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Title: Dissolution-Assisted Pattern Formation During Olivine Carbonation

Abstract

Olivine and pyroxene-bearing rocks in the oceanic crust react with hydrothermal fluids producing changes in the physical characteristics and behaviors of the altered rocks. Notably, these reactions tend to increase solid volume, reducing pore volume, permeability, and available reactive surface area, yet entirely hydrated and/or carbonated rocks are commonly observed in the field. We investigate the evolution of porosity and permeability of fractured dunites reacted with CO2-rich solutions in laboratory experiments. The alteration of crack surfaces changes the mechanical and transport properties of the bulk samples. Analysis of three-dimensional microstructural data shows that although precipitation of secondary minerals causes the total porosity of the sample to decrease, an interconnected network of porosity is maintained through channelized dissolution and coupled carbonate precipitation. The observed microstructure appears to be the result of chemo-mechanical coupling, which may provide a mechanism of porosity maintenance without the need to invoke reaction-driven cracking.

Authors:
ORCiD logo [1]; ORCiD logo [2];  [2];  [3]
  1. Univ. of Maryland, College Park, MD (United States); Stanford Univ., Stanford, CA (United States)
  2. Univ. of Maryland, College Park, MD (United States)
  3. Argonne National Lab. (ANL), Lemont, IL (United States)
Publication Date:
Research Org.:
Argonne National Lab. (ANL), Argonne, IL (United States); Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Basic Energy Sciences (BES)
OSTI Identifier:
1421960
Alternate Identifier(s):
OSTI ID: 1571935
Grant/Contract Number:  
AC02-06CH11357; AC02-05CH11231
Resource Type:
Accepted Manuscript
Journal Name:
Geophysical Research Letters
Additional Journal Information:
Journal Volume: 44; Journal Issue: 19; Journal ID: ISSN 0094-8276
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; Rock deformation; Permeability; Carbon sequestration, storage and utilization (CSSU); Ultramafic; Chemo-mechanical coupling; Fluid-rock interaction; Carbon mineralization.

Citation Formats

Lisabeth, Harrison, Zhu, Wenlu, Xing, Tiange, and De Andrade, Vincent. Dissolution-Assisted Pattern Formation During Olivine Carbonation. United States: N. p., 2017. Web. doi:10.1002/2017GL074393.
Lisabeth, Harrison, Zhu, Wenlu, Xing, Tiange, & De Andrade, Vincent. Dissolution-Assisted Pattern Formation During Olivine Carbonation. United States. https://doi.org/10.1002/2017GL074393
Lisabeth, Harrison, Zhu, Wenlu, Xing, Tiange, and De Andrade, Vincent. Thu . "Dissolution-Assisted Pattern Formation During Olivine Carbonation". United States. https://doi.org/10.1002/2017GL074393. https://www.osti.gov/servlets/purl/1421960.
@article{osti_1421960,
title = {Dissolution-Assisted Pattern Formation During Olivine Carbonation},
author = {Lisabeth, Harrison and Zhu, Wenlu and Xing, Tiange and De Andrade, Vincent},
abstractNote = {Olivine and pyroxene-bearing rocks in the oceanic crust react with hydrothermal fluids producing changes in the physical characteristics and behaviors of the altered rocks. Notably, these reactions tend to increase solid volume, reducing pore volume, permeability, and available reactive surface area, yet entirely hydrated and/or carbonated rocks are commonly observed in the field. We investigate the evolution of porosity and permeability of fractured dunites reacted with CO2-rich solutions in laboratory experiments. The alteration of crack surfaces changes the mechanical and transport properties of the bulk samples. Analysis of three-dimensional microstructural data shows that although precipitation of secondary minerals causes the total porosity of the sample to decrease, an interconnected network of porosity is maintained through channelized dissolution and coupled carbonate precipitation. The observed microstructure appears to be the result of chemo-mechanical coupling, which may provide a mechanism of porosity maintenance without the need to invoke reaction-driven cracking.},
doi = {10.1002/2017GL074393},
journal = {Geophysical Research Letters},
number = 19,
volume = 44,
place = {United States},
year = {2017},
month = {8}
}

