🚨 Brand new paper alert!
Are you interested in natural hydrogen gas (H2), a potential green energy source?
Check out our new paper in the AAAS' Science Advances (a sister journal of Science Magazine), in which we show that natural H2 exploration should focus on mountain ranges. 😃
Link to paper: https://lnkd.in/e5d6B-WZ
A promising natural H2 source is the serpentinization of exhumed mantle material as it reacts with water. Using state-of-the-art geodynamic modelling methods, we trace where serpentinization is likely to occur during rifting and subsequent basin inversion / mountain building.
Serpentinization-related H2 generation is best known from rifted margins and spreading ridges.
Yet, we surprisingly find that yearly serpentinization capacity (and thus natural H2 generation capacity) can be up to 20x higher during mountain building than during initial rifting.
Combined with the much more likely presence of reservoir rocks that would allow for H2 accumulation during bulk serpentinization (in contrast to deep marine rift basins), mountain ranges are the place to be for natural H2 exploration!
We propose an orogenic natural H2 system concept, which shows the key ingredients for the successful development of natural H2 accumulations that can be drilled and explored. Alternatively, we may also consider directly drilling into the serpentinizing mantle rocks themselves.
Our work shows the importance of understanding the geodynamic factors that control the distribution of natural resources (and the use of modelling work). Such insights are of particular importance for the energy transition, given the vast amounts of resources we will need.
A big thank you to my co-authors Sascha Brune, Anne Glerum, Dylan Vasey, John Naliboff, Gianreto Manatschal, and Eric C. Gaucher, from GFZ Helmholtz Centre for Geosciences, University of Potsdam, Tufts University, New Mexico Institute of Mining and Technology, University of Strasbourg, and Lavoisier H2 Geoconsult for their help and support during this exciting research
Many thanks also to GFZ colleagues, reviewers, the paper editor, and the CIG / ASPECT development team.
This research was principally funded through a GFZ Helmholtz Centre for Geosciences Discovery Fellowship, with additional (financial) support from European Research Council (ERC), Helmholtz-Gemeinschaft / Helmholtz Association, University of Strasbourg, CNRS, Lavoisier H2 Geoconsult, and the Alliance for National High Performance Computing in Germany. I was also a visiting scientist at Université de Fribourg - Universität Freiburg during part of this research.