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<front>
<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Earth Sci.</journal-id>
<journal-title>Frontiers in Earth Science</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Earth Sci.</abbrev-journal-title>
<issn pub-type="epub">2296-6463</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="publisher-id">854816</article-id>
<article-id pub-id-type="doi">10.3389/feart.2022.854816</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Earth Science</subject>
<subj-group>
<subject>Original Research</subject>
</subj-group>
</subj-group>
</article-categories>
<title-group>
<article-title>Anisotropic Elastic Properties of Montmorillonite With Different Layer Charge Densities and Layer Charge Distributions Through Molecular Dynamic Simulation</article-title>
<alt-title alt-title-type="left-running-head">Wang et&#x20;al.</alt-title>
<alt-title alt-title-type="right-running-head">Anisotropic Elastic Properties of Montmorillonite</alt-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Wang</surname>
<given-names>Xueying</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1665992/overview"/>
</contrib>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Han</surname>
<given-names>Tongcheng</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="corresp" rid="c001">&#x2a;</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1588110/overview"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Fu</surname>
<given-names>Li-Yun</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/995373/overview"/>
</contrib>
</contrib-group>
<aff id="aff1">
<sup>1</sup>
<institution>Shandong Provincial Key Laboratory of Deep Oil and Gas</institution>, <institution>China University of Petroleum (East China)</institution>, <addr-line>Qingdao</addr-line>, <country>China</country>
</aff>
<aff id="aff2">
<sup>2</sup>
<institution>Laboratory for Marine Mineral Resources</institution>, <institution>Pilot National Laboratory for Marine Science and Technology</institution>, <addr-line>Qingdao</addr-line>, <country>China</country>
</aff>
<author-notes>
<fn fn-type="edited-by">
<p>
<bold>Edited by:</bold> <ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/1234578/overview">Lidong Dai</ext-link>, Institute of geochemistry (CAS), China</p>
</fn>
<fn fn-type="edited-by">
<p>
<bold>Reviewed by:</bold> <ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/1636566/overview">Guohui Chen</ext-link>, China University of Geosciences Wuhan, China</p>
<p>
<ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/1637216/overview">Junfang Zhang</ext-link>, Commonwealth Scientific and Industrial Research Organisation (CSIRO), Australia</p>
</fn>
<corresp id="c001">&#x2a;Correspondence: Tongcheng Han, <email>hantc@upc.edu.cn</email>
</corresp>
<fn fn-type="other">
<p>This article was submitted to Solid Earth Geophysics, a section of the journal Frontiers in Earth Science</p>
</fn>
</author-notes>
<pub-date pub-type="epub">
<day>17</day>
<month>02</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="collection">
<year>2022</year>
</pub-date>
<volume>10</volume>
<elocation-id>854816</elocation-id>
<history>
<date date-type="received">
<day>14</day>
<month>01</month>
<year>2022</year>
</date>
<date date-type="accepted">
<day>28</day>
<month>01</month>
<year>2022</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2022 Wang, Han and Fu.</copyright-statement>
<copyright-year>2022</copyright-year>
<copyright-holder>Wang, Han and Fu</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/">
<p>This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these&#x20;terms.</p>
</license>
</permissions>
<abstract>
<p>The knowledge of the anisotropic elastic properties of clay minerals is of crucial importance for the exploration and development of shale oil and gas. Montmorillonite (MMT) is a common natural clay mineral with different layer charge densities and layer charge distributions due to different geological conditions. Therefore, it is important to understand the currently poorly known effect of layer charge density and layer charge distribution on the anisotropic elastic properties of MMTs. This work aims to obtain such knowledge by studying the anisotropic elastic properties of different MMTs under stratigraphic conditions through molecular dynamic simulations. We showed that the in-plane compressional coefficients <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub> and <italic>C</italic>
<sub>12</sub> decrease with the increasing layer charge density for MMTs with different layer charge distributions, and the MMTs with the layer charges distributed on the two tetrahedral (T) sheets were found to have the smallest <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub> and <italic>C</italic>
<sub>12</sub>. We also showed that the out-of-plane compressional coefficients <italic>C</italic>
<sub>33</sub>, <italic>C</italic>
<sub>13</sub> and <italic>C</italic>
<sub>23</sub> of the MMTs with the layer charges distributed in the two T sheets decrease, while those with the layer charges in the octahedral (O) sheet increase and those with layer charges distributed in both the O sheet and the T sheets do not vary much with the increasing layer charge density. The variations of the anisotropic compressional elastic coefficients with different layer charge densities and layer charge distributions were found to be a result of the impact of the density and distribution of layer charges on the molecular interactions within the MMT layer. We further demonstrated that the layer charge density and layer charge distribution do not influence significantly the shear coefficients <italic>C</italic>
<sub>44</sub>, <italic>C</italic>
<sub>55</sub>, and <italic>C</italic>
<sub>66</sub>. The results revealed the mechanisms of how the density and distribution of layer charges affect the anisotropic elastic properties of MMTs and will contribute to the more successful exploration and development of unconventional resources in MMT bearing shale reservoirs.</p>
</abstract>
<kwd-group>
<kwd>montmorillonite</kwd>
<kwd>molecular dynamic simulation</kwd>
<kwd>elastic property</kwd>
<kwd>layer charge density</kwd>
<kwd>layer charge distribution</kwd>
</kwd-group>
<contract-num rid="cn001">41821002 42174136&#x20;41874151</contract-num>
<contract-num rid="cn002">ZR2021JQ14</contract-num>
<contract-sponsor id="cn001">National Natural Science Foundation of China<named-content content-type="fundref-id">10.13039/501100001809</named-content>
</contract-sponsor>
<contract-sponsor id="cn002">Natural Science Foundation of Shandong Province<named-content content-type="fundref-id">10.13039/501100007129</named-content>
</contract-sponsor>
</article-meta>
</front>
<body>
<sec id="s1">
<title>Introduction</title>
<p>In recent years, shale oil and gas have a contribution to a country&#x2019;s energy security by lowering the dependence on imported energy (<xref ref-type="bibr" rid="B27">Kobek et&#x20;al., 2015</xref>; <xref ref-type="bibr" rid="B34">Raszewski, 2016</xref>), and specifically the shale gas is considered to play a role as a bridging fuel to a low-carbon future (<xref ref-type="bibr" rid="B20">Kirkland, 2010</xref>; <xref ref-type="bibr" rid="B11">Few et&#x20;al., 2017</xref>). Exploration and development of shale oil and gas are drawing a lot of attentions (<xref ref-type="bibr" rid="B4">Chen et&#x20;al., 2021</xref>; <xref ref-type="bibr" rid="B30">Pu et&#x20;al., 2021</xref>), in which the knowledge about the elastic properties of shale is of vital importance because the elastic properties provide crucial geomechanical information required by seismic inversion to predict &#x201c;sweet spot&#x201d; (<xref ref-type="bibr" rid="B15">Han et&#x20;al., 2021</xref>) and by hydraulic fracturing projects to increase permeability for the flow of the hydrocarbon (<xref ref-type="bibr" rid="B33">Rahm, 2011</xref>; <xref ref-type="bibr" rid="B18">Bian et&#x20;al., 2019</xref>). Clay minerals, as the main mineral type and the matrix of shale, cause shale to be elastically anisotropic because of their layered structure (<xref ref-type="bibr" rid="B1">Bailey, 1966</xref>; <xref ref-type="bibr" rid="B44">Weaver and Pollard, 2011</xref>). In the process of shale oil and gas exploration and development, problems such as poor fracturing effect, high development cost, and great difficulty in finding sweet spot and stabilizing the borehole wall would arise if the influence of anisotropy is ignored (<xref ref-type="bibr" rid="B12">Gao et&#x20;al., 2021</xref>). Therefore, it is of great significance to study the anisotropic elastic properties of clay minerals for the exploration and development of shale oil and&#x20;gas.</p>
