Geologic Hydrogen

Hydrogen is a clean energy carrier that could play a central role in the global shift toward sustainable energy systems. In the geologic environment, hydrogen is naturally generated during serpentinization reactions, when ultramafic rocks such as dunite react with water. These reactions not only transform minerals but also release hydrogen gas as a byproduct. Despite decades of study, however, the details of serpentinization remain poorly understood—particularly in intact rocks where the reactions modify permeability, induce stress, and even deform the rock due to the significant volume increase associated with mineral transformation.
Uncertainty over reaction rates is a major challenge: current estimates of hydrogen generation rates vary by several orders of magnitude, making it difficult to assess the economic viability of geologic hydrogen exploitation. At ERL, our research addresses this problem using a combination of field studies and laboratory experiments. Field outcrops provide a natural record of how serpentinization unfolds over geological time, while controlled experiments allow us to measure reaction rates directly and uncover the mechanisms that govern them.
Together, these approaches shed light on the kinetic and transport processes that regulate hydrogen production. Our findings reveal how permeability feedbacks can sustain serpentinization and generate permeability, offering crucial insights into both natural hydrogen reservoirs and potential engineered systems. By bridging fundamental geoscience with practical applications, we aim to inform the future development of geologic hydrogen as a clean, large-scale energy resource.
Image: Cross polarized image of an experimentally serpentinized dunite core. Large olivine grains are being broken down and transformed to serpentine while liberating hydrogen. Courtesy of Gage Coon.
Current ERL projects in this area:
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Modeling Supershear Earthquakes to Forecast Induced Seismicity Hazard
While the potential for subsurface fluid injection and extraction to trigger earthquakes has long been recognized, the sharp increase in the extent and vigor of injection-induced seismicity calls for much deeper understanding than is currently available. One of the features of some highly destructive earthquakes… more info
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Seismic Imaging, Inversion and Uncertainty Quantification
The algorithmic workhorse for creating a map of the subsurface from seismic surveys is full waveform inversion. Many fundamental questions remain wide open about it, including how to deal with the lack of convexity in optimization, how to make use of AI to speed it… more info













