Rates and mechanisms of mineral carbonation in peridotite: natural processes and recipes for enhanced, in situ CO2 capture and storage
Origin paper
Rates and mechanisms of mineral carbonation in peridotite: natural processes and recipes for enhanced, in situ CO2 capture and storage
In situ carbonation of peridotite for CO2 storage
A simple model of reaction-induced cracking applied to serpentinization and carbonation of peridotite
Reaction-driven cracking during retrograde metamorphism: Olivine hydration and carbonation
Geochemistry and petrology of listvenite in the Samail ophiolite, Sultanate of Oman: Complete carbonation of peridotite during ophiolite emplacement
Reaction path modeling of enhanced in situ CO2 mineralization for carbon sequestration in the peridotite of the Samail Ophiolite, Sultanate of Oman
Coexisting serpentine and quartz from carbonate-bearing serpentinized peridotite in the Samail Ophiolite, Oman
Thermodynamic constraints on mineral carbonation of serpentinized peridotite
Carbonation rates of peridotite in the Samail Ophiolite, Sultanate of Oman, constrained through 14C dating and stable isotopes
Permanent storage of carbon dioxide in geological reservoirs by mineral carbonation
Carbonation of Peridotite in The Oman Ophiolite
Massive serpentinite carbonation at Linnajavri, N–Norway
Characterization of hyperalkaline fluids produced by low‐temperature serpentinization of mantle peridotites in the Oman and Ligurian ophiolites
Modern water/rock reactions in Oman hyperalkaline peridotite aquifers and implications for microbial habitability
CARBONATED SERPENTINITE (LISTWANITE) AT ATLIN, BRITISH COLUMBIA: A GEOLOGICAL ANALOGUE TO CARBON DIOXIDE SEQUESTRATION
Field observations and theoretical studies relevant to enhance in situ carbonation of peridotite
The interface-scale mechanism of reaction-induced fracturing during serpentinization
Experimental study of carbon sequestration reactions controlled by the percolation of CO2-rich brine through peridotites.
Determining timescales of natural carbonation of peridotite in the Samail Ophiolite, Sultanate of Oman
Applications and limitations of U–Th disequilibria systematics for determining ages of carbonate alteration minerals in peridotite
Microstructure and porosity evolution during experimental carbonation of a natural peridotite
Carbonation of mantle peridotite by CO2-rich fluids: the formation of listvenites in the Advocate ophiolite complex (Newfoundland, Canada)
Controls on the stable isotope compositions of travertine from hyperalkaline springs in Oman: Insights from clumped isotope measurements
CO2 sequestration and extreme Mg depletion in serpentinized peridotite clasts from the Devonian Solund basin, SW-Norway
Etude pétro-structurale et géochimique des processus de serpentinisation et de carbonatation des péridotites de l’ophiolite d’Oman
From serpentinization to carbonation: New insights from a CO2 injection experiment
Mineralogical assemblages forming at hyperalkaline warm springs hosted on ultramafic rocks: A case study of Oman and Ligurian ophiolites
Fluid rock interactions on residual mantle peridotites overlain by shallow oceanic limestones: Insights from Wadi Fins, Sultanate of Oman
Reaction induced fracturing during replacement processes
Experimental study of carbonate formation in oceanic peridotite
Engineered carbon mineralization in ultramafic rocks for CO2 removal from air: Review and new insights
Reaction-assisted hierarchical fracturing during serpentinization
Serpentinization and carbon sequestration: A study of two ancient peridotite-hosted hydrothermal systems
Past And Present Serpentinisation of Ultramafic Rocks; An Example from the Semail Ophiolite Nappe of Northern Oman
Enhanced CO2-mineral sequestration by cyclic hydraulic fracturing and Si-rich fluid infiltration into serpentinites at Malentrata (Tuscany, Italy)
Iron partitioning and hydrogen generation during serpentinization of abyssal peridotites from 15°N on the Mid-Atlantic Ridge
Experimental evidence of reaction‐induced fracturing during olivine carbonation
Low Temperature Hydrogen Production and Habitability of a Hyperalkaline Serpentinite Aquifer in the Samail Ophiolite
In situ sequestration of atmospheric CO2 at low temperature and surface cracking of serpentinized peridotite in mine shafts
Reaction enhanced permeability during retrogressive metamorphism
Incipient hydration of mantle lithosphere at ridges: A reactive-percolation experiment
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Near-surface reaction of CO2-bearing fluids with silicate minerals in peridotite and basalt forms solid carbonate minerals. Such processes form abundant veins and travertine deposits, particularly in association with tectonically exposed mantle peridotite. This is important in the global carbon cycle, in weathering, and in understanding physical-chemical interaction during retrograde metamorphism. Enhancing the rate of such reactions is a proposed method for geologic CO2 storage, and perhaps for direct capture of CO2 from near-surface fluids. We review, synthesize, and extend inferences from a variety of sources. We include data from studies on natural peridotite carbonation processes, carbonation kinetics, feedback between permeability and volume change via reaction-driven cracking, and proposed methods for enhancing the rate of natural mineral carbonation via in situ processes (“at the outcrop”) rather than ex situ processes (“at the smokestack”).