<p>Clay minerals, any of a group of important hydrous aluminum silicates with a layer (sheet-like) structure (<xref ref-type="bibr" rid="B14">Grim and Kodama, 2014</xref>), consist of some combinations of silicon tetrahedra (T) and aluminum octahedra (O) (<xref ref-type="bibr" rid="B10">Ebrahimi et&#x20;al., 2012</xref>). This work considers montmorillonite (MMT), a kind of clay mineral that has more significant swelling properties and expands more considerably than the other clay minerals, and therefore can more seriously affect the anisotropic elastic properties of shale (<xref ref-type="bibr" rid="B9">Dewhurst and Siggins, 2006</xref>; <xref ref-type="bibr" rid="B40">Sridharan, 2014</xref>; <xref ref-type="bibr" rid="B36">Sayers and den Boer, 2016</xref>). The experimental measurement of the anisotropic elastic properties of MMTs can be challenging because of their small grain particle size (<xref ref-type="bibr" rid="B42">Vanorio et&#x20;al., 2003</xref>; <xref ref-type="bibr" rid="B46">Zartman et&#x20;al., 2010</xref>). Alternatively, all-atom molecular simulation makes it possible to study the anisotropic elastic parameters of MMTs by simulating the motion of the MMT molecular system based on Newtonian mechanics. Many successful results, to date, have been obtained reporting the anisotropic elastic properties of MMTs under the effect of pressure, temperature, water content and interlayer cation types (<xref ref-type="bibr" rid="B10">Ebrahimi et&#x20;al., 2012</xref>; <xref ref-type="bibr" rid="B3">Carrier et&#x20;al., 2014</xref>; <xref ref-type="bibr" rid="B48">Zhao et&#x20;al., 2021</xref>), which are of significance to understand the elastic anisotropy of clay minerals.</p>
<p>However, isomorphous substitution is always associated with MMTs, making them contain different layer charge densities and different layer charge distributions because of the number and locations of the isomorphous substitution (<xref ref-type="bibr" rid="B46">Zartman et&#x20;al., 2010</xref>; <xref ref-type="bibr" rid="B17">Herling et&#x20;al., 2012</xref>). Previous researches show that the different layer charge densities and layer charge distributions can significantly affect the physicochemical properties of MMTs such as the exfoliation performance (<xref ref-type="bibr" rid="B49">Zhong et&#x20;al., 2021</xref>), the adsorption capacity (<xref ref-type="bibr" rid="B25">Lee et&#x20;al., 2005</xref>; <xref ref-type="bibr" rid="B2">Barrientos-Vel&#xe1;zquez et&#x20;al., 2016</xref>; <xref ref-type="bibr" rid="B22">Koutsopoulou et&#x20;al., 2020</xref>), the hydration performance (<xref ref-type="bibr" rid="B32">Qiu et&#x20;al., 2019</xref>), the swelling properties (<xref ref-type="bibr" rid="B41">Teich-McGoldrick et&#x20;al., 2015</xref>; <xref ref-type="bibr" rid="B7">Daab et&#x20;al., 2018</xref>; <xref ref-type="bibr" rid="B13">Ghasemi and Sharifi, 2021</xref>), and the thermal stability (<xref ref-type="bibr" rid="B31">Qin et&#x20;al., 2021</xref>) among others. Moreover, the structures of MMTs are also influenced by different layer charge densities and layer charge distributions. For instance, the basal layer spacing and interlayer spacing can be affected by different layer charge densities and distributions (<xref ref-type="bibr" rid="B28">Peng et&#x20;al., 2021</xref>) and the introduction of the substitutions generates structural tension to the layer structure leading to the structure expansion (<xref ref-type="bibr" rid="B23">Lavikainen et&#x20;al., 2016</xref>). Since the anisotropic elastic properties of MMTs are strongly correlated with their structure (<xref ref-type="bibr" rid="B49">Zhong et&#x20;al., 2021</xref>), the variation of structure may potentially cause a change in the anisotropic elastic properties of MMTs. However, there are very few studies reporting the anisotropic elastic properties of MMTs with different layer charge densities and layer charge distributions. Therefore, it is necessary to study the influences of different layer charge densities and layer charge distributions on the anisotropic elastic properties of MMTs to strengthen our understanding of the elastic properties of clay minerals.</p>
<p>This work aims to investigate the influence of different layer charge densities and layer charge distributions on the anisotropic elastic properties of MMTs through dedicated molecular dynamic simulation. To achieve this goal, we first build a series of MMT models with different layer charge densities and layer charge distributions by molecular mechanics. The anisotropic elastic parameters of the different MMT models are subsequently calculated under stratigraphic conditions using molecular dynamic simulation. The relationships between the anisotropic elastic parameters and the different charge densities and layer charge distributions are finally analyzed and interpreted.</p>
</sec>
<sec sec-type="methods" id="s2">
<title>Methods</title>
<sec id="s2-1">
<title>Model Establishment</title>
<p>In this study, we construct the MMT model from the structure of pyrophyllite unit cell with the crystal constant <italic>a</italic>&#x20;&#x3d; 0.5160 nm, <italic>b</italic>&#x20;&#x3d; 0.8966 nm, <italic>c</italic>&#x20;&#x3d; 0.9347 nm, and <italic>&#x3b1;</italic> &#x3d; 91.18&#xb0;, <italic>&#x3b2;</italic> &#x3d; 100.46&#xb0;, and <italic>&#x3b3;</italic> &#x3d; 89.64&#xb0; (<xref ref-type="bibr" rid="B24">Lee and Guggenheim, 1981</xref>; <xref ref-type="bibr" rid="B38">Skipper et&#x20;al., 1995</xref>). The pyrophyllite unit cell <inline-formula id="inf1">
<mml:math id="m1">
<mml:mrow>
<mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mtext>Al</mml:mtext>
</mml:mrow>
<mml:mn>4</mml:mn>
</mml:msub>
<mml:msub>
<mml:mtext>O</mml:mtext>
<mml:mn>4</mml:mn>
</mml:msub>
<mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mtext>OH</mml:mtext>
<mml:mo>)</mml:mo>
</mml:mrow>
<mml:mn>4</mml:mn>
</mml:msub>
<mml:msub>
<mml:mrow>
<mml:mo>)</mml:mo>
<mml:mo>(</mml:mo>
<mml:mtext>Si</mml:mtext>
</mml:mrow>
<mml:mn>8</mml:mn>
</mml:msub>
<mml:msub>
<mml:mtext>O</mml:mtext>
<mml:mrow>
<mml:mn>12</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:math>
</inline-formula> is then replicated (8 &#xd7; 6&#x20;&#xd7; 2) along the <italic>a</italic>, <italic>b</italic>, and <italic>c</italic> crystallographic directions, respectively to form a supercell of two TOT clay layers. The sizes of the replicated cell are <italic>Lx</italic> &#x3d; 4.1280&#xa0;nm, <italic>Ly</italic> &#x3d; 5.3796&#xa0;nm and <italic>Lz</italic> &#x3d; 1.8694&#xa0;nm. The constructed supercell not only decreases the subsequent excessive ordering of isomorphous substitution but also ensures that the atom in MMTs does not interact with its image in the next cell, when three-dimensional periodic boundary conditions are applied.</p>
