Turning Carbon into Rocks: A New Approach
This method uses microbes to transform CO2 into solid rock.
Joseph J. Lee, Luke Plante, Brooke Pian, Sabrina Marecos, Sean A. Medin, Jacob D. Klug, Matthew C. Reid, Greeshma Gadikota, Esteban Gazel, Buz Barstow
― 5 min read
Table of Contents
- How Does CO2 Become Rock?
- Getting Help from Friendly Microbes
- The Race to Capture CO2
- What’s in it for the Metals?
- The Challenge of Extraction
- The Magic of Microbial Solutions
- What Happened Over Time?
- The Power of Sweet Alternatives
- Mutant Microbes to the Rescue
- The Big Picture
- Let’s Not Forget About pH
- The Future is Bright, But…
- Conclusion: Rocks, Microbes, and CO2-Oh My!
- Original Source
We are all aware that our planet is heating up. Over a trillion tonnes of carbon dioxide (CO2) from human activities are floating around in the atmosphere. This is not just a minor issue; it’s one of the biggest challenges we face today. To combat this, a special report has suggested we need to remove huge amounts of CO2 from the air every year. One method that’s gaining attention is turning CO2 into rock. Yes, you heard that right-rocks!
How Does CO2 Become Rock?
This clever process is called carbon mineralization. Think of it as turning a gas into a solid. To do this, we take certain types of rocks, known as Ultramafic Rocks, which are packed with minerals. When these rocks weather-kind of like how a cookie crumbles over time-they release Magnesium ions. These ions can then react with CO2, creating magnesite, a solid form of CO2. It's like nature's way of putting a cork in a bottle of carbon!
Getting Help from Friendly Microbes
Now here’s where it gets interesting: we can speed up this process using microbes. Specifically, a friendly little bug called Gluconobacter Oxydans can help. When this microbe is fed sugar, it produces a solution that can dissolve minerals in ultramafic rocks. The best part? It can do this way faster than what happens in nature!
The Race to Capture CO2
Naturally, this process is quite slow and could take hundreds of thousands of years to balance CO2 levels. So, we need a quick fix! While some may think of mechanical methods like crushing rocks, which can be effective, they are also expensive and energy-intensive. Enter G. oxydans! This microbe can efficiently pull metals from these rocks while also helping us store CO2.
What’s in it for the Metals?
Besides capturing CO2, ultramafic rocks are also home to valuable metals like nickel and cobalt, which we need for batteries and other technologies. We can recover these metals while also taking care of CO2. It’s like getting a two-for-one deal, but instead of tacos, you get carbon storage and metal recovery!
The Challenge of Extraction
While the potential is there, extracting metals from rocks is not a walk in the park. The traditional methods can be slow, requiring a lot of energy. However, using G. oxydans could help us leach out metals much more quickly and cost-effectively. Think of it like using a blender instead of a mortar and pestle; it just makes things easier and faster.
The Magic of Microbial Solutions
The biolixiviant produced by G. oxydans is quite magical. It can leach out magnesium ions from dunite-a type of ultramafic rock-far better than just using plain water. In fact, after just a day, it can be up to 20 times more effective! Imagine pouring some magic potion on the rocks and watching them spill out metal.
What Happened Over Time?
But wait, there’s more! If you let the magic potion work for longer, like three or even ten days, the extraction efficiency keeps getting better. In our tests, after 96 hours, the magnesium extraction was a whopping 42 times more than just using water! It’s like the longer you let the potion brew, the more treasure you find.
The Power of Sweet Alternatives
Now, let’s talk sugar-or rather, where to get it. Feeding G. oxydans regular glucose can get pricey, especially if we want to scale up this solution. Instead, we can use lignocellulosic sugars, which come from agricultural waste. It’s like having dessert made from leftover vegetables. Not the tastiest option, but it gets the job done and is way cheaper!
