 removal on a global scale is going to be incredibly 373 00:20:18,200 --> 00:20:21,740 challenging, which is why these sort of open field trials are so 374 00:20:21,740 --> 00:20:25,280 important, because if you can monitor it on the small scale, 375 00:20:25,340 --> 00:20:28,700 and you can prove that you are able to monitor how much carbon 376 00:20:28,700 --> 00:20:32,180 dioxide is removed on the small scale, and then other people are 377 00:20:32,180 --> 00:20:35,300 able to verify that you are measuring what you think you're 378 00:20:35,300 --> 00:20:40,100 measuring, then that basically opens the door to realistic 379 00:20:40,130 --> 00:20:41,990 sorts of deployments in the future. 380 00:20:42,170 --> 00:20:44,030 Craig Bettenhausen: Okay, well, Fiona, thanks for diving deep on 381 00:20:44,030 --> 00:20:44,660 this with us. 382 00:20:44,690 --> 00:20:46,550 Fionna Samuels: Thanks for having me. Thank you so much. 383 00:20:46,610 --> 00:20:47,810 Craig Bettenhausen: And I usually use that line. It's not 384 00:20:47,810 --> 00:20:49,190 always literal, but this time it was, 385 00:20:49,190 --> 00:20:52,430 Fionna Samuels: I was gonna say, that's a great pun you caught me 386 00:20:52,430 --> 00:20:53,570 off guard with that one. 387 00:20:55,370 --> 00:20:57,380 Craig Bettenhausen: You can find Fionna Samuels story about 388 00:20:57,380 --> 00:21:00,740 oceans as climate change allies on CNN website, or in the April 389 00:21:00,740 --> 00:21:04,340 14, 2025, print issue of CNN, we put a link in the show notes 390 00:21:04,340 --> 00:21:06,320 along with the episode credits. We'd love to know what you think 391 00:21:06,320 --> 00:21:08,750 of CNN uncovered. You can share your feedback with us by 392 00:21:08,750 --> 00:21:13,040 emailing C E N feedback at ACS, dot, O, R, G, you can find me on 393 00:21:13,040 --> 00:21:15,530 social media as at Craig of waffles, Fiona. How can 394 00:21:15,530 --> 00:21:16,520 listeners get in touch with you? 395 00:21:16,580 --> 00:21:18,950 Fionna Samuels: I'm at F Morningstar on blue sky. 396 00:21:19,160 --> 00:21:21,050 Craig Bettenhausen: All right, this has been C&EN uncovered a 397 00:21:21,050 --> 00:21:23,930 series from C&EN Stereo Chemistry. Stereo Chemistry is 398 00:21:23,930 --> 00:21:26,600 the official podcast of chemical and Engineering News. Chemical 399 00:21:26,600 --> 00:21:28,730 and Engineering News is an independent news outlet 400 00:21:28,730 --> 00:21:30,710 published by the American Chemical Society. Thanks for 401 00:21:30,710 --> 00:21:31,100 listening.