<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article">
 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">
    jmmce
   </journal-id>
   <journal-title-group>
    <journal-title>
     Journal of Minerals and Materials Characterization and Engineering
    </journal-title>
   </journal-title-group>
   <issn pub-type="epub">
    2327-4077
   </issn>
   <issn publication-format="print">
    2327-4085
   </issn>
   <publisher>
    <publisher-name>
     Scientific Research Publishing
    </publisher-name>
   </publisher>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="doi">
    10.4236/jmmce.2024.125015
   </article-id>
   <article-id pub-id-type="publisher-id">
    jmmce-135514
   </article-id>
   <article-categories>
    <subj-group subj-group-type="heading">
     <subject>
      Articles
     </subject>
    </subj-group>
    <subj-group subj-group-type="Discipline-v2">
     <subject>
      Chemistry 
     </subject>
     <subject>
       Materials Science, Engineering
     </subject>
    </subj-group>
   </article-categories>
   <title-group>
    The Effect of External Pressure on Mechanical Properties of Aquamarine Gemstone Using First Principles Studies
   </title-group>
   <contrib-group>
    <contrib contrib-type="author" xlink:type="simple">
     <name name-style="western">
      <surname>
       Evarist
      </surname>
      <given-names>
       Kahuluda
      </given-names>
     </name>
    </contrib>
    <contrib contrib-type="author" xlink:type="simple">
     <name name-style="western">
      <surname>
       Pulapa Ventkata Kanaka
      </surname>
      <given-names>
       Rao
      </given-names>
     </name>
    </contrib>
    <contrib contrib-type="author" xlink:type="simple">
     <name name-style="western">
      <surname>
       Stanley
      </surname>
      <given-names>
       Mwanga
      </given-names>
     </name>
    </contrib>
   </contrib-group> 
   <aff id="affnull">
    <addr-line>
     aDepartment of Physics, College of Natural and Mathematical Sciences, University of Dodoma, Dodoma, United Republic of Tanzania
    </addr-line> 
   </aff> 
   <pub-date pub-type="epub">
    <day>
     26
    </day> 
    <month>
     08
    </month>
    <year>
     2024
    </year>
   </pub-date> 
   <volume>
    12
   </volume> 
   <issue>
    05
   </issue>
   <fpage>
    237
   </fpage>
   <lpage>
    246
   </lpage>
   <history>
    <date date-type="received">
     <day>
      17,
     </day>
     <month>
      May
     </month>
     <year>
      2024
     </year>
    </date>
    <date date-type="published">
     <day>
      23,
     </day>
     <month>
      May
     </month>
     <year>
      2024
     </year> 
    </date> 
    <date date-type="accepted">
     <day>
      23,
     </day>
     <month>
      August
     </month>
     <year>
      2024
     </year> 
    </date>
   </history>
   <permissions>
    <copyright-statement>
     © Copyright 2014 by authors and Scientific Research Publishing Inc. 
    </copyright-statement>
    <copyright-year>
     2014
    </copyright-year>
    <license>
     <license-p>
      This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/
     </license-p>
    </license>
   </permissions>
   <abstract>
    Aquamarine gemstones are popular jewelry in the gemstone trade and are currently one of the important products in the world market because of their economic value. Aquamarine is a Beryllium Aluminium Silicate with the chemical formula Be
    <sub>3</sub>Al
    <sub>2</sub>Si
    <sub>6</sub>O
    <sub>18</sub> and crystallizes in the hexagonal system with space group P6/mcc (192), and Tanzania has wide deposits of aquamarine gemstones. The quality of gemstone depends on its characteristic properties, including electronic, optical, and mechanical properties. In the present study, the effect of external pressure on mechanical properties including independent elastic constants and other related parameters such as Bulk modulus, Shear modulus, Young modulus, Poisson’s ratio, and Compressibility were studied. Density Function Theory in the forcite module of the material studies software on the external pressure within the range of 0 - 200 GPa on the optimized structure at electrostatic, Van der Waals and Ewald terms were used in this study. The results reveal that the independent elastic constants are mechanically unstable at 50 - 120 Gpa and are stable at 0 - 40 GPa and above 120 GPa, with the average bulk modulus, shear modulus, young modulus, Poisson’s ratio of 2319.9447, 652.3058, 1789.2236, and 0.26 respectively with the compressibility of 0.059921/TPa, this indicates that aquamarine gemstones are stable against strain and strongly against shear stress but opposing shear deformation. These values are within other crystalline materials found in the literature. This provides technological backing for the comprehensive valuation of mechanical properties, quality, and stability of gemstones available in Tanzania. 