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Works referenced in this record:

Experimental evidence for chemo-mechanical coupling during carbon mineralization in ultramafic rocks
journal, September 2017


Generation of evenly-spaced pressure-solution seams during (late) diagenesis: A kinetic theory
journal, June 1983

  • Merino, Enrique; Ortoleva, Peter; Strickholm, Peter
  • Contributions to Mineralogy and Petrology, Vol. 82, Issue 4
  • DOI: 10.1007/BF00399713

Stress from crystallization of salt
journal, September 2004


TomoPy: a framework for the analysis of synchrotron tomographic data
journal, August 2014

  • Gürsoy, Dogˇa; De Carlo, Francesco; Xiao, Xianghui
  • Journal of Synchrotron Radiation, Vol. 21, Issue 5
  • DOI: 10.1107/S1600577514013939

Effect of CO 2 -induced reactions on the mechanical behaviour of fractured wellbore cement
journal, September 2016

  • Wolterbeek, Timotheus K. T.; Hangx, Suzanne J. T.; Spiers, Christopher J.
  • Geomechanics for Energy and the Environment, Vol. 7
  • DOI: 10.1016/j.gete.2016.02.002

Experimental Study of Carbon Sequestration Reactions Controlled by the Percolation of CO 2 -Rich Brine through Peridotites
journal, February 2009

  • Andreani, M.; Luquot, L.; Gouze, P.
  • Environmental Science & Technology, Vol. 43, Issue 4
  • DOI: 10.1021/es8018429

In situ carbonation of peridotite for CO2 storage
journal, November 2008

  • Kelemen, P. B.; Matter, J.
  • Proceedings of the National Academy of Sciences, Vol. 105, Issue 45
  • DOI: 10.1073/pnas.0805794105

Controls on rock weathering rates by reaction-induced hierarchical fracturing
journal, November 2008

  • Røyne, Anja; Jamtveit, Bjørn; Mathiesen, Joachim
  • Earth and Planetary Science Letters, Vol. 275, Issue 3-4
  • DOI: 10.1016/j.epsl.2008.08.035

Mechanisms of classical crystal growth theory explain quartz and silicate dissolution behavior
journal, October 2005

  • Dove, P. M.; Han, N.; De Yoreo, J. J.
  • Proceedings of the National Academy of Sciences, Vol. 102, Issue 43
  • DOI: 10.1073/pnas.0507777102

Reaction enhanced permeability during retrogressive metamorphism
journal, March 2008

  • Jamtveit, B.; Malthesorenssen, A.; Kostenko, O.
  • Earth and Planetary Science Letters, Vol. 267, Issue 3-4
  • DOI: 10.1016/j.epsl.2007.12.016

Reaction-driven cracking during retrograde metamorphism: Olivine hydration and carbonation
journal, September 2012


Dissolution kinetics of fosteritic olivine at 90–150°C including effects of the presence of CO2
journal, September 2006


A Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal Field
journal, March 2005


The mechanism of reequilibration of solids in the presence of a fluid phase
journal, May 2007


Diffusion in fluid-bearing and slightly-melted rocks: experimental and numerical approaches illustrated by iron transport in dunite
journal, June 1991

  • Watson, E. Bruce
  • Contributions to Mineralogy and Petrology, Vol. 107, Issue 4
  • DOI: 10.1007/BF00310677

Massive serpentinite carbonation at Linnajavri, N-Norway: Massive serpentinite carbonation at Linnajavri, N-Norway
journal, July 2012


Peridotite dissolution and carbonation rates at fracture surfaces under conditions relevant for in situ mineralization of CO2
journal, April 2013


CO2 disposal by means of silicates
journal, June 1990


Nondilatant brittle deformation of serpentinites: Implications for Mohr-Coulomb theory and the strength of faults
journal, February 1997