<p>Based on the formed supercell, the isomorphous substitutions of octahedral Mg atom for Al atom and tetrahedral Al atom for Si atom with various compositions are introduced to establish different MMT models needed in this paper. Since one isomorphous substitution produces one negative charge (referring to the Supporting Information for details), which is referred to as the layer charge (<xref ref-type="bibr" rid="B19">Karnland, 2010</xref>), we introduce 48, 60, 72, 96, and 108 isomorphous substitutions to obtain the MMT models with the layer charge density (defined as the ratio between the number of layer charge to the number of unit cell, which is 96) of &#x2212;0.5, &#x2212;0.625, &#x2212;0.75, &#x2212;1.0, and &#x2212;1.125 e/uc, respectively. For the MMT models with each layer charge density, three different isomorphous substitution positions, i.e.,&#x20;complete tetrahedral substitutions in the T sheet, entire octahedral substitutions in the O sheet and the ratio of the tetrahedral to octahedral substitutions is 1:1, are designed and the corresponding MMT models are denoted as M1, M2, and M3, respectively. All isomorphous substitutions obey Lowenstein&#x2019;s substitution rule (i.e.,&#x20;the substitution sites cannot be adjacent to each other). We finally add the same number of Na cations as the layer charge between the layers of the MMT models to make sure that each MMT system is electrically neutral. Eventually, fifteen MMT models are established. <xref ref-type="fig" rid="F1">Figure&#x20;1</xref> shows the schematic view of the three MMT models and the snapshot of the molecular dynamic simulation supercell for the M3 Model with the layer charge of 0.75 e/uc.</p>
<fig id="F1" position="float">
<label>FIGURE 1</label>
<caption>
<p>Schematic views of <bold>(A)</bold> the two unit cells for the M1 Model, <bold>(B)</bold> the unit cell for the M2 Model, and <bold>(C)</bold> the four unit cells for the M3 Model and snapshot of <bold>(D)</bold> the molecular dynamic simulation supercell for the M3 Model with the layer charge of 0.75 e/uc. The color code is Si (blue), Al (blue-grey), Mg (orange), O (red), H (pink), and Na (yellow). The atoms in the black circle are the representative atoms of replacement.</p>
</caption>
<graphic xlink:href="feart-10-854816-g001.tif"/>
</fig>
</sec>
<sec id="s2-2">
<title>Elastic Tensor Computation</title>
<p>In our molecular dynamic simulation, the Parinello&#x2212;Rahman (PR) strain fluctuation formula (<xref ref-type="bibr" rid="B35">Ray and Rahman, 1985</xref>; <xref ref-type="bibr" rid="B5">Cui et&#x20;al., 2007</xref>; <xref ref-type="bibr" rid="B3">Carrier et&#x20;al., 2014</xref>) is used to calculate the anisotropic elastic parameters in the constant-pressure and constant-temperature (NPT) ensemble. The PR strain fluctuation formula is given as<disp-formula id="e1">
<mml:math id="m2">
<mml:mrow>
<mml:msub>
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<mml:mi>k</mml:mi>
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</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:msub>
<mml:mi>K</mml:mi>
<mml:mi>B</mml:mi>
</mml:msub>
<mml:mi>T</mml:mi>
</mml:mrow>
<mml:mrow>
<mml:mrow>
<mml:mo>&#x2329;</mml:mo>
<mml:mi>V</mml:mi>
<mml:mo>&#x232a;</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:mfrac>
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<mml:mi>l</mml:mi>
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<mml:mo>&#x2212;</mml:mo>
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<mml:mo>&#x232a;</mml:mo>
</mml:mrow>
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<mml:mo>&#x2329;</mml:mo>
<mml:msub>
<mml:mi>&#x3b5;</mml:mi>
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<mml:mi>k</mml:mi>
<mml:mi>l</mml:mi>
</mml:mrow>
</mml:msub>
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</mml:mrow>
</mml:mrow>
<mml:mo>]</mml:mo>
</mml:mrow>
</mml:mrow>
<mml:mrow>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msup>
</mml:mrow>
</mml:math>
<label>(1)</label>
</disp-formula>where <inline-formula id="inf2">
<mml:math id="m3">
<mml:mrow>
<mml:msub>
<mml:mi>K</mml:mi>
<mml:mi>B</mml:mi>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula> is the Boltzmann constant, equal to 1.38065 &#xd7; 10<sup>&#x2013;23</sup>&#xa0;J/K, <italic>T</italic> is the temperature in Kelvin, <italic>V</italic> is the volume in cubic meters, <inline-formula id="inf3">
<mml:math id="m4">
<mml:mrow>
<mml:msub>
<mml:mi>&#x3b5;</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula> is the strain tensor, and <inline-formula id="inf4">
<mml:math id="m5">
<mml:mrow>
<mml:mtext>&#xa0;</mml:mtext>
<mml:mrow>
<mml:mo>&#x2329;</mml:mo>
<mml:mi mathvariant="italic">&#x25aa;</mml:mi>
<mml:mo>&#x232a;</mml:mo>
</mml:mrow>
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</inline-formula> denotes the ensemble average. The subscripts <italic>i</italic>, <italic>j</italic>, <italic>k</italic> and <italic>l</italic> run from one to three and represent the three dimensions in the Cartesian coordinates. The indexes one and two correspond to the <italic>x-</italic> and <italic>y-</italic>axes, respectively, which are parallel to the MMT layer, and the index three corresponds to the <italic>z</italic>-axis, which is perpendicular to the MMT layer. The strain tensor <inline-formula id="inf5">
<mml:math id="m6">
<mml:mrow>
<mml:msub>
<mml:mi>&#x3b5;</mml:mi>
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<mml:mi>j</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula> can be determined by<disp-formula id="e2">
<mml:math id="m7">
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<mml:mrow>
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</mml:msub>
<mml:mo>&#x3d;</mml:mo>
<mml:mfrac>
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<mml:mrow>
<mml:mo>[</mml:mo>
<mml:mrow>
<mml:msubsup>
<mml:mrow>
<mml:mrow>
<mml:mo>&#x2329;</mml:mo>
<mml:mi>h</mml:mi>
<mml:mo>&#x232a;</mml:mo>
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<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>k</mml:mi>
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<mml:mrow>
<mml:mo>&#x2212;</mml:mo>
<mml:mi>T</mml:mi>
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<mml:msubsup>
<mml:mi>h</mml:mi>
<mml:mrow>
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<mml:mi>l</mml:mi>
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<mml:mi>T</mml:mi>
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<mml:msub>
<mml:mi>h</mml:mi>
<mml:mrow>
<mml:mi>l</mml:mi>
<mml:mi>m</mml:mi>
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<mml:msubsup>
<mml:mi>h</mml:mi>
<mml:mrow>
<mml:mi>m</mml:mi>
<mml:mi>j</mml:mi>
</mml:mrow>
<mml:mrow>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msubsup>
<mml:mo>&#x2212;</mml:mo>
<mml:msub>
<mml:mi>&#x3b4;</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
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</mml:mrow>
<mml:mo>]</mml:mo>
</mml:mrow>
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<label>(2)</label>
</disp-formula>where <inline-formula id="inf6">
<mml:math id="m8">
<mml:mrow>
<mml:msub>
<mml:mi>&#x3b4;</mml:mi>
<mml:mrow>
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<mml:mi>j</mml:mi>
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</inline-formula> is the Kronecker tensor, and <italic>h</italic> is the scaling matrix, which can be obtained through molecular dynamic simulation.</p>