   </abstract>
   <kwd-group> 
    <kwd>
     Aquamarine Gemstones
    </kwd> 
    <kwd>
      Mechanical Properties
    </kwd> 
    <kwd>
      External Pressure
    </kwd> 
    <kwd>
      Biovia Material Studio
    </kwd> 
    <kwd>
      Forcite Module
    </kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <sec id="s1">
   <title>1. Introduction</title>
   <p>Information shows that aquamarine gemstones are currently one of the Tanzania gemstones products it her market because of their economic value <xref ref-type="bibr" rid="scirp.135514-1">
     [1]
    </xref>. This gemstone is a Beryllium Aluminium Silicate with the chemical formula Be<sub>3</sub>Al<sub>2</sub>Si<sub>6</sub>O<sub>18</sub> and exhibits a hexagonal structure with P6/mcc (192) space group <xref ref-type="bibr" rid="scirp.135514-2">
     [2]
    </xref> <xref ref-type="bibr" rid="scirp.135514-3">
     [3]
    </xref>. Most aquamarine gemstone is found in the Namtumbo district, Ruvuma region <xref ref-type="bibr" rid="scirp.135514-1">
     [1]
    </xref>.</p>
   <p>Researchers have studied various properties of the gemstone experimentally and theoretically and observed that its colors vary from light blue to greenish blue with other possible variants as shown in <xref ref-type="fig" rid="fig1">
     Figure 1
    </xref> and <xref ref-type="fig" rid="fig2">
     Figure 2
    </xref> <xref ref-type="bibr" rid="scirp.135514-4">
     [4]
    </xref>. Further, the study revealed that gemstone hardness values vary from 7.5 ˗ 8.0, specific gravity between 2.67 - 2.71, and refractive index between 1.577 - 1.583 <xref ref-type="bibr" rid="scirp.135514-5">
     [5]
    </xref>. However, many properties such as mechanical, optical, and electronic properties still need to be explored because the quality of a gemstone depends widely on the nature of the mineral and its origin and external pressure due to the height from sea level <xref ref-type="bibr" rid="scirp.135514-6">
     [6]
    </xref> <xref ref-type="bibr" rid="scirp.135514-7">
     [7]
    </xref>.</p>
   <fig id="fig1" position="float">
    <label>Figure 1</label>
    <caption>
     <title>Figure 1. Beryl varieties <xref ref-type="bibr" rid="scirp.135514-4">
       [4]
      </xref>.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/2711088-rId12.jpeg?20240826033248" />
   </fig>
   <fig id="fig2" position="float">
    <label>Figure 2</label>
    <caption>
     <title>Figure 2. Aquamarine raw stone <xref ref-type="bibr" rid="scirp.135514-4">
       [4]
      </xref>.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/2711088-rId13.jpeg?20240826033248" />
   </fig>
   <p>Understanding elastic constants and elastic moduli is crucial to knowing the mechanical characteristics of materials <xref ref-type="bibr" rid="scirp.135514-8">
     [8]
    </xref>. To obtain important information on the stability unit cell structure by calculating the elastic constant and the elastic modulus such as bulk modulus B, shear modulus G, Young’s modulus E, and Poisson’s ration are important to be known to establish the stability of the crystal <xref ref-type="bibr" rid="scirp.135514-9">
     [9]
    </xref>. Each material has certain respect of strengths and weaknesses in certain respect <xref ref-type="bibr" rid="scirp.135514-10">
     [10]
    </xref>.</p>
   <p>Density Functional Theory (DFT) is the most widely used ab initio quantum computational framework for theoretically understanding the material properties at the atomistic level <xref ref-type="bibr" rid="scirp.135514-11">
     [11]
    </xref>. DFT calculations utilized the total energy and plane-wave methodology to solve the Kohn-Sham equation <xref ref-type="bibr" rid="scirp.135514-9">
