A 2.5D Reactive Transport Model for Fracture Alteration Simulation
Abstract
Understanding fracture alteration resulting from geochemical reactions is critical in predicting fluid migration in the subsurface and is relevant to multiple environmental challenges. Here in this paper, we present a novel 2.5D continuum reactive transport model that captures and predicts the spatial pattern of fracture aperture change and the development of an altered layer in the near-fracture region. The model considers permeability heterogeneity in the fracture plane and updates fracture apertures and flow fields based on local reactions. It tracks the reaction front of each mineral phase and calculates the thickness of the altered layer. Given this treatment, the model is able to account for the diffusion limitation on reaction rates associated with the altered layer. The model results are in good agreement with an experimental study in which a CO2-acidified brine was injected into a fracture in the Duperow Dolomite, causing dissolution of calcite and dolomite that result in the formation of a preferential flow channel and an altered layer. Finally, with an effective diffusion coefficient consistent with the experimentally observed porosity of the altered layer, the model captures the progressive decrease in the dissolution rate of the fast-reacting mineral in the altered layer.
- Authors:
-
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Univ. of California, Berkeley, CA (United States). Earth and Planetary Science
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States); Energy Frontier Research Centers (EFRC) (United States). Center for Nanoscale Control of Geologic CO2 (NCGC)
- Sponsoring Org.:
- USDOE Office of Science (SC), Basic Energy Sciences (BES)
- OSTI Identifier:
- 1439203
- Grant/Contract Number:
- AC02-05CH11231
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Environmental Science and Technology
- Additional Journal Information:
- Journal Volume: 50; Journal Issue: 14; Related Information: © 2016 American Chemical Society.; Journal ID: ISSN 0013-936X
- Publisher:
- American Chemical Society (ACS)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; 58 GEOSCIENCES
Citation Formats
Deng, Hang, Molins, Sergi, Steefel, Carl, DePaolo, Donald, Voltolini, Marco, Yang, Li, and Ajo-Franklin, Jonathan. A 2.5D Reactive Transport Model for Fracture Alteration Simulation. United States: N. p., 2016.
Web. doi:10.1021/acs.est.6b02184.
Deng, Hang, Molins, Sergi, Steefel, Carl, DePaolo, Donald, Voltolini, Marco, Yang, Li, & Ajo-Franklin, Jonathan. A 2.5D Reactive Transport Model for Fracture Alteration Simulation. United States. https://doi.org/10.1021/acs.est.6b02184
Deng, Hang, Molins, Sergi, Steefel, Carl, DePaolo, Donald, Voltolini, Marco, Yang, Li, and Ajo-Franklin, Jonathan. Thu .
"A 2.5D Reactive Transport Model for Fracture Alteration Simulation". United States. https://doi.org/10.1021/acs.est.6b02184. https://www.osti.gov/servlets/purl/1439203.
@article{osti_1439203,
title = {A 2.5D Reactive Transport Model for Fracture Alteration Simulation},
author = {Deng, Hang and Molins, Sergi and Steefel, Carl and DePaolo, Donald and Voltolini, Marco and Yang, Li and Ajo-Franklin, Jonathan},
abstractNote = {Understanding fracture alteration resulting from geochemical reactions is critical in predicting fluid migration in the subsurface and is relevant to multiple environmental challenges. Here in this paper, we present a novel 2.5D continuum reactive transport model that captures and predicts the spatial pattern of fracture aperture change and the development of an altered layer in the near-fracture region. The model considers permeability heterogeneity in the fracture plane and updates fracture apertures and flow fields based on local reactions. It tracks the reaction front of each mineral phase and calculates the thickness of the altered layer. Given this treatment, the model is able to account for the diffusion limitation on reaction rates associated with the altered layer. The model results are in good agreement with an experimental study in which a CO2-acidified brine was injected into a fracture in the Duperow Dolomite, causing dissolution of calcite and dolomite that result in the formation of a preferential flow channel and an altered layer. Finally, with an effective diffusion coefficient consistent with the experimentally observed porosity of the altered layer, the model captures the progressive decrease in the dissolution rate of the fast-reacting mineral in the altered layer.},
doi = {10.1021/acs.est.6b02184},
journal = {Environmental Science and Technology},
number = 14,
volume = 50,
place = {United States},
year = {Thu Jun 30 00:00:00 EDT 2016},
month = {Thu Jun 30 00:00:00 EDT 2016}
}
Web of Science
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