<p>In this work, the LAMMPS code (<xref ref-type="bibr" rid="B29">Plimpton, 1995</xref>) is employed to perform the molecular dynamic simulation to obtain the scaling matrix <italic>h</italic>. In the simulation, a force field is required to describe the interactions of the atoms in the MMT, and we use the CLAYFF force field (<xref ref-type="bibr" rid="B6">Cygan et&#x20;al., 2004</xref>) for this purpose (the interaction parameters and charge of the relevant atoms are shown in the Supporting Information). The CLAYFF force field consists solely of the electrostatic terms, the Lennard-Jones terms and the O-H bond constrained by a harmonic bond stretch potential and is widely used in the simulations of clay minerals (<xref ref-type="bibr" rid="B10">Ebrahimi et&#x20;al., 2012</xref>; <xref ref-type="bibr" rid="B3">Carrier et&#x20;al., 2014</xref>). In our molecular dynamic simulations, we set the time step to be 1 fs in the NPT ensemble under stratigraphic conditions (i.e.,&#x20;<italic>p</italic>&#x20;&#x3d; 10&#xa0;MPa, and <italic>T</italic>&#x20;&#x3d; 323&#xa0;K). The Langevin dynamics and Nos&#xe9;&#x2212;Hoover barostat are used to control the pressure and temperature, respectively. The cutoff distance of the nonbonded interaction is set to be 10.0&#xa0;&#xc5;, and the long-range electrostatic interactions are calculated employing the particle-particle particle mesh (PPPM) method with an accuracy of 10<sup>&#x2013;4</sup>. The system is equilibrated for 2 ns. The box size (<italic>lx</italic>, <italic>ly</italic>, <italic>lz</italic>), tilt factors (<italic>xy</italic>, <italic>xz</italic>, <italic>yz</italic>) and volume of box (<italic>V</italic>) are then sampled every ten steps for 8&#xa0;ns<italic>.</italic> After that, the sample data (<italic>lx</italic>, <italic>ly</italic>, <italic>lz</italic>, <italic>xy</italic>, <italic>xz</italic>, <italic>yz</italic>) are sorted to form the scaling matrix <italic>h</italic> in the form of<disp-formula id="e3">
<mml:math id="m9">
<mml:mrow>
<mml:mi>h</mml:mi>
<mml:mo>&#x3d;</mml:mo>
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<mml:mo>&#xa0;</mml:mo>
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<mml:mtr>
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<mml:mtext>&#x200a;</mml:mtext>
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<mml:mtext>&#x200a;</mml:mtext>
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<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mi>l</mml:mi>
<mml:mi>y</mml:mi>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mi>y</mml:mi>
<mml:mi>z</mml:mi>
</mml:mrow>
</mml:mtd>
</mml:mtr>
<mml:mtr>
<mml:mtd>
<mml:mrow>
<mml:mn>0</mml:mn>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mn>0</mml:mn>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mtext>&#x200a;</mml:mtext>
<mml:mi>l</mml:mi>
<mml:mi>z</mml:mi>
</mml:mrow>
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</mml:mtable>
</mml:mrow>
<mml:mo>]</mml:mo>
</mml:mrow>
</mml:mrow>
</mml:math>
<label>(3)</label>
</disp-formula>
</p>
<p>Then the resulting scaling matrix <italic>h</italic> is substituted into <xref ref-type="disp-formula" rid="e2">Eq. 2</xref> to obtain the strain tensor <inline-formula id="inf7">
<mml:math id="m10">
<mml:mrow>
<mml:msub>
<mml:mi>&#x3b5;</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula>, which are further integrated into <xref ref-type="disp-formula" rid="e1">Eq. 1</xref> with <italic>V</italic> and <italic>T</italic> to determine the elastic tensors <inline-formula id="inf8">
<mml:math id="m11">
<mml:mrow>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
<mml:mi>k</mml:mi>
<mml:mi>l</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula> of the&#x20;MMTs.</p>
<p>When we show the elastic tensors, the Voigt notation is used to represent the calculated fourth-order stiffness tensor <inline-formula id="inf9">
<mml:math id="m12">
<mml:mrow>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
<mml:mi>k</mml:mi>
<mml:mi>l</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula> by the second-order tensors <inline-formula id="inf10">
<mml:math id="m13">
<mml:mrow>
<mml:msub>
<mml:mi>C</mml:mi>
<mml:mrow>
<mml:mi>i</mml:mi>
<mml:mi>j</mml:mi>
</mml:mrow>
</mml:msub>
</mml:mrow>
</mml:math>
</inline-formula> <italic>.</italic> The indexes change as follows: <inline-formula id="inf11">
<mml:math id="m14">
<mml:mrow>
<mml:mn>11</mml:mn>
<mml:mo>&#x2192;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:math>
</inline-formula>, <inline-formula id="inf12">
<mml:math id="m15">
<mml:mrow>
<mml:mn>22</mml:mn>
<mml:mo>&#x2192;</mml:mo>
<mml:mn>2</mml:mn>
</mml:mrow>
</mml:math>
</inline-formula>, <inline-formula id="inf13">
<mml:math id="m16">
<mml:mrow>
<mml:mn>33</mml:mn>
<mml:mo>&#x2192;</mml:mo>
<mml:mn>3</mml:mn>
</mml:mrow>
</mml:math>
</inline-formula>, <inline-formula id="inf14">
<mml:math id="m17">
<mml:mrow>
<mml:mn>23</mml:mn>
<mml:mo>&#x2192;</mml:mo>
<mml:mn>4</mml:mn>
</mml:mrow>
</mml:math>
</inline-formula>, <inline-formula id="inf15">
<mml:math id="m18">
<mml:mrow>
<mml:mn>13</mml:mn>
<mml:mo>&#x2192;</mml:mo>
<mml:mn>5</mml:mn>
</mml:mrow>
</mml:math>
</inline-formula>, and <inline-formula id="inf16">
<mml:math id="m19">
<mml:mrow>
<mml:mn>12</mml:mn>
<mml:mo>&#x2192;</mml:mo>
<mml:mn>6</mml:mn>
</mml:mrow>
</mml:math>
</inline-formula>. The indexes 1, 2, and three correspond to the compressions in the <italic>x</italic>, <italic>y</italic>, and <italic>z</italic> directions, respectively, and the indexes 4, 5, and six correspond to the shears in the <italic>yz-</italic>, <italic>xz-</italic>, and <italic>xy</italic>-planes, respectively. Although 36 coefficients of the stiffness tensor are computed, we only report the nine coefficients <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, <italic>C</italic>
<sub>12</sub>, <italic>C</italic>
<sub>33</sub>, <italic>C</italic>
<sub>13</sub>, <italic>C</italic>
<sub>23</sub>, <italic>C</italic>
<sub>44</sub>, <italic>C</italic>
<sub>55</sub>, and <italic>C</italic>
<sub>66</sub> because of the transverse isotropic characteristics of MMT (<xref ref-type="bibr" rid="B10">Ebrahimi et&#x20;al., 2012</xref>; <xref ref-type="bibr" rid="B3">Carrier et&#x20;al., 2014</xref>). According to the deformation modes involving the crystalline structure of the clay layer and interlayer space, the nine data are divided into three groups: the in-plane compressional coefficients <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub>, the out-of-plane compressional coefficients <italic>C</italic>
<sub>33</sub>, <italic>C</italic>
<sub>13</sub>, <italic>C</italic>
<sub>23</sub>, and the shear coefficients <italic>C</italic>
<sub>44</sub>, <italic>C</italic>
<sub>55</sub>, and&#x20;<italic>C</italic>
<sub>66</sub>.</p>
</sec>
</sec>
<sec sec-type="results|discussion" id="s3">
<title>Results and Discussion</title>
<p>Before presenting the simulation results of the anisotropic elastic coefficient with varying layer charge density and layer charge distribution, we need to test the validity of the employed method for the computation of the anisotropic elastic tensors. This is achieved by performing the calculation on the elastic coefficients of the MMT model [<inline-formula id="inf17">
<mml:math id="m20">
<mml:mrow>
<mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
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</mml:mrow>
<mml:mn>6</mml:mn>
</mml:msub>
<mml:msub>
<mml:mrow>
<mml:mo>[</mml:mo>
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</mml:mrow>
<mml:mrow>
<mml:mn>62</mml:mn>
</mml:mrow>
</mml:msub>
<mml:msub>
<mml:mrow>
<mml:mtext>Al</mml:mtext>
</mml:mrow>
<mml:mn>2</mml:mn>
</mml:msub>
<mml:msub>
<mml:mrow>
<mml:mo>]</mml:mo>
<mml:mo>[</mml:mo>
<mml:mtext>Al</mml:mtext>
</mml:mrow>
<mml:mrow>
<mml:mn>28</mml:mn>
</mml:mrow>
</mml:msub>
<mml:msub>
<mml:mrow>
<mml:mtext>Mg</mml:mtext>
</mml:mrow>
<mml:mn>4</mml:mn>
</mml:msub>
<mml:msub>
<mml:mrow>
<mml:mo>]</mml:mo>
<mml:mtext>O</mml:mtext>
</mml:mrow>
<mml:mrow>
<mml:mn>160</mml:mn>
</mml:mrow>
</mml:msub>
<mml:msub>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mtext>OH</mml:mtext>
<mml:mo>)</mml:mo>
</mml:mrow>
<mml:mrow>
<mml:mn>32</mml:mn>
</mml:mrow>
</mml:msub>
<mml:mo>)</mml:mo>
</mml:mrow>
</mml:math>
</inline-formula>] at the pressure and temperature of 1 Bar and 300&#xa0;K, respectively, and comparing the results with those published by <xref ref-type="bibr" rid="B3">Carrier et&#x20;al. (2014)</xref> using the same model at the same pressure and temperature. The comparison of the calculated elastic coefficients is given in <xref ref-type="table" rid="T1">Table&#x20;1</xref>, from which we can see that our calculated elastic coefficients are in good agreement with those of <xref ref-type="bibr" rid="B3">Carrier et&#x20;al. (2014)</xref>. The excellent agreement validates the computation method for the elastic tensors, and lays the foundation for the study of the anisotropic elastic properties of MMTs with different layer charge densities and layer charge distributions.</p>
