Opportunity Information: Apply for DE FOA 0002786
This opportunity is a Department of Energy ARPA-E Request for Information (RFI) focused on a possible future research program about using the subsurface as a kind of engineered chemical reactor to generate hydrogen and helium with little to no carbon emissions. It is not a grant solicitation and it is not accepting funding applications. Instead, ARPA-E is collecting technical and programmatic input from researchers, companies, and other stakeholders to help decide whether and how to shape a future funding program aimed at subsurface chemical production and the related challenge of separating and producing useful gases at the surface.
The core idea ARPA-E wants to pressure-test is whether underground environments can be intentionally stimulated to drive geochemical reactions that produce hydrogen at a cost level aligned with DOE's Hydrogen Shot goal of $1 per kilogram, while also potentially producing helium without carbon emissions. The RFI highlights that the subsurface already hosts a wide range of naturally occurring reactions, from abiogenic methane formation to rare cases such as natural nuclear fission, and asks whether those natural conditions can be harnessed and scaled in a controlled way. ARPA-E points to several subsurface features that resemble conditions used in industrial chemistry: elevated temperatures common in deep geothermal settings (roughly 175 to 400 degrees F), high pressures that increase predictably with depth (on the order of 10 kPa per meter), and rocks that can contain catalytically relevant metals such as nickel and iron. The RFI notes that pressures used in major industrial processes are reachable at typical drilling depths; for example, around 400 atmospheres, comparable to pressures found at about 2 km depth, which is within the range of many existing subsurface operations.
Within that broader framing, ARPA-E is especially interested in two subsurface contexts for hydrogen generation. The first is hard rock systems, particularly old Precambrian formations that make up a large fraction of continental crust. In these settings, hydrogen can be produced naturally through radiolysis, where radiation from radioactive decay splits water to form hydrogen and oxygen, and through serpentinization, where iron-bearing mafic and ultramafic rocks react with water in redox processes that produce hydrogen. The RFI references published estimates suggesting that natural terrestrial hydrogen seepage could correspond to a wide range, roughly 0.1 to 33 percent of today's global fossil-based hydrogen production, while emphasizing that uncertainty in actual production rates is large. ARPA-E is looking for information on whether these reactions can be accelerated or sustained through stimulation methods (for example, by managing water availability, temperature, permeability, reactive surface area, or other controllable parameters) so the subsurface can function as a practical "georeactor" for clean hydrogen.
The second context is hydrocarbon-rich basins, where ARPA-E is exploring whether hydrogen could be produced by cracking hydrocarbons underground and bringing only hydrogen to the surface while leaving carbon in place. The motivation is to avoid the large carbon emissions associated with conventional surface hydrogen production, which today is dominated by steam methane reforming and coal gasification. The RFI cites typical emissions intensities on the order of about 9 tons of CO2 per ton of H2 for steam methane reforming and about 19 tons of CO2 per ton of H2 for coal gasification. ARPA-E frames subsurface hydrogen-from-hydrocarbons as a hypothesis that might reduce or eliminate the need for separate surface carbon capture and sequestration steps, potentially lowering cost and complexity. At the same time, the RFI is explicit that it is not yet clear whether this approach is technically feasible at meaningful scale, whether the necessary reaction control and gas separation can be achieved, and whether it can be economically competitive with surface hydrogen production paired with carbon capture and storage.
Because the envisioned end state involves not only generating hydrogen (and possibly helium) underground but also collecting and purifying it, the RFI also signals interest in enabling technical advances in subsurface gas handling and separations. That includes practical issues like how gases move through porous or fractured media, how to manage competing reactions and byproducts, how to avoid loss mechanisms, and how to selectively produce, extract, and separate hydrogen and helium from other subsurface gases under real field conditions. Overall, ARPA-E is trying to understand what breakthroughs would be needed to make subsurface chemical synthesis and gas production a credible new clean energy pathway, and what the most promising technical routes, target formations, and development milestones might look like.