     [9]
    </xref>, and investigate mechanical properties of the materials <xref ref-type="bibr" rid="scirp.135514-12">
     [12]
    </xref>. The mechanical properties of the crystal’s stability are due to its capacity to withstand external stress and can be studied by elastic properties <xref ref-type="bibr" rid="scirp.135514-13">
     [13]
    </xref>. This study intends to investigate and analyze the mechanical properties of aquamarine gemstones using the DFT method to explore their mechanical properties at the atomistic level under applied external pressure in the range of 0 - 200 GPa.</p>
  </sec><sec id="s2">
   <title>2. Methodology</title>
   <p>The crystal structure was built in the materials studio software package from the experimental values of the crystal system obtained from the crystalline database <xref ref-type="bibr" rid="scirp.135514-14">
     [14]
    </xref>. The geometry optimization of the structure was carried out using the forcite module <xref ref-type="bibr" rid="scirp.135514-15">
     [15]
    </xref>-<xref ref-type="bibr" rid="scirp.135514-17">
     [17]
    </xref>. During optimization and energy calculations, a smart algorithm with universal force fields was used, with an ultra-fine quality setting of 2 × 10<sup>−5</sup> kcal/mol of energy, 0.001 kcal/mol/Å of force, and 1 × 10<sup>−5</sup> Å of displacement <xref ref-type="bibr" rid="scirp.135514-18">
     [18]
    </xref>-<xref ref-type="bibr" rid="scirp.135514-20">
     [20]
    </xref>.</p>
   <p>After the geometry optimization of the structure, the mechanical properties were computed on the geometry optimization results obtained using the forcite module <xref ref-type="bibr" rid="scirp.135514-16">
     [16]
    </xref> <xref ref-type="bibr" rid="scirp.135514-19">
     [19]
    </xref>. During these calculations, the stiffness constants Cijs were first calculated using the elastic matric Equation (1) <xref ref-type="bibr" rid="scirp.135514-21">
     [21]
    </xref>. Independent elastic constants C<sub>11</sub>, C<sub>12</sub>, C<sub>44</sub> and C<sub>66</sub> obtained from the results of the stiffness matrix C<sub>ij</sub> independently for all external pressure were used to analyze the necessary stability criteria are presented on Equation (2) <xref ref-type="bibr" rid="scirp.135514-8">
     [8]
    </xref> <xref ref-type="bibr" rid="scirp.135514-9">
     [9]
    </xref> <xref ref-type="bibr" rid="scirp.135514-22">
     [22]
    </xref> <xref ref-type="bibr" rid="scirp.135514-23">
     [23]
    </xref>.</p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <msub> 
       <mi>
         C 
       </mi> 
       <mrow> 
        <mi>
          i 
        </mi> 
        <mi>
          j 
        </mi> 
       </mrow> 
      </msub> 
      <mo>
        = 
      </mo> 
      <mrow> 
       <mo>
         ( 
       </mo> 
       <mrow> 
        <mtable> 
         <mtr> 
          <mtd> 
           <mrow> 
            <msub> 
             <mi>
               C 
             </mi> 
             <mrow> 
              <mn>
                11 
              </mn> 
             </mrow> 
            </msub> 
           </mrow> 
          </mtd> 
          <mtd> 
           <mrow> 
            <msub> 
             <mi>
               C 
             </mi> 
             <mrow> 
              <mn>
                12 
              </mn> 
             </mrow> 
            </msub> 
           </mrow> 
          </mtd> 
          <mtd> 
           <mrow> 
            <msub> 
             <mi>
               C 
             </mi> 
             <mrow> 
              <mn>
                13 
              </mn> 
             </mrow> 
            </msub> 