<table-wrap id="T1" position="float">
<label>TABLE 1</label>
<caption>
<p>Comparison of calculated the elastic coefficients of the MMT at 1 Bar and 300&#xa0;K by <xref ref-type="bibr" rid="B3">Carrier et&#x20;al. (2014)</xref> and by the method provided in this&#x20;work.</p>
</caption>
<table>
<thead valign="top">
<tr>
<th align="left">
<italic>C</italic>
<sub>
<italic>ij</italic>
</sub> (GPa)</th>
<th align="center">
<italic>C</italic>
<sub>11</sub>
</th>
<th align="center">
<italic>C</italic>
<sub>22</sub>
</th>
<th align="center">
<italic>C</italic>
<sub>12</sub>
</th>
<th align="center">
<italic>C</italic>
<sub>13</sub>
</th>
<th align="center">
<italic>C</italic>
<sub>23</sub>
</th>
<th align="center">
<italic>C</italic>
<sub>33</sub>
</th>
<th align="center">
<italic>C</italic>
<sub>44</sub>
</th>
<th align="center">
<italic>C</italic>
<sub>55</sub>
</th>
<th align="center">
<italic>C</italic>
<sub>66</sub>
</th>
</tr>
</thead>
<tbody valign="top">
<tr>
<td align="left">
<xref ref-type="bibr" rid="B3">Carrier et&#x20;al. (2014)</xref>
</td>
<td align="char" char=".">292.3</td>
<td align="char" char=".">274.2</td>
<td align="char" char=".">132.4</td>
<td align="char" char=".">17.0</td>
<td align="char" char=".">17.3</td>
<td align="char" char=".">35.2</td>
<td align="char" char=".">10.6</td>
<td align="char" char=".">18.5</td>
<td align="char" char=".">82.3</td>
</tr>
<tr>
<td align="left">This study</td>
<td align="char" char=".">292.0</td>
<td align="char" char=".">276.1</td>
<td align="char" char=".">136.3</td>
<td align="char" char=".">16.3</td>
<td align="char" char=".">15.6</td>
<td align="char" char=".">37.4</td>
<td align="char" char=".">10.2</td>
<td align="char" char=".">17.5</td>
<td align="char" char=".">81.8</td>
</tr>
</tbody>
</table>
</table-wrap>
<sec id="s3-1">
<title>In-Plane Compressional Coefficients</title>
<p>The variations of the in-plane compressional coefficients <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> with different layer charge densities for the three models with different layer charge distributions are shown in <xref ref-type="fig" rid="F2">Figure&#x20;2</xref>. It is interesting that all the three in-plane compressional coefficients decrease approximately linearly with the increasing layer charge density in the three models. The reduction in the three coefficients indicates that the compressional resistance of the three models decreases with the increasing layer charge density. Specifically, the decreasing <italic>C</italic>
<sub>11</sub> and <italic>C</italic>
<sub>22</sub> represents the reduction in the compressional resistance in the <italic>x</italic>-axis and <italic>y</italic>-axis, respectively, and the declining <italic>C</italic>
<sub>12</sub> stands for the decrease of the compressional resistance in the <italic>y</italic>-direction when a given positive pressure is applied to the <italic>x</italic>-axis.</p>
<fig id="F2" position="float">
<label>FIGURE 2</label>
<caption>
<p>The in-line compressional elastic constants <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> as a function of layer charge density for the <bold>(A)</bold> M1 Model, <bold>(B)</bold> M2 Model and <bold>(C)</bold> M3 Model.</p>
</caption>
<graphic xlink:href="feart-10-854816-g002.tif"/>
</fig>
<p>Since <italic>C</italic>
<sub>11</sub> and <italic>C</italic>
<sub>22</sub> reflect the strength of the intermolecular interactions of the MMT molecules in the <italic>x</italic>-axis and <italic>y</italic>-axis, respectively, and <italic>C</italic>
<sub>12</sub> reflects the strength of the intermolecular interactions in the <italic>xy</italic>-plane, the decrease of <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22,</sub> and <italic>C</italic>
<sub>12</sub> can be explained by the weakening of the intermolecular interactions of the MMT in these directions. The intermolecular interaction is inversely proportional to the atomic distance (<xref ref-type="bibr" rid="B6">Cygan et&#x20;al., 2004</xref>; <xref ref-type="bibr" rid="B8">Davarcioglu, 2011</xref>), and thus the decrease of the three coefficients with the increasing layer charge density may be related to the increase in the atomic distance of the MMT. <xref ref-type="fig" rid="F3">Figure&#x20;3</xref> shows the atomic distances (distance between the replaced atom or replacement atom and the adjacent oxygen atom) before and after the substitutions, and the results clearly demonstrate that the atomic distances in the MMT layer (composed of three sheets) after the substitutions are increasing, no matter whether the tetrahedral substitutions or the octahedral substitutions are introduced into the MMT. The increase in the atomic distance in the MMT layer may lead to the weakening of the intermolecular interactions within the MMT layer in all directions.</p>
<fig id="F3" position="float">
<label>FIGURE 3</label>
<caption>
<p>The frequency of the distance between the substituted atom or replacement atom and the adjacent oxygen atom in the <bold>(A)</bold> T sheet and <bold>(B, C)</bold> O sheet of the MMT layer before and after the isomorphous substitution. The symbol &#x2a; represents the atoms after substitution. In the O sheet, the Al/Mg-O distances are classified into the Al/Mg-Ob(os) and Al/Mg-Oh(s) distances according to the type of the connected oxygen atoms (i.e.,&#x20;bridging oxygen or hydroxyl oxygen) as shown in <xref ref-type="fig" rid="F1">Figure&#x20;1</xref>.</p>
</caption>
<graphic xlink:href="feart-10-854816-g003.tif"/>
</fig>
<p>To further support the explained variation of the interaction strength, we also calculate the interaction energy (the difference between the molecules&#x2019; combined energy and all of their isolated energies) between the replaced atom or replacement atom and the adjacent oxygen atom (i.e.,&#x20;the forming atom pair) as shown in <xref ref-type="fig" rid="F4">Figure&#x20;4</xref>. It can be seen that the interaction energy between the atom pair increases after the tetrahedral substitutions or the octahedral substitutions, directly indicating that the interaction within the MMT layer is weakened (<xref ref-type="bibr" rid="B39">&#x160;poner et&#x20;al., 1999</xref>; <xref ref-type="bibr" rid="B26">Lovelock, 2017</xref>). Considering the in-plane compressional coefficients are related to the intermolecular interactions in the <italic>x</italic>- and <italic>y</italic>-axes of the MMT layer (<xref ref-type="bibr" rid="B3">Carrier et&#x20;al., 2014</xref>), the increase in the atomic distances will reduce these intermolecular interactions in these directions and hence the in-line compressional elastic coefficient <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and&#x20;<italic>C</italic>
<sub>12</sub>.</p>
<fig id="F4" position="float">
<label>FIGURE 4</label>
<caption>
<p>The frequency of the interaction energy between the replaced atom or replacement atom and the adjacent oxygen atom in the <bold>(A)</bold> T sheet and <bold>(B,C)</bold> O sheet of the MMT layer before and after the isomorphous substitution.</p>
</caption>
<graphic xlink:href="feart-10-854816-g004.tif"/>
</fig>