  • Escartín, J.; Hirth, G.; Evans, B.
  • Journal of Geophysical Research: Solid Earth, Vol. 102, Issue B2
  • DOI: 10.1029/96JB02792

Scientific data exchange: a schema for HDF5-based storage of raw and analyzed data
journal, October 2014

  • De Carlo, Francesco; Gürsoy, Dogˇa; Marone, Federica
  • Journal of Synchrotron Radiation, Vol. 21, Issue 6
  • DOI: 10.1107/S160057751401604X

Testing the cation-hydration effect on the crystallization of Ca-Mg-CO3 systems
journal, October 2013

  • Xu, J.; Yan, C.; Zhang, F.
  • Proceedings of the National Academy of Sciences, Vol. 110, Issue 44
  • DOI: 10.1073/pnas.1307612110

Theory of Preferred Crystal Orientation Developed by Crystallization under Stress
journal, March 1959

  • Kamb, W. Barclay
  • The Journal of Geology, Vol. 67, Issue 2
  • DOI: 10.1086/626571

The interface-scale mechanism of reaction-induced fracturing during serpentinization
journal, December 2012

  • Plümper, Oliver; Røyne, Anja; Magrasó, Anna
  • Geology, Vol. 40, Issue 12
  • DOI: 10.1130/G33390.1

The effect of pore size on cementation in porous rocks
journal, February 2001


Dynamic control on serpentine crystallization in veins: Constraints on hydration processes in oceanic peridotites: SERPENTINE CRYSTALLIZATION
journal, February 2007

  • Andreani, M.; Mével, C.; Boullier, A. -M.
  • Geochemistry, Geophysics, Geosystems, Vol. 8, Issue 2
  • DOI: 10.1029/2006GC001373

Reaction-assisted hierarchical fracturing during serpentinization
journal, March 2008


Generalized Titarenko's algorithm for ring artefacts reduction
journal, October 2014


Sculpting of Rocks by Reactive Fluids
journal, July 2012


Experimental evidence of reaction-induced fracturing during olivine carbonation: Fracturing During Olivine Carbonation
journal, September 2016

  • Zhu, Wenlu; Fusseis, Florian; Lisabeth, Harrison
  • Geophysical Research Letters, Vol. 43, Issue 18
  • DOI: 10.1002/2016GL070834

Microstructure and porosity evolution during experimental carbonation of a natural peridotite
journal, December 2012


Wormhole formation and compact dissolution in single- and two-phase CO 2 -brine injections
journal, April 2015

  • Ott, Holger; Oedai, Sjaam
  • Geophysical Research Letters, Vol. 42, Issue 7
  • DOI: 10.1002/2015GL063582

Permeability of thermally cracked granite
journal, May 1992

  • Darot, Michel; Gueguen, Yves; Baratin, Marie-Laure
  • Geophysical Research Letters, Vol. 19, Issue 9
  • DOI: 10.1029/92GL00579

Geochemistry of subduction zone serpentinites: A review
journal, September 2013


Mechanisms controlling rupture shape during subcritical growth of joints in layered rocks
journal, January 2005

  • Savalli, Laura; Engelder, Terry
  • Geological Society of America Bulletin, Vol. 117, Issue 3
  • DOI: 10.1130/B25368.1

Nanoscale 3D imaging at the Advanced Photon Source
journal, May 2016


Use of Complex Pore Pressure Transients to Measure Permeability of Rocks
conference, April 2013

  • Boitnott, G. N.
  • SPE Annual Technical Conference and Exhibition
  • DOI: 10.2118/38717-MS

Works referencing / citing this record:

Intracrystalline Reaction-Induced Cracking in Olivine Evidenced by Hydration and Carbonation Experiments
journal, September 2018

  • Lafay, Romain; Montes-Hernandez, German; Renard, François
  • Minerals, Vol. 8, Issue 9
  • DOI: 10.3390/min8090412

Generating porosity during olivine carbonation via dissolution channels and expansion cracks
journal, January 2018