           </mrow> 
          </mtd> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
         </mtr> 
         <mtr> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
          <mtd> 
           <mrow> 
            <msub> 
             <mi>
               C 
             </mi> 
             <mrow> 
              <mn>
                11 
              </mn> 
             </mrow> 
            </msub> 
           </mrow> 
          </mtd> 
          <mtd> 
           <mrow> 
            <msub> 
             <mi>
               C 
             </mi> 
             <mrow> 
              <mn>
                13 
              </mn> 
             </mrow> 
            </msub> 
           </mrow> 
          </mtd> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
         </mtr> 
         <mtr> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
          <mtd> 
           <mrow> 
            <msub> 
             <mi>
               C 
             </mi> 
             <mrow> 
              <mn>
                33 
              </mn> 
             </mrow> 
            </msub> 
           </mrow> 
          </mtd> 
         </mtr> 
         <mtr> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
          <mtd> 
           <mrow></mrow> 
          </mtd> 
          <mtd> 
           <mrow> 
            <msub> 
             <mi>
               C 
             </mi> 
             <mrow> 
              <mn>
                44 
              </mn> 
             </mrow> 
            </msub> 
           </mrow> 
          </mtd> 
         </mtr> 
        </mtable> 
       </mrow> 
       <mo>
         ) 
       </mo> 
      </mrow> 
     </mrow> 
    </math>(1)</p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <msub> 
       <mi>
         C 
       </mi> 
       <mrow> 
        <mn>
          11 
        </mn> 
       </mrow> 
      </msub> 
      <mo>
        &gt; 
      </mo> 
      <mrow> 
       <mo>
         | 
       </mo> 
       <mrow> 
        <msub> 
         <mi>
           C 
         </mi> 
         <mrow> 
          <mn>
            12 
          </mn> 
         </mrow> 
        </msub> 
       </mrow> 
       <mo>
         | 
       </mo> 
      </mrow> 
     </mrow> 
    </math></p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <mn>
        2 
      </mn> 
      <msubsup> 
       <mi>
         C 
       </mi> 
       <mrow> 
        <mn>
          13 
        </mn> 
       </mrow> 
       <mn>
         2 
       </mn> 
      </msubsup> 
      <mo>
        &lt; 
      </mo> 
      <msub> 
       <mi>
         C 
       </mi> 
       <mrow> 
        <mn>
          22 
        </mn> 
       </mrow> 
      </msub> 
      <mrow> 
       <mo>
         ( 
       </mo> 
       <mrow> 
        <msub> 
         <mi>
           C 
         </mi> 
         <mrow> 
          <mn>
            11 
          </mn> 
         </mrow> 
        </msub> 
        <mo>
          + 
        </mo> 
        <msub> 
         <mi>
           C 
         </mi> 
         <mrow> 
          <mn>
            12 
          </mn> 
         </mrow> 
        </msub> 
       </mrow> 
       <mo>
         ) 
       </mo> 
      </mrow> 
     </mrow> 
    </math>(2)</p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <msub> 
       <mi>
         C 
       </mi> 
       <mrow> 
        <mn>
          44 
        </mn> 
       </mrow> 
      </msub> 
      <mo>
        &gt; 
      </mo> 
      <mn>
        0 
      </mn> 
     </mrow> 
    </math></p>
   <p>Similarly, Bulk modulus (B) and shear modulus (G) were calculated from Reus, Voight, and Hill using Equations (3) and (4), while Youngs’ Modulus and Poisson’s ratio were calculated by using Equations (5) and (6) respectively as used elsewhere <xref ref-type="bibr" rid="scirp.135514-23">