<p>It is worth noting that although <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> of all the models are decreasing, we find the values and the variations of <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> in the three models are different. First, it is evident that <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> in the M2 Model are larger than those in the other two models when the layer charge densities are the same. This means that <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> of the MMT with the layer charges distributed in the O sheet are greater than those of the MMT with the layer charges distributed in the two T sheets and in both the O sheet and the T sheets. This result can be closely related to the structure of the MMT. As shown in <xref ref-type="fig" rid="F1">Figure&#x20;1D</xref>, the MMT consists of a sandwich of one O sheet between two T sheets, called a TOT structure. Since the O sheet is constrained by the two T sheets and there are interactions among the sheets, the increase in the atomic distance and in the interaction energy between the atomic pairs in the O sheet after the octahedral substitution is weakened. As a result, the intermolecular interactions in the <italic>xy</italic>-plane are less reduced, leading to a greater <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> in the M2&#x20;model.</p>
<p>In addition to the difference in the values of the three in-plane compressional coefficients, it is also interesting to note that the changing rates of the compressional coefficient with layer charge densities in the three models are different. <xref ref-type="table" rid="T2">Table&#x20;2</xref> tabulates the slopes of <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> after linear fitting for the three models. By comparing the slopes of the same parameter in the three models, we find that the M1 model has the largest slopes of <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub>, followed by the M3 model and the M2 model. This result implies that the layer charge density has a greater effect on <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> of MMT with the layer charges distributed in the T sheet. The difference in the slopes of the in-plane compressional coefficients in the three models can again be explained through the structure of the MMT, where the TOT architecture will confine the expansion of the O sheet, and hence the octahedral substitution has less impaction on the elastic properties, resulting in a gentler slope of the in-plane compressional coefficients with varying layer charge density.</p>
<table-wrap id="T2" position="float">
<label>TABLE 2</label>
<caption>
<p>The linear-fit slopes of the compressional elastic constants <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub>, and <italic>C</italic>
<sub>12</sub> with the varying layer charge density for the three models.</p>
</caption>
<table>
<thead valign="top">
<tr>
<th align="left">Model</th>
<th align="center">M1</th>
<th align="center">M2</th>
<th align="center">M3</th>
</tr>
</thead>
<tbody valign="top">
<tr>
<td align="left">Slope of <italic>C</italic>
<sub>11</sub>
</td>
<td align="char" char=".">&#x2212;45.08</td>
<td align="char" char=".">&#x2212;26.59</td>
<td align="char" char=".">&#x2212;35.10</td>
</tr>
<tr>
<td align="left">Slope of <italic>C</italic>
<sub>22</sub>
</td>
<td align="char" char=".">&#x2212;39.45</td>
<td align="char" char=".">&#x2212;19.82</td>
<td align="char" char=".">&#x2212;35.81</td>
</tr>
<tr>
<td align="left">Slope of <italic>C</italic>
<sub>12</sub>
</td>
<td align="char" char=".">&#x2212;34.61</td>
<td align="char" char=".">&#x2212;25.94</td>
<td align="char" char=".">&#x2212;33.58</td>
</tr>
</tbody>
</table>
</table-wrap>
</sec>
<sec id="s3-2">
<title>Out-of-Plane Compressional Coefficients</title>
<p>
<xref ref-type="fig" rid="F5">Figure&#x20;5</xref> shows the variations of the out-of-plane compressional coefficients <italic>C</italic>
<sub>33</sub>, <italic>C</italic>
<sub>13</sub>, and <italic>C</italic>
<sub>23</sub> with the increase of layer charge density for the three models with different layer charge distributions. Unlike the in-plane compressional coefficients that show consistent downward trends in the three models, the out-of-plane compressional coefficients show very different variations with layer charge density in the three models. Therefore, to more conveniently understand the influences of the layer charge distribution on the out-of-plane compressional coefficients, we choose to analyze the same elastic coefficient in the different models.</p>
<fig id="F5" position="float">
<label>FIGURE 5</label>
<caption>
<p>The out-of-plane compressional elastic constants <italic>C</italic>
<sub>33</sub>, <italic>C</italic>
<sub>13</sub>, and <italic>C</italic>
<sub>23</sub> as a function of layer charge density for the <bold>(A)</bold> M1 Model, <bold>(B)</bold> M2 Model and <bold>(C)</bold> M3 Model.</p>
</caption>
<graphic xlink:href="feart-10-854816-g005.tif"/>
</fig>
<p>We first compare the variations of <italic>C</italic>
<sub>33</sub> with layer charge density in the three models that represents the compressional resistance of the MMT in the <italic>z</italic>-axis. As shown in <xref ref-type="fig" rid="F5">Figure&#x20;5A</xref>, <italic>C</italic>
<sub>33</sub> of the M1 Model increases slightly and then decreases linearly with the increase of layer charge density. The initial increasing and then decreasing <italic>C</italic>
<sub>33</sub> indicates that the increasing layer charge density first increases and then reduces the compressional resistance of the M1 Model in the <italic>z</italic>-axis. In a different manner, <italic>C</italic>
<sub>33</sub> of the M2 Model consistently increases with increasing layer charge density, suggesting that the compressional resistance of the M2 Model in the <italic>z</italic>-axis is increasing with the increasing layer charge density. For the M3 Model, <italic>C</italic>
<sub>33</sub> doesn&#x2019;t vary much as the layer charge density increases, implying that the layer charge density is not affecting significantly the compressional resistance of the M3 Model in the <italic>z</italic>-axis.</p>
<p>Because <italic>C</italic>
<sub>33</sub> reflects the strength of the intermolecular interactions of the MMT in the <italic>z</italic>-axis, the different trends of <italic>C</italic>
<sub>33</sub> with the increase of layer charge density in the different models can be explained by the difference in the <italic>z</italic>-axis intermolecular interaction strength of the MMT caused by the layer charge distributions. The intermolecular interactions of the MMT in the <italic>z</italic>-axis involve the intermolecular interactions in the <italic>z</italic>-axis both within the MMT layer (each layer is composed of three sheets) and between the neighboring MMT layers because the MMT contains the MMT layers and the interlayers in the <italic>z</italic>-axis as shown in <xref ref-type="fig" rid="F1">Figure&#x20;1D</xref>. We have employed atomic distance inversely to represent the strength of the intermolecular interactions in the previous section, however, the atomic distance can only reflect the intermolecular strength of the MMT layer in the <italic>x</italic>- and <italic>y</italic>-axes, but will not fully represent the intermolecular strength in the <italic>z</italic>-axis. This is because the <italic>z</italic>-axis intermolecular interaction includes not only the <italic>z</italic>-axis intermolecular interaction within each MMT layer but also that between the MMT layers (i.e.,&#x20;the interlayers). To characterize the strength of the intermolecular interactions of the MMT in the <italic>z</italic>-axis, we will use the interaction energy of the MMT layer and the interlayer. However, the interaction energy will not directly quantify the interaction strength in a particular direction because it contains the information of the intermolecular interactions in all directions. Therefore, we combine the interaction energy with the calculated atomic distance (as shown in <xref ref-type="fig" rid="F3">Figure&#x20;3</xref>) that reflects the intermolecular interactions in the <italic>x</italic>- and <italic>y</italic>-axes for the better characterization of the intermolecular strength in the <italic>z</italic>-axis.</p>
