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Dissolution‐Assisted Pattern Formation During Olivine Carbonation

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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

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Wormhole formation and compact dissolution in single‐ and two‐phase CO2‐brine injections
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Experimental evidence of reaction‐induced fracturing during olivine carbonation
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Stress from crystallization of salt
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Microstructure and porosity evolution during experimental carbonation of a natural peridotite
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Reaction-assisted hierarchical fracturing during serpentinization
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Reaction enhanced permeability during retrogressive metamorphism
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Controls on rock weathering rates by reaction-induced hierarchical fracturing
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Reaction-driven cracking during retrograde metamorphism: Olivine hydration and carbonation
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Experimental evidence for chemo-mechanical coupling during carbon mineralization in ultramafic rocks
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Dissolution kinetics of fosteritic olivine at 90–150°C including effects of the presence of CO2
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Peridotite dissolution and carbonation rates at fracture surfaces under conditions relevant for in situ mineralization of CO2
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Effect of CO 2 -induced reactions on the mechanical behaviour of fractured wellbore cement
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The mechanism of reequilibration of solids in the presence of a fluid phase
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Experimental Study of Carbon Sequestration Reactions Controlled by the Percolation of CO 2 -Rich Brine through Peridotites
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Dynamic control on serpentine crystallization in veins: Constraints on hydration processes in oceanic peridotites
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Permeability of thermally cracked granite
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CO2 disposal by means of silicates
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The effect of pore size on cementation in porous rocks
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Mechanisms of classical crystal growth theory explain quartz and silicate dissolution behavior
inferredcites →https://doi.org/10.1073/pnas.0805794105openalex-snapshot
In situ carbonation of peridotite for CO 2 storage
inferredcites →https://doi.org/10.1073/pnas.1307612110openalex-snapshot
Testing the cation-hydration effect on the crystallization of Ca–Mg–CO 3 systems
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Theory of Preferred Crystal Orientation Developed by Crystallization under Stress
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The mechanism of porosity formation during solvent-mediated phase transformations
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Generalized Titarenko's algorithm for ring artefacts reduction
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Massive serpentinite carbonation at Linnajavri, N–Norway
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Nanoscale 3D imaging at the Advanced Photon Source
inferredcites →https://doi.org/10.1126/science.1102556openalex-snapshot
A Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal Field
inferredcites →https://doi.org/10.1127/0935-1221/2004/0016-0731openalex-snapshot
Oriented, non-topotactic olivine serpentine replacement in mesh-textured, serpentinized peridotites
inferredcites →https://doi.org/10.1130/b25368.1openalex-snapshot
Mechanisms controlling rupture shape during subcritical growth of joints in layered rocks
inferredcites →https://doi.org/10.1130/g33390.1openalex-snapshot
The interface-scale mechanism of reaction-induced fracturing during serpentinization
inferredcites →https://doi.org/10.1515/9781501508233openalex-snapshot
Kinetics of Geochemical Processes
inferredcites →https://doi.org/10.2118/38717-msopenalex-snapshot
Use of Complex Pore Pressure Transients to Measure Permeability of Rocks
inferredcites →https://doi.org/10.7185/geochempersp.1.3openalex-snapshot
Sculpting of Rocks by Reactive Fluids

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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A Comprehensive Prediction and Interpretation of Concrete Corrosion Induced by Carbon Dioxide Using Machine Learning
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Reactive transport experiments of coupled carbonation and serpentinization in a natural serpentinite. Implication for hydrogen production and carbon geological storage
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Impact of particle size and vertical heterogeneity on carbonate precipitation and pore structure during natural olivine carbonation
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Additional file 1 of Aqueous alteration without initial water: possibility of organic-induced hydration of anhydrous silicates in meteorite parent bodies
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