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DOE OSTI · 3424772

A Quantum Mechanical Study of Quartz (101) Interfacial Boundaries

Kubicki, James D. [University of Texas at El Paso, TX (United States)] (ORCID:0000000292779044)·Watts, Heath D. [University of Texas at El Paso, TX (United States)] (ORCID:0000000169935398)
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Abstract

Density functional theory (DFT) calculations were performed on periodic and molecular models to explore the energetics of bonding modes at quartz–quartz interfaces, common grain contacts in sandstones. Four interface types were modeled: H 2 O-mediated, silanol H-bond mediated, O–O peroxide bonds, and siloxane bonds. Each type of interface may exist in the subsurface of the Earth, depending upon water activity, temperature, and pressure, as interfacial structures are stable within DFT molecular dynamics simulations up to 473 K. The results predict interfacial energies SiOSi > SiOOSi > SiOH-6H 2 O > 2SiOH, as expected based on similar bond strengths in other systems. The proposed SiOOSi interface is not generally accounted for in chemomechanical models but could be important in sandstones at depth in the Earth. The implications for intergrain fracturing and H2 generation are discussed.

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Kubicki, James D. [University of Texas at El Paso, TX (United States)] (ORCID:0000000292779044), Watts, Heath D. [University of Texas at El Paso, TX (United States)] (ORCID:0000000169935398). 2026-08-03. A Quantum Mechanical Study of Quartz (101) Interfacial Boundaries. https://doi.org/10.1021/acs.jpcc.5c08350

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