<p>
<xref ref-type="fig" rid="F6">Figure&#x20;6</xref> shows the simulated interaction energy in the MMT layer and the interlayer as a function of layer charge density for the three models. In the three models, the interaction energy in the interlayer all decreases with the increasing layer charge density, indicating enhanced interlayer interactions (<xref ref-type="bibr" rid="B37">Shiu and Tsai, 2014</xref>; <xref ref-type="bibr" rid="B43">Wang et&#x20;al., 2018</xref>). The decreasing interlayer interaction energy with increasing layer charge density can be explained by the fact that with increasing layer charge density there are more compensating Na cations in the interlayer that bind stronger the MMT layers (<xref ref-type="bibr" rid="B49">Zhong et&#x20;al., 2021</xref>), resulting in lower interlayer interaction energy. On the contrary, the interaction energy in the MMT layer varies differently with the increase of layer charge density in the three models. The layer interaction energy of the MMT increases remarkably with the increasing layer charge density in the M1 model, and the increase becomes less significant in the M3 model, indicating the strength of the intermolecular interactions within the MMT layer are reducing significantly and gently in the M1 Model and M3 Model, respectively. In a different way, the interaction energy of the MMT layer reduces with the increasing layer charge density in the M2 Model, suggesting an increasing interaction strength of the intermolecular within the MMT layer with the increasing layer charge density.</p>
<fig id="F6" position="float">
<label>FIGURE 6</label>
<caption>
<p>The interaction energy of each MMT layer and interlayer as a function of layer charge density for the <bold>(A)</bold> M1 Model, <bold>(B)</bold> M2 Model and <bold>(C)</bold> M3 Model.</p>
</caption>
<graphic xlink:href="feart-10-854816-g006.tif"/>
</fig>
<p>The decreasing interaction strength of the MMT layer (the increasing layer interaction energy) in the M1 Model can be understandable, because the isomorphous substitutions in the T sheet will increase the atomic distance (as shown in <xref ref-type="fig" rid="F3">Figure&#x20;3A</xref>) and hence reduce the interaction strength, and therefore more isomorphous substitutions with greater layer charge density will result in the more significant reduction in the interaction strength. However, the increasing atomic distance due to the isomorphous substitutions cannot explain the obtained increasing interaction strength (decreasing layer interaction energy) in the M2 Model. Although the isomorphous substitutions in the O sheet (M2 Model) will increase the atomic distance, the increase occurs only in the O sheet, and with the increasing atomic distance in the O sheet, the distance of the atoms between the O and T sheets is reduced. As a result, the interaction strength between the O sheet and the T sheets gets enhanced, leading to an increasing layer interaction strength. Accordingly, the obtained increasing layer interaction strength with layer charge density in the M2 Model implies that the increasing interaction strength between the O sheet and the T sheets overwhelms the decreasing interaction strength in the O sheet. Similarly, the gently decreasing interaction strength of the MMT layer with layer charge density in the M3 Model indicates that the effects of the increasing interaction strength between the O sheet and the T sheets are less significant than the decreasing interaction strength in the O and T sheets.</p>
<p>After analyzing the impact of the layer charge density on the two interactions and on the interactions in the <italic>x</italic>- and <italic>y</italic>-axes (which can be represented by the in-plane compressional coefficients presented above) in the three models, the variations of the calculated <italic>C</italic>
<sub>33</sub> in the three models that reflect the interaction strength in the <italic>z</italic>-axis can be more understandable. For the M2 Model, the interaction strength in the <italic>x</italic>- and <italic>y</italic>-axes decreases with increasing layer charge density, however, the total interaction strength (i.e.,&#x20;the interaction strength in both the MMT layer and the interlayer) increases with layer charge density, and accordingly the <italic>z</italic>-axis interaction strength (i.e.,&#x20;<italic>C</italic>
<sub>33</sub>) must increase with the increasing layer charge density. Unlike <italic>C</italic>
<sub>33</sub> in the M2 Models, <italic>C</italic>
<sub>33</sub> in the M1 Model and M3 Model can not be directly explained by the total interaction strength and the interaction strength in the <italic>x</italic>- and <italic>y</italic>-axes, but can reflect the competition between the interaction strength of the layer and interlayer in the <italic>z</italic>-axis (i.e.,&#x20;the difference between the layer and interlayer interaction strength and their contribution from the <italic>x</italic>- and <italic>y</italic>-axes, respectively).</p>
<p>For the M1 Model, because the total interlayer interaction strength increases while the interaction strength in the <italic>x</italic>- and <italic>y</italic>-axes decreases with increasing layer charge density, the <italic>z</italic>-axis interlayer interaction strength must increase with the increasing layer charge density. On the other hand, the variation of the layer interaction strength in the <italic>z</italic>-axis with the increasing layer charge density cannot be determined because both the layer interaction strength and the interaction strength in the <italic>x</italic>- and <italic>y</italic>-axes decrease with layer charge density. When the layer charge density is low, it can be difficult to deduce the variation of the layer interaction strength in the <italic>z</italic>-axis from the increasing <italic>C</italic>
<sub>33</sub>, because the interlayer interaction strength in the <italic>z</italic>-axis also increases with increasing layer charge density. However, when the layer charge density increases from 0.625 e/uc, the decreasing <italic>C</italic>
<sub>33</sub> indicates the layer interaction strength in the <italic>z</italic>-axis also decreases and the decreasing of the layer interaction strength in the <italic>z</italic>-axis is playing a more significant role than the increasing interlayer interaction strength in the <italic>z</italic>-axis.</p>
<p>Since the trends of the interlayer interaction strength and the layer interaction strength in the M3 Model are similar to those in the M1 Model, it is reasonable that the <italic>z</italic>-axis interlayer interaction strength increases (because the interaction strength in the <italic>x</italic>- and <italic>y</italic>-axes decreases) and the layer interaction strength in the <italic>z</italic>-axis can not be determined (because both the layer interaction strength and the interaction strength in the <italic>x</italic>- and <italic>y</italic>-axes decrease) in the M3 Model. However, according to the fact that the <italic>C</italic>
<sub>33</sub> of the M3 Model doesn&#x2019;t vary much with the increase of the layer charge density and the <italic>z</italic>-axis interlayer interaction strength increases, we can infer that the layer interaction strength in the <italic>z</italic>-axis decreases and the decreasing interlayer interaction in the <italic>z</italic>-axis balances with the increasing layer interaction in the <italic>z</italic>-axis.</p>
<p>Having analyzed the variations of <italic>C</italic>
<sub>33</sub> with layer charge density and provided a plausible explanation through the interaction energy, we proceed to present and interpret the variations of <italic>C</italic>
<sub>13</sub> and <italic>C</italic>
<sub>23</sub> with layer charge density in the three models with different layer charge distributions. Interestingly, although the values are much smaller, <italic>C</italic>