     [23]
    </xref>-<xref ref-type="bibr" rid="scirp.135514-27">
     [27]
    </xref>.</p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <mi>
        B 
      </mi> 
      <mo>
        = 
      </mo> 
      <mfrac> 
       <mrow> 
        <mi>
          B 
        </mi> 
        <mi>
          V 
        </mi> 
        <mo>
          − 
        </mo> 
        <mi>
          B 
        </mi> 
        <mi>
          R 
        </mi> 
       </mrow> 
       <mn>
         2 
       </mn> 
      </mfrac> 
     </mrow> 
    </math>(3)</p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <mi>
        G 
      </mi> 
      <mo>
        = 
      </mo> 
      <mfrac> 
       <mrow> 
        <mi>
          G 
        </mi> 
        <mi>
          V 
        </mi> 
        <mo>
          + 
        </mo> 
        <mi>
          G 
        </mi> 
        <mi>
          R 
        </mi> 
       </mrow> 
       <mn>
         2 
       </mn> 
      </mfrac> 
     </mrow> 
    </math>(4)</p>
   <p>where: BV is the Bulk Modulus Voigt,</p>
   <p>BR is the Bulk modulus, Reus,</p>
   <p>GV is the Bulk Modulus Voigt,</p>
   <p>GR is shear modulus Reus,</p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <mi>
        Y 
      </mi> 
      <mo>
        = 
      </mo> 
      <mfrac> 
       <mrow> 
        <mn>
          9 
        </mn> 
        <mi>
          B 
        </mi> 
        <mi>
          G 
        </mi> 
       </mrow> 
       <mrow> 
        <mn>
          3 
        </mn> 
        <mi>
          B 
        </mi> 
        <mi>
          G 
        </mi> 
        <mo>
          + 
        </mo> 
        <mi>
          G 
        </mi> 
       </mrow> 
      </mfrac> 
     </mrow> 
    </math>(5)</p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <mi>
        ν 
      </mi> 
      <mo>
        = 
      </mo> 
      <mfrac> 
       <mrow> 
        <mn>
          3 
        </mn> 
        <mi>
          B 
        </mi> 
        <mo>
          − 
        </mo> 
        <mn>
          2 
        </mn> 
        <mi>
          G 
        </mi> 
       </mrow> 
       <mrow> 
        <mn>
          2 
        </mn> 
        <mrow> 
         <mo>
           ( 
         </mo> 
         <mrow> 
          <mn>
            3 
          </mn> 
          <mi>
            B 
          </mi> 
          <mo>
            + 
          </mo> 
          <mi>
            G 
          </mi> 
         </mrow> 
         <mo>
           ) 
         </mo> 
        </mrow> 
       </mrow> 
      </mfrac> 
     </mrow> 
    </math>(6)</p>
   <p>where B is Bulk Modulus,</p>
   <p>G is the hear Modulus,</p>
   <p>Y is Young Modulus,</p>
   <p>ν is the Poisson’s ratio.</p>
   <p>The ability to resist the deformation and flexibility of the gemstone is represented by the equation</p>
   <p>
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <mi>
        H 
      </mi> 
      <mo>
        = 
      </mo> 
      <mfrac> 
       <mrow> 
        <mn>
          1 
        </mn> 
        <mo>
          − 
        </mo> 
        <mn>
          2 
        </mn> 
        <mi>
          v 
        </mi> 
       </mrow> 
       <mrow> 
        <mn>
          6 
        </mn> 
        <mrow> 
         <mo>
           ( 
         </mo> 
         <mrow> 
          <mn>
            1 
          </mn> 
          <mo>
            + 
          </mo> 
          <mi>
            v 
          </mi> 
         </mrow> 
         <mo>
           ) 
         </mo> 
        </mrow> 
       </mrow> 
      </mfrac> 
      <mi>
        Y 
      </mi> 
     </mrow> 
    </math>(7)</p>
   <p>where H is the hardness or stiffness constant,</p>
