The Science
Our Science page will provide in-depth explanations of our lab experiments and field pilot, as well as links to additional resources that apply to our technology.
Bennu was founded by scientists committed to addressing the existential threat of climate change. That commitment extends beyond emission reduction into broader environmental and community stewardship. Our team has been investigating methane elimination technology in the lab for years, and we’re excited to pilot our technology on Lomar shipping vessels throughout 2024.
Methane (CH₄), though less abundant than carbon dioxide (CO₂), has a much higher global warming potential (GWP) over a shorter timescale, making its removal crucial for mitigating climate change. Methane’s atmospheric lifetime is primarily governed by reactions with hydroxyl (OH) radicals, which break down various trace gases through oxidation.
The interaction between methane, ozone (O₃), and hydroxyl radicals forms a complex and dynamic part of atmospheric chemistry. Feedback mechanisms suggest that small changes in atmospheric composition can significantly affect global methane concentrations. Factors like temperature, sunlight, and emissions of reactive gases, such as NOx, influence the strength of the methane feedback system. Moreover, as methane levels rise, more hydroxyl radicals are consumed, which could reduce the atmosphere’s capacity to remove pollutants.
By targeting the O₃-to-OH pathway, we aim to reduce methane's overall atmospheric lifetime to help mitigate climate change.
Oxidative Down-Conversion of Methane via UV Generated Ozone and Hydroxyl Activation
Our technology focuses on the oxidative “down-conversion”of methane (sometimes called “cracking”) into less harmful products like carbon dioxide and water (H₂O) using a dual-wavelength ultraviolet (UV) approach. This process utilizes off-the-shelf germicidal UV lamps that produce 185 nm UV light, which generates ozone, and 254 nm UV light, which catalyzes downstream reactions. (Together we call these “UVZ”.)
The process begins with the generation of ozone when oxygen molecules (O₂) are dissociated by the high-energy 185 nm wavelength:
O₂ + 185 nm → 2O
O + O₂→O₃
Once ozone is formed, the second step involves exposing it to 254 nm UV radiation. This triggers a chain of reactions that dissociate ozone, recreating molecular oxygen and reactive oxygen atoms (O). These oxygen atoms then react with water vapor in the air to produce hydroxyl radicals which are the key players in methane oxidation:
O₃ + 254 nm UV→O₂ + O(¹D)
O(¹D) + H₂O→2OH
Once hydroxyl radicals are produced, they initiate the oxidation of methane through a series of reactions. The hydroxyl radical reacts with methane, abstracting a hydrogen atom and forming water and a methyl radical (CH₃):
OH + CH₄→H₂O + CH₃
The methyl radical then reacts with molecular oxygen, ultimately leading through a series of reactions to the formation of carbon dioxide and water again:
This reaction chain down-converts the highly potent greenhouse gas methane, into carbon dioxide and water, drastically reducing its impact on climate change.
Efficiency and Climate Impact
Methane has over 25 times the global warming potential of carbon dioxide over a 100-year period, making its reduction a critical target for climate mitigation. Our UVZ-based technology accelerates the natural methane oxidation process, which otherwise takes many years to occur. The dual-wavelength UVZ system ensures that both ozone generation and methane oxidation occur efficiently, significantly enhancing the rate of methane down-conversion.
By focusing on methane cracking, Bennu Climate directly addresses one of the largest contributors to atmospheric warming. This method can be applied across various industries and environments, offering a scalable solution for reducing greenhouse gases.
References
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Jacob, Daniel J. Introduction to Atmospheric Chemistry. doi:10.1515/9781400841547-012.
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Holmes, Christopher D. “Methane Feedback on Atmospheric Chemistry: Methods, Models, and Mechanisms.” Journal of Advances in Modeling Earth Systems, 2018. doi:10.1002/2017MS001196.
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Jackson, Robert B., et al. “Atmospheric Methane Removal: A Research Agenda.” Philosophical Transactions of the Royal Society A, 2021. doi:10.1098/rsta.2020.0454.
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Ming, Tingzhen, et al. “Perspectives on Removal of Atmospheric Methane.” Advances in Applied Energy, 2022. doi:10.1016/j.adapen.2022.100085.
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Wang, Yuyin, et al. “Atmospheric Removal of Methane by Enhancing the Natural Hydroxyl Radical Sink.” Greenhouse Gases: Science and Technology, 2022. doi:10.1002/ghg.2191.