Administrative details in the notice clarify that this is an RFI under Funding Opportunity Number DE-FOA-0002786 (CFDA 81.135) issued by ARPA-E within DOE. There is no award ceiling and no expected number of awards because no funding is being offered through this RFI. Eligibility is described as unrestricted for providing information, meaning any type of entity may respond subject to any clarifications in the full RFI text. Responses were requested as PDFs submitted by email to ARPA-E-RFI@hq.doe.gov, with the deadline listed as 5:00 p.m. Eastern Time on July 11, 2022. The full RFI text and instructions were made available through the ARPA-E funding opportunity website (arpa-e-foa.energy.gov).Apply for DE FOA 0002786
- The Department of Energy, Advanced Research Projects Agency Energy in the opportunity zone benefits, science and technology and other research and development sector is offering a public funding opportunity titled "Request for Information (RFI): Stimulating Geochemical Reactions in the Subsurface for in-situ Generation of Hydrogen and Helium Production" and is now available to receive applicants.
- Interested and eligible applicants and submit their applications by referencing the CFDA number(s): 81.135.
- This funding opportunity was created on May 23, 2022.
- Applicants must submit their applications by Jul 11, 2022 Reponses to this RFI should be submitted in PDF format to the email address ARPA-E-RFI@hq.doe.gov by 500 p.m. Eastern Time on 7/11/2022. For further instruction, please review the RFI in its entirety at https://apra-e-foa.energy.gov.. (Agency may still review applications by suitable applicants for the remaining/unused allocated funding in 2026.)
- Eligible applicants include: Unrestricted (i.e., open to any type of entity above), subject to any clarification in text field entitled Additional Information on Eligibility.
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FAQs: DOE ARPA-E RFI on Subsurface Hydrogen and Helium "Georeactors" (DE-FOA-0002786)
1) What is this opportunity?
This notice is a Department of Energy (DOE) ARPA-E Request for Information (RFI) about a possible future research program. The concept being explored is whether the subsurface can be used as an engineered chemical reactor to generate hydrogen, and potentially helium, with little to no carbon emissions.
2) Is this a grant solicitation or a funding opportunity I can apply to?
No. This is not a grant solicitation and it is not accepting funding applications. ARPA-E is only collecting input to help decide whether to create (and how to shape) a future funding program.
3) What is ARPA-E trying to learn from the RFI?
ARPA-E is seeking technical and programmatic input from researchers, companies, and other stakeholders on whether subsurface environments can be intentionally stimulated to produce hydrogen at meaningful scale and cost, and what breakthroughs would be required to make subsurface chemical synthesis and gas production a credible clean energy pathway.
4) What is the core idea ARPA-E wants to "pressure-test"?
The core hypothesis is that underground environments might be stimulated and managed to drive geochemical reactions that produce hydrogen at a cost aligned with DOE's Hydrogen Shot goal of $1 per kilogram, while also potentially producing helium with little to no carbon emissions.
5) Why does ARPA-E think the subsurface could work like an industrial reactor?
The RFI points to several subsurface characteristics that resemble industrial chemistry conditions, including elevated temperatures common in deep geothermal settings (roughly 175 to 400 degrees F), high pressures that increase predictably with depth (on the order of 10 kPa per meter), and rocks that can contain catalytically relevant metals such as nickel and iron.
6) What pressure and depth ranges does the RFI highlight as relevant?
ARPA-E notes that industrially relevant pressures are reachable at typical drilling depths. As an example, around 400 atmospheres is comparable to pressures found at about 2 km depth, which is within the range of many existing subsurface operations.
7) What subsurface settings are of special interest for hydrogen generation?
The RFI highlights two main contexts: (1) hard rock systems (especially old Precambrian formations) and (2) hydrocarbon-rich basins where hydrogen might be produced from hydrocarbons underground.
8) Why are Precambrian hard rock systems mentioned?
ARPA-E points out that Precambrian formations make up a large fraction of continental crust and can host natural hydrogen-generating processes such as radiolysis and serpentinization.
9) What is radiolysis in the context of this RFI?
