%AEvans, Owen [Department of Applied Physics and Applied Mathematics Columbia University New York NY USA]%AEvans, Owen [Department of Applied Physics and Applied Mathematics, Columbia University, New York NY USA]%ASpiegelman, Marc [Department of Applied Physics and Applied Mathematics Columbia University New York NY USA, Lamont‐Doherty Earth Observatory Columbia University Palisades NY USA, Department of Earth and Environmental Sciences Columbia University New York NY USA]%ASpiegelman, Marc [Department of Applied Physics and Applied Mathematics, Columbia University, New York NY USA, Lamont-Doherty Earth Observatory, Columbia University, Palisades NY USA, Department of Earth and Environmental Sciences, Columbia University, New York NY USA]%AKelemen, Peter [Lamont‐Doherty Earth Observatory Columbia University Palisades NY USA, Department of Earth and Environmental Sciences Columbia University New York NY USA]%AKelemen, Peter [Lamont-Doherty Earth Observatory, Columbia University, Palisades NY USA, Department of Earth and Environmental Sciences, Columbia University, New York NY USA]%BJournal Name: Journal of Geophysical Research: Solid Earth; Journal Volume: 123; Journal Issue: 10; Related Information: CHORUS Timestamp: 2023-09-03 06:10:56 %D2018%IDOI PREFIX: 10.1029 %JJournal Name: Journal of Geophysical Research: Solid Earth; Journal Volume: 123; Journal Issue: 10; Related Information: CHORUS Timestamp: 2023-09-03 06:10:56 %K %MOSTI ID: 10078450 %PMedium: X %TA Poroelastic Model of Serpentinization: Exploring the Interplay Between Rheology, Surface Energy, Reaction, and Fluid Flow %X
The interactions between reactive fluids and solids are critical in Earth dynamics. Implications of such processes are wide ranging: from earthquake physics to geologic carbon sequestration and the cycling of fluids and volatiles through subduction zones. Peridotite alteration is a common feature in many of these processes, which—despite its obvious importance—is relatively poorly understood from a geodynamical perspective. In particular, although frequently observed in nature, it is still unknown how rocks can undergo 100% hydration/carbonation. One potential explanation of this observation is the mechanism of