<sub>13</sub> and <italic>C</italic>
<sub>23</sub> show very similar trends with <italic>C</italic>
<sub>33</sub> in each model, and this indicates that the interaction strength in the <italic>z</italic>-axis that determines <italic>C</italic>
<sub>33</sub>, may also be the main factor influencing <italic>C</italic>
<sub>13</sub> and <italic>C</italic>
<sub>23</sub>. Therefore, it can be reasonable that the difference in variations of the out-of-plane compressional coefficients with layer charge density in the three models with different layer charge distributions is controlled mainly by the layer interaction strength in the <italic>z</italic>-axis.</p>
</sec>
<sec id="s3-3">
<title>Shear Coefficients</title>
<p>
<xref ref-type="fig" rid="F7">Figure&#x20;7</xref> shows the variations of the in-plane shear coefficient <italic>C</italic>
<sub>66</sub> and the out-of-plane shear coefficients <italic>C</italic>
<sub>44</sub> and <italic>C</italic>
<sub>55</sub> with the increasing layer charge density. We can see that <italic>C</italic>
<sub>66</sub> of the three models keeps almost constant at around 80&#xa0;GPa as the layer charge density increases, indicating the shear deformation resistance in the <italic>xy</italic>-plane is independent of the density and distribution of the layer charges. Unlike the flat in-plane shear coefficient <italic>C</italic>
<sub>66</sub>, the out-of-plane shear parameters <italic>C</italic>
<sub>44</sub> and <italic>C</italic>
<sub>55</sub> are fluctuant with the increasing layer charge density in all the three models, and their values in each model are approximately the same. This suggests the shear deformation resistance in the <italic>yz</italic>-plane and <italic>xz</italic>-plane is not significantly affected by the layer charge density and the layer charge distribution. Since the shear coefficients are mainly reflecting the torsion interaction of the bonding atoms at the molecular level (<xref ref-type="bibr" rid="B40">Sridharan, 2014</xref>; <xref ref-type="bibr" rid="B45">Yang and Xu, 2021</xref>), the unchanging shear coefficients indicate that the torsion interaction of the bonding atoms is independent of the varying layer charge density and layer charge distribution.</p>
<fig id="F7" position="float">
<label>FIGURE 7</label>
<caption>
<p>The shear elastic constants <italic>C</italic>
<sub>44</sub>, <italic>C</italic>
<sub>55</sub>, and <italic>C</italic>
<sub>66</sub> as a function of layer charge density for the <bold>(A)</bold> M1 Model, <bold>(B)</bold> M2 Model, and <bold>(C)</bold> M3 Model.</p>
</caption>
<graphic xlink:href="feart-10-854816-g007.tif"/>
</fig>
<p>Although the layer charge density and layer charge distribution are not impacting greatly the shear coefficients, it is found that the out-of-plane shear elastic coefficients <italic>C</italic>
<sub>44</sub> and <italic>C</italic>
<sub>55</sub> are considerably smaller than the in-plane shear elastic constant <italic>C</italic>
<sub>66</sub>. This result indicates that the shear deformation is more likely to occur in the <italic>yz</italic>-plane and <italic>xz</italic>-plane than in the <italic>xy</italic>-plane of the MMTs. This may be related to the interlayer structure of the MMTs as shown in <xref ref-type="fig" rid="F1">Figure&#x20;1D</xref>. Because the interlayer structure is perpendicular to the <italic>z</italic>-axis and the interlayer interactions are much weaker than the intermolecular interactions within the MMT layer (<xref ref-type="bibr" rid="B47">Zhang et&#x20;al., 2018</xref>; <xref ref-type="bibr" rid="B48">Zhao et&#x20;al., 2021</xref>), the <italic>yz</italic>- and <italic>xz</italic>-planes are easier to form slip deformation than the <italic>xy</italic>-plane when a shear force is applied, resulting in the smaller shear coefficients <italic>C</italic>
<sub>44</sub> and <italic>C</italic>
<sub>55</sub> than&#x20;<italic>C</italic>
<sub>66</sub>.</p>
</sec>
</sec>
<sec sec-type="conclusion" id="s4">
<title>Conclusion</title>
<p>We have studied the elastic coefficients of MMTs with different charge densities and different charge distributions under stratigraphic conditions using molecular dynamic simulations. The following conclusions can be drawn from the results and analyses presented in the context.<list list-type="simple">
<list-item>
<p>1) The in-plane compressional coefficients <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub> and <italic>C</italic>
<sub>12</sub> decrease with increasing layer charge density in the MMTs with different layer charge distributions. The <italic>C</italic>
<sub>11</sub>, <italic>C</italic>
<sub>22</sub> and <italic>C</italic>
<sub>12</sub> of the MMTs with the layer charges distributed in the octahedral (O) sheet are respectively greater than those distributed in both the octahedral (O) sheet and the tetrahedral (T) sheets, which in turn are greater than those distributed in the tetrahedral (T) sheets.</p>
</list-item>
<list-item>
<p>2) The out-of-plane compressional coefficient <italic>C</italic>
<sub>33</sub> shows different trends with increasing layer charge density in the MMTs with different layer charge distributions. <italic>C</italic>
<sub>33</sub> decreases overall with the increasing layer charge density when the layer charges are on the two tetrahedral (T) sheets, whereas it shows an increasing trend with layer charge density when the layer charges are distributed on the octahedral (O) sheet. For the MMTs with the layer charges distributed on both the octahedral (O) sheet and the tetrahedral (T) sheets, the increasing layer charge density shows a weak impact on <italic>C</italic>
<sub>33</sub>. The variations of <italic>C</italic>
<sub>13</sub> and <italic>C</italic>
<sub>23</sub> with the layer charge density in the MMTs with different layer charge distributions are similar to that of&#x20;<italic>C</italic>
<sub>33</sub>.</p>
</list-item>
<list-item>
<p>3) All the shear coefficients <italic>C</italic>
<sub>44</sub>, <italic>C</italic>
<sub>55</sub>, and <italic>C</italic>
<sub>66</sub> of MMT show no strong correlation with the layer charge density and layer charge distribution, and <italic>C</italic>
<sub>66</sub> is considerably greater than <italic>C</italic>
<sub>44</sub> and&#x20;<italic>C</italic>
<sub>55</sub>.</p>
</list-item>
<list-item>
<p>4) The variations of the anisotropic compressional elastic coefficients with different layer charge densities and layer charge distributions are found to be a result of the impact of the density and distribution of layer charges on the molecular interactions within the MMT&#x20;layer.</p>
</list-item>
</list>
</p>
</sec>
</body>
<back>
<sec id="s5">
<title>Data Availability Statement</title>
<p>The raw data supporting the conclusion of this article will be made available by the authors, without undue reservation.</p>
</sec>
<sec id="s6">
<title>Author Contributions</title>
<p>XW and TH conceive this research. XW writes the manuscript and prepares the figures. TH reviews and supervises the manuscript. The co-author L-YF is involved in the discussion of the manuscript. All authors finally approve the manuscript and thus agree to be accountable for this&#x20;work.</p>
</sec>
<sec id="s7">
<title>Funding</title>
<p>The research is supported by the National Natural Science Foundation of China (41821002, 42174136, and 41874151), the Shandong Provincial Natural Science Foundation, China (ZR2021JQ14), and the Postgraduate Innovation Project&#x20;of&#x20;China University of Petroleum (East China) (YCX2021009).</p>
</sec>
<sec sec-type="COI-statement" id="s8">
<title>Conflict of Interest</title>
<p>The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.</p>
</sec>
<sec sec-type="disclaimer" id="s9">
<title>Publisher&#x2019;s Note</title>
<p>All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.</p>
</sec>
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