Radiolysis is described as a process where radiation from radioactive decay splits water to form hydrogen and oxygen, which can lead to natural hydrogen generation in some hard rock environments.
10) What is serpentinization in the context of this RFI?
Serpentinization is described as a redox reaction where iron-bearing mafic and ultramafic rocks react with water in ways that produce hydrogen.
11) Does the RFI claim we already know how much hydrogen the Earth naturally produces?
No. The RFI references published estimates suggesting natural terrestrial hydrogen seepage could correspond to a wide range (roughly 0.1 to 33 percent of today's global fossil-based hydrogen production), but it also emphasizes that uncertainty in actual production rates is large.
12) What kinds of stimulation or control methods is ARPA-E asking about for hard rock systems?
ARPA-E is looking for information on whether hydrogen-generating reactions could be accelerated or sustained by managing controllable parameters such as water availability, temperature, permeability, reactive surface area, or other factors that might enable the subsurface to function as a practical "georeactor" for clean hydrogen.
13) What is the hydrocarbon-basin idea ARPA-E is exploring?
In hydrocarbon-rich basins, ARPA-E is exploring a hypothesis that hydrogen could be produced by cracking hydrocarbons underground and bringing only hydrogen to the surface, while leaving carbon in place.
14) Why is ARPA-E interested in subsurface hydrogen from hydrocarbons?
The motivation described in the RFI is to avoid the large carbon emissions associated with conventional surface hydrogen production, which today is dominated by steam methane reforming and coal gasification.
15) What emissions numbers does the RFI cite for conventional hydrogen production?
The RFI cites typical emissions intensities of about 9 tons of CO2 per ton of H2 for steam methane reforming and about 19 tons of CO2 per ton of H2 for coal gasification.
16) Does the RFI say subsurface hydrocarbon cracking is proven to work?
No. ARPA-E is explicit that it is not yet clear whether this approach is technically feasible at meaningful scale, whether reaction control and gas separation can be achieved, or whether it can be economically competitive with surface hydrogen production paired with carbon capture and storage.
17) Why does the RFI focus on gas handling and separations?
The envisioned end state involves not only generating hydrogen (and possibly helium) underground, but also collecting and purifying it. The RFI therefore signals interest in advances in subsurface gas handling and separations, including how gases move through porous or fractured media, how to manage competing reactions and byproducts, how to avoid loss mechanisms, and how to selectively produce, extract, and separate hydrogen and helium from other subsurface gases under real field conditions.
18) Is helium part of this concept too?
Yes. The RFI discusses the possibility of producing both hydrogen and helium with little to no carbon emissions, and it highlights the related challenge of separating and producing useful gases at the surface.
19) What agency and program is issuing this RFI?
This is issued by ARPA-E within the U.S. Department of Energy (DOE).
20) What is the Funding Opportunity Number (FON) and CFDA listing?
The notice identifies Funding Opportunity Number DE-FOA-0002786 and CFDA 81.135.
21) Are there any awards, an award ceiling, or an expected number of awards?
No. Because this is an RFI and no funding is being offered through it, the notice states there is no award ceiling and no expected number of awards.
22) Who is eligible to respond to the RFI?
Eligibility is described as unrestricted for providing information, meaning any type of entity may respond, subject to any clarifications in the full RFI text.
23) How were responses requested to be submitted?
Responses were requested as PDFs submitted by email to ARPA-E-RFI@hq.doe.gov.
24) What was the deadline to submit an RFI response?
The deadline listed in the notice was 5:00 p.m. Eastern Time on July 11, 2022.
25) Where were the full RFI text and instructions posted?
The full RFI text and instructions were made available through the ARPA-E funding opportunity website at arpa-e-foa.energy.gov.
26) What should respondents focus on in their input, based on the notice?
Based on the notice, ARPA-E is looking for input on promising technical routes, target formations, the key technical hurdles and enabling breakthroughs (including reaction control and separations), and what development milestones a future program might use to evaluate progress toward credible subsurface hydrogen (and possibly helium) production.
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