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Title: Molecular Dynamics Simulation of Hydration and Swelling of Mixed-Layer Clays

Abstract

Swelling of clay minerals is important to a broad class of problems in science and engineering. While the problem has been extensively studied experimentally, past molecular modeling of the phenomenon was focused on pure clays of one type or another. In practice, however, there is a diverse class of mixed-layer clays (MLCs) in sedimentary rock with intermixed stacking sequence of two or more types of distinct layers within a single crystal. In fact, more than 60% of sedimentary rocks in the U.S. contain various types of MLCs. In this work, we present the results, to our knowledge, of the first molecular dynamics simulation of hydration energetics and swelling of illite–montmorillonite (I–MMT) MLCs, the most common type of mixed clays. The swelling is studied as a function of the water concentration with three combinations of interlayer cations, namely, Na+ and K+. The hydration energies, the radial distribution functions, and the density profiles in the interlayer region are computed. For regular Na–MMT with layer charge concentrated in the octahedral sheet, weak cation–surface interaction results in fully hydrated ions and significant swelling. In the asymmetric interlayer of the MLC, however, the illite sheet with stronger interaction of surface and ions causes adsorption ofmore » the cations deep in the ditrigonal cavities of the siloxane surface. Given that the hydration enthalpy of K+ is smaller than that of Na+, its hydration shell is quite unstable compared with that of Na+. Therefore, swelling is inhibited as the ratio K+/Na+ increases. Finally, the results demonstrate the significant differences between the hydration and swelling properties of pure clays and the mixed ones, which have important implications in practice, particularly for sequestration of CO2 in sedimentary rock.« less

Authors:
 [1]; ORCiD logo [1]
  1. Univ. of Southern California, Los Angeles, CA (United States)
Publication Date:
Research Org.:
Energy Frontier Research Centers (EFRC) (United States). Center for Geologic Storage of CO2 (GSCO2); Univ. of Illinois at Urbana-Champaign, IL (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Basic Energy Sciences (BES)
OSTI Identifier:
1566349
Grant/Contract Number:  
SC0012504
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Physical Chemistry. C
Additional Journal Information:
Journal Volume: 122; Journal Issue: 26; Journal ID: ISSN 1932-7447
Publisher:
American Chemical Society
Country of Publication:
United States
Language:
English
Subject:
36 MATERIALS SCIENCE; defects; mechanical behavior; carbon sequestration; mesostructured materials

Citation Formats

Rahromostaqim, Mahsa, and Sahimi, Muhammad. Molecular Dynamics Simulation of Hydration and Swelling of Mixed-Layer Clays. United States: N. p., 2018. Web. doi:10.1021/acs.jpcc.8b03693.
Rahromostaqim, Mahsa, & Sahimi, Muhammad. Molecular Dynamics Simulation of Hydration and Swelling of Mixed-Layer Clays. United States. https://doi.org/10.1021/acs.jpcc.8b03693
Rahromostaqim, Mahsa, and Sahimi, Muhammad. Mon . "Molecular Dynamics Simulation of Hydration and Swelling of Mixed-Layer Clays". United States. https://doi.org/10.1021/acs.jpcc.8b03693. https://www.osti.gov/servlets/purl/1566349.
@article{osti_1566349,
title = {Molecular Dynamics Simulation of Hydration and Swelling of Mixed-Layer Clays},
author = {Rahromostaqim, Mahsa and Sahimi, Muhammad},
abstractNote = {Swelling of clay minerals is important to a broad class of problems in science and engineering. While the problem has been extensively studied experimentally, past molecular modeling of the phenomenon was focused on pure clays of one type or another. In practice, however, there is a diverse class of mixed-layer clays (MLCs) in sedimentary rock with intermixed stacking sequence of two or more types of distinct layers within a single crystal. In fact, more than 60% of sedimentary rocks in the U.S. contain various types of MLCs. In this work, we present the results, to our knowledge, of the first molecular dynamics simulation of hydration energetics and swelling of illite–montmorillonite (I–MMT) MLCs, the most common type of mixed clays. The swelling is studied as a function of the water concentration with three combinations of interlayer cations, namely, Na+ and K+. The hydration energies, the radial distribution functions, and the density profiles in the interlayer region are computed. For regular Na–MMT with layer charge concentrated in the octahedral sheet, weak cation–surface interaction results in fully hydrated ions and significant swelling. In the asymmetric interlayer of the MLC, however, the illite sheet with stronger interaction of surface and ions causes adsorption of the cations deep in the ditrigonal cavities of the siloxane surface. Given that the hydration enthalpy of K+ is smaller than that of Na+, its hydration shell is quite unstable compared with that of Na+. Therefore, swelling is inhibited as the ratio K+/Na+ increases. Finally, the results demonstrate the significant differences between the hydration and swelling properties of pure clays and the mixed ones, which have important implications in practice, particularly for sequestration of CO2 in sedimentary rock.},
doi = {10.1021/acs.jpcc.8b03693},
journal = {Journal of Physical Chemistry. C},
number = 26,
volume = 122,
place = {United States},
year = {Mon Jun 11 00:00:00 EDT 2018},
month = {Mon Jun 11 00:00:00 EDT 2018}
}

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Hertz‐Mindlin Theory of Contacting Grains and the Effective‐Medium Approximation for the Permeability of Deforming Porous Media
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Effect of Layer Charge Density on Hydration Properties of Montmorillonite: Molecular Dynamics Simulation and Experimental Study
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