Mutant Microbes to the Rescue
We’ve also been tinkering with our friendly microbe. By using genetic engineering, we created a mutant strain of G. oxydans that can do even better at leaching metals. This mutant can increase metal extraction by 12%, just by changing a few genes. Who knew that science could bring a superhero to the party?
The Big Picture
So what does this all mean for us? If we can optimize these processes, we could potentially sequester one tonne of CO2 for just about $100. While that sounds expensive, it's a considerable drop from methods costing $358,000! If we could make that a reality, we could start tackling our climate issues one rock at a time.
Let’s Not Forget About pH
Of course, there are always hurdles (not on the banned list, thankfully!) to tackle. For example, the leachate's pH tends to be on the low side after all that mineral dissolving, which isn't ideal for turning that leachate into solid rock. We would need to adjust the pH to help the process along, but with a little creativity, we can find ways to do this using safe compounds.
The Future is Bright, But…
While we've made significant strides, there’s still much to learn about optimizing the use of G. oxydans for leaching. The clearer our path, the better we can tackle the massive task of removing excess CO2 from our air. It’s all about maximizing what we can extract while minimizing our resource costs-after all, we don’t want to put too much strain on our planet while we’re at it.
Conclusion: Rocks, Microbes, and CO2-Oh My!
In summary, we have a promising method of dealing with climate change by turning carbon into rocks, powered by friendly microbes. The potential of G. oxydans to help with this process, along with the chance to recover valuable metals, could lead us toward a more sustainable future. If we keep making advances and solving the remaining challenges, we might just find ourselves on a solid path to a cooler planet. So here’s to rocks, microbes, and a cleaner environment!
Title: Bio-Accelerated Weathering of Ultramafic Minerals with Gluconobacter oxydans
Abstract: Ultramafic rocks are an abundant source of cations for CO2 mineralization (e.g., Mg) and elements for sustainability technologies (e.g., Ni, Cr, Mn, Co, Al). However, there is no industrially useful process for dissolving ultramafic materials to release cations for CO2 sequestration or mining them for energy-critical elements. Weathering of ultramafic rocks by rainwater, release of metal cations, and subsequent CO2 mineralization already naturally sequesters CO2 from the atmosphere, but this natural process will take thousands to hundreds of thousands of years to remove excess anthropogenic CO2, far too late to deal with global warming that will happen over the next century. Mechanical acceleration of weathering by grinding can accelerate cation release but is prohibitively expensive. In this article we show that gluconic acid-based lixiviants produced by the mineral-dissolving microbe Gluconobacter oxydans accelerate leaching of Mg2+ by 20x over deionized water, and that leaching of Mg, Mn, Fe, Co, and Ni further improves by 73% from 24 to 96 hours. At low pulp density (1%) the G. oxydans biolixiviant is only 6% more effective than gluconic acid. But, at 60% pulp density the G. oxydans biolixiviant is 3.2x more effective than just gluconic acid. We demonstrate that biolixiviants made with cellulosic hydrolysate are not significantly worse than biolixiviants made with glucose, dramatically improving the feedstock available for bioleaching. Finally, we demonstrate that we can reduce the number of carbon atoms in the biolixiviant feedstock (e.g., glucose or cellulosic hydrolysate) needed to release one Mg2+ ion and mineralize one atom of carbon from CO2 from 525 to 1.
Authors: Joseph J. Lee, Luke Plante, Brooke Pian, Sabrina Marecos, Sean A. Medin, Jacob D. Klug, Matthew C. Reid, Greeshma Gadikota, Esteban Gazel, Buz Barstow
Last Update: 2024-11-28 00:00:00
Language: English
Source URL: https://www.biorxiv.org/content/10.1101/2024.11.25.625253
Source PDF: https://www.biorxiv.org/content/10.1101/2024.11.25.625253.full.pdf
Licence: https://creativecommons.org/licenses/by-nc/4.0/
Changes: This summary was created with assistance from AI and may have inaccuracies. For accurate information, please refer to the original source documents linked here.
Thank you to biorxiv for use of its open access interoperability.