   <p>ν is Poisson’s ratio,</p>
   <p>Y is the Young’s modulus.</p>
  </sec><sec id="s3">
   <title>3. Results and Discussion</title>
   <p>The optimized structure was subjected to force fields, with an ultra-fine quality setting of 2 × 10<sup>−5</sup> kcal/mol of energy, 0.001 kcal/mol/Å of force, and 1 × 10<sup>−5</sup> Å of displacement in order to investigate its stability conditions. <xref ref-type="fig" rid="fig3">
     Figure 3
    </xref> represents the optimized structure, and all the constituent atoms of the aquamarine gemstone with their respective positions.</p>
   <fig id="fig3" position="float">
    <label>Figure 3</label>
    <caption>
     <title>Figure 3. The optimized structure.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/2711088-rId32.jpeg?20240826033249" />
   </fig>
   <p>The crystal lattice parameters a = b = 9.2909 Å; c = 9.1996 Å; α = 90; β = 90; γ = 270; V = 687.726 Å<sup>3</sup> which is concurrent with the results reported in the crystalline database with Be, Al Si, and O <xref ref-type="bibr" rid="scirp.135514-2">
     [2]
    </xref>.</p>
   <p>The Born stability conditions are represented by <xref ref-type="fig" rid="fig4">
     Figure 4
    </xref>, whereby C<sub>11</sub> indicates the stiffness of the material (<xref ref-type="fig" rid="fig4(a)">
     Figure 4(a)
    </xref>), C<sub>12</sub> shear stress (<xref ref-type="fig" rid="fig4(b)">
     Figure 4(b)
    </xref>), and C<sub>44</sub> shear deformation (<xref ref-type="fig" rid="fig4(c)">
     Figure 4(c)
    </xref>). <xref ref-type="fig" rid="fig4(a)">
     Figure 4(a)
    </xref> indicates the values of stiffness oscillate with variations of external pressure, this indicates that aquamarine gemstones are stable against strain. While shear stress values oscillated in positive and negative values (<xref ref-type="fig" rid="fig4(b)">
     Figure 4(b)
    </xref>), the positive values outperformed the negative values. This also shows that the gemstone considered in this study is strongly against shear stress. However, C<sub>11</sub> is 0 GPa at the external pressure 140 GPa and C<sub>12</sub> is 4800 GPa at that particular pressure, this violate the stiffness condition one from equation 2 mean while at C<sub>11</sub> is less 1400 Gpa while C<sub>12</sub> is 2400 Gpa at the external pressure 60 GPa which also violet the Born stiffness condition. <xref ref-type="fig" rid="fig4(c)">
     Figure 4(c)
    </xref>, large portions of shear deformation to the negative side, this indicates that aquamarine gemstone to a large extent opposes the shear deformation <xref ref-type="bibr" rid="scirp.135514-25">
     [25]
    </xref>. With these parameters considered for Born stability, we can conclusively say that aquamarine gemstone is has accepted Born stability conditions except at external pressure 60 GPa and 140 GPa.</p>
   <fig-group id="fig4" position="float">
    <fig id="fig4" position="float">
     <label>Figure 4</label>
     <caption>
      <title>(a)--(b) (c)--Figure 4. (a) C11 vs external pressure, (b) C12 vs external pressure (GPa), (c) C44 vs external pressure (GPa).</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/2711088-rId33.jpeg?20240826033249" />
    </fig>
    <fig id="fig4" position="float">
     <label>Figure 4</label>
     <caption>
      <title>(a)--(b) (c)--Figure 4. (a) C11 vs external pressure, (b) C12 vs external pressure (GPa), (c) C44 vs external pressure (GPa).</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/2711088-rId34.jpeg?20240826033249" />
    </fig>
   </fig-group>
   <p>On the basis of mechanical properties such as compressibility, bulk modulus, and shear modulus with variations of external pressure were also investigated. <xref ref-type="fig" rid="figFigures 5-7">
