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Title: Application of a pore-scale reactive transport model to a natural analog for reaction-induced pore alterations

Dissolved CO 2 in the subsurface resulting from geological CO 2 storage may react with minerals in fractured rocks, confined aquifers, or faults, resulting in mineral precipitation and dissolution. The overall rate of reaction can be affected by coupled processes including hydrodynamics, transport, and reactions at the (sub) pore-scale. In this work pore-scale modeling of coupled fluid flow, reactive transport, and heterogeneous reactions at the mineral surface is applied to account for permeability alterations caused by precipitation-induced pore-blocking. This paper is motivated by observations of CO 2 seeps from a natural CO 2 sequestration analog, Crystal Geyser, Utah. Observations along the surface exposure of the Little Grand Wash fault indicate the lateral migration of CO 2 seep sites (i.e., alteration zones) of 10–50 m width with spacing on the order of ~100 m over time. Sandstone permeability in alteration zones is reduced by 3–4 orders of magnitude by carbonate cementation compared to unaltered zones. One granular porous medium and one fracture network systems are used to conceptually represent permeable porous media and locations of conduits controlled by fault-segment intersections and/or topography, respectively. Simulation cases accounted for a range of reaction regimes characterized by the Damköhler (Da) and Peclet (Pe) numbers.more » Pore-scale simulation results demonstrate that combinations of transport (Pe), geochemical conditions (Da), solution chemistry, and pore and fracture configurations contributed to match key patterns observed in the field of how calcite precipitation alters flow paths by pore plugging. This comparison of simulation results with field observations reveals mechanistic explanations of the lateral migration and enhances our understanding of subsurface processes associated with the CO 2 injection. In addition, permeability and porosity relations are constructed from pore-scale simulations which account for a range of reaction regimes characterized by the Da and Pe numbers. Finally, the functional relationships obtained from pore-scale simulations can be used in a continuum scale model that may account for large-scale phenomena mimicking lateral migration of surface CO 2 seeps.« less
Authors:
 [1] ;  [2] ;  [1] ;  [2]
  1. Sandia National Lab. (SNL-NM), Albuquerque, NM (United States). Geomechanics Dept.
  2. Univ. of Texas, Austin, TX (United States). Bureau of Economic Geology
Publication Date:
Report Number(s):
SAND2016-3725J
Journal ID: ISSN 0920-4105; 638548
Grant/Contract Number:
AC04-94AL85000; SC0001114
Type:
Accepted Manuscript
Journal Name:
Journal of Petroleum Science and Engineering
Additional Journal Information:
Journal Volume: 155; Journal ID: ISSN 0920-4105
Publisher:
Elsevier
Research Org:
Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
Sponsoring Org:
USDOE Office of Science (SC), Basic Energy Sciences (BES) (SC-22)
Country of Publication:
United States
Language:
English
Subject:
02 PETROLEUM
OSTI Identifier:
1340241

Yoon, Hongkyu, Major, Jonathan, Dewers, Thomas, and Eichhubl, Peter. Application of a pore-scale reactive transport model to a natural analog for reaction-induced pore alterations. United States: N. p., Web. doi:10.1016/j.petrol.2017.01.002.
Yoon, Hongkyu, Major, Jonathan, Dewers, Thomas, & Eichhubl, Peter. Application of a pore-scale reactive transport model to a natural analog for reaction-induced pore alterations. United States. doi:10.1016/j.petrol.2017.01.002.
Yoon, Hongkyu, Major, Jonathan, Dewers, Thomas, and Eichhubl, Peter. 2017. "Application of a pore-scale reactive transport model to a natural analog for reaction-induced pore alterations". United States. doi:10.1016/j.petrol.2017.01.002. https://www.osti.gov/servlets/purl/1340241.
@article{osti_1340241,
title = {Application of a pore-scale reactive transport model to a natural analog for reaction-induced pore alterations},
author = {Yoon, Hongkyu and Major, Jonathan and Dewers, Thomas and Eichhubl, Peter},
abstractNote = {Dissolved CO2 in the subsurface resulting from geological CO2 storage may react with minerals in fractured rocks, confined aquifers, or faults, resulting in mineral precipitation and dissolution. The overall rate of reaction can be affected by coupled processes including hydrodynamics, transport, and reactions at the (sub) pore-scale. In this work pore-scale modeling of coupled fluid flow, reactive transport, and heterogeneous reactions at the mineral surface is applied to account for permeability alterations caused by precipitation-induced pore-blocking. This paper is motivated by observations of CO2 seeps from a natural CO2 sequestration analog, Crystal Geyser, Utah. Observations along the surface exposure of the Little Grand Wash fault indicate the lateral migration of CO2 seep sites (i.e., alteration zones) of 10–50 m width with spacing on the order of ~100 m over time. Sandstone permeability in alteration zones is reduced by 3–4 orders of magnitude by carbonate cementation compared to unaltered zones. One granular porous medium and one fracture network systems are used to conceptually represent permeable porous media and locations of conduits controlled by fault-segment intersections and/or topography, respectively. Simulation cases accounted for a range of reaction regimes characterized by the Damköhler (Da) and Peclet (Pe) numbers. Pore-scale simulation results demonstrate that combinations of transport (Pe), geochemical conditions (Da), solution chemistry, and pore and fracture configurations contributed to match key patterns observed in the field of how calcite precipitation alters flow paths by pore plugging. This comparison of simulation results with field observations reveals mechanistic explanations of the lateral migration and enhances our understanding of subsurface processes associated with the CO2 injection. In addition, permeability and porosity relations are constructed from pore-scale simulations which account for a range of reaction regimes characterized by the Da and Pe numbers. Finally, the functional relationships obtained from pore-scale simulations can be used in a continuum scale model that may account for large-scale phenomena mimicking lateral migration of surface CO2 seeps.},
doi = {10.1016/j.petrol.2017.01.002},
journal = {Journal of Petroleum Science and Engineering},
number = ,
volume = 155,
place = {United States},
year = {2017},
month = {1}
}