Crystallographic Alignment and Phonon Corridors: Enhanced Hydrogen Production via Engineered Thermal Pathways in Ultramafic Rocks

Geological hydrogen Serpentinization Phonon transport Thermal conductivity anisotropy Crystallographic fabric Nanofoam Ultramafic rocks Supracrystalline alignment Enhanced geothermal systems Carbon mineralization Clean energy Flow-through reactors Radiolysis Methane generation Fischer-Tropsch reactions Thermal metamaterials Natural hydrogen systems Subsurface energy Phonon coherence length Olivine hydration

Authors

Volume 2025
Research Articles
May 27, 2025

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The optimization of subsurface hydrogen generation requires addressing fundamental heat transport limitations that constrain water-rock reactions. Here we present experimental validation of the Supracrystalline Phonon-Aligned Reaction Corridor (SPARC) framework, which demonstrates that crystallographic fabric alignment at mesoscopic scales (10⁻⁶ to 10⁻² m) creates preferential thermal pathways that significantly enhance hydrogen yields from both serpentinization and radiolytic processes.

Using our proprietary nitrogen hybrid nanofoam system (95% N₂ with 0.6-0.8% vol Al₂O₃ and 0.3-0.5% vol SiO₂ nanoparticles), we established aligned fracture networks in olivine-rich cores that exhibited remarkable thermal anisotropy. Laboratory measurements confirmed directional thermal conductivity of 30.5 ± 1.2 W/m·K along SPARC-aligned corridors—over three times higher than perpendicular orientations (9.8 ± 0.5 W/m·K) and conventional systems (10-11 W/m·K). High-resolution characterization revealed extended phonon coherence lengths of approximately 50 nm in aligned systems compared to <1 nm in isotropic matrices.

Flow-through experiments conducted at 200°C and 100 bar over 60 days demonstrated that SPARC-treated samples maintained stable fracture apertures (88% retention) while producing 78% more hydrogen than controls (32 mmol/kg vs. 18 mmol/kg). The reaction front propagation speed increased by 63% in structurally aligned domains, correlating directly with enhanced hydrogen yields. When CO₂ was introduced, methane generation increased nearly six-fold in SPARC systems (170 μmol/kg vs. 30 μmol/kg in controls), indicating improved catalytic conversion efficiency.

Our comprehensive characterization program employed electron backscatter diffraction, micro-computed tomography, laser flash analysis, time-domain thermoreflectance, and continuous monitoring of fluid chemistry to establish the relationship between structural alignment, thermal transport, and reaction productivity. These findings demonstrate that the SPARC approach successfully transforms conventional thermal barriers into conductive channels that guide heat directly to reaction sites, overcoming the self-limiting nature of serpentinization reactions.

This engineered enhancement of hydrogen production efficiency has significant implications for geothermal energy extraction, subsurface hydrogen resource development, and carbon mineralization technologies, providing a scalable approach to accelerate the deployment of geological hydrogen as a clean energy carrier.