     Figures 5-7
    </xref> present the fluctuations of compressibility, bulk modulus and shear modulus with external pressure respectively. As it can be seen from all three curves, the beryllium aluminum silicate material is mechanically stable at the external pressure 0 - 40 GPa and above 120 GPa. This stability is indicated by small oscillations, while it was unstable at the pressure of around 50 - 120 GPa.</p>
   <fig id="fig5" position="float">
    <label>Figure 5</label>
    <caption>
     <title>Figure 5. Compressibility vs external pressure.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/2711088-rId36.jpeg?20240826033249" />
   </fig>
   <fig id="fig6" position="float">
    <label>Figure 6</label>
    <caption>
     <title>Figure 6. Young’s modulus with external pressure.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/2711088-rId37.jpeg?20240826033249" />
   </fig>
   <fig id="fig7" position="float">
    <label>Figure 7</label>
    <caption>
     <title>Figure 7. Poisson’s ratio with external pressure.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/2711088-rId38.jpeg?20240826033249" />
   </fig>
   <p>Other important parameters for determining the hardness of the crystalline material are Young’s modulus, Poisson’s ratio (ν) and Young’s modulus tells how the material can withstand once subjected to elastic deformation. <xref ref-type="fig" rid="fig6">
     Figure 6
    </xref> shows the variations of the young modulus with the applied external pressure. In the range where the beryllium aluminum silicate material was found to be mechanically stable, the values of Young’s modulus varied from 0 - 9000 GPa. Thus, this material is mechanically stable within that range of external pressure. While the average value of Poisson’s ratio was 0.26 as indicated in <xref ref-type="fig" rid="fig7">
     Figure 7
    </xref>, this value is within other crystalline materials found in the literature <xref ref-type="bibr" rid="scirp.135514-8">
     [8]
    </xref> <xref ref-type="bibr" rid="scirp.135514-16">
     [16]
    </xref> <xref ref-type="bibr" rid="scirp.135514-28">
     [28]
    </xref>.</p>
   <p>The critical value of Poisson’s ratio is 0.28 <xref ref-type="bibr" rid="scirp.135514-29">
     [29]
    </xref>, where changes from brittle materials to ductile materials. The materials are regarded as ductile materials when 
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <mn>
        0.2857 
      </mn> 
      <mo>
        &lt; 
      </mo> 
      <mi>
        v 
      </mi> 
      <mo>
        ≪ 
      </mo> 
      <mn>
        0.5 
      </mn> 
     </mrow> 
    </math> and as brittle materials 
    <math display="inline" xmlns="http://www.w3.org/1998/Math/MathML"> <mrow> 
      <mn>
        0.125 
      </mn> 
      <mo>
        &lt; 
      </mo> 
      <mi>
        v 
      </mi> 
      <mo>
        &lt; 
      </mo> 
      <mn>
        0.285 
      </mn> 
     </mrow> 
    </math> <xref ref-type="bibr" rid="scirp.135514-30">
     [30]
    </xref>. Moreover, some materials have both ductile and brittle properties, and their Poisson ratio range varies from 0.26 to 0.42 <xref ref-type="bibr" rid="scirp.135514-29">
     [29]
    </xref> <xref ref-type="bibr" rid="scirp.135514-30">
     [30]
    </xref>. Therefore, it is seen from <xref ref-type="fig" rid="fig7">
     Figure 7
    </xref> that most values of the Poisson ratio with increasing external pressure dominated above the average value of 0.26. Hence, aquamarine gemstone considered in this study exhibits ductile properties.</p>
  </sec><sec id="s4">
   <title>4. Conclusion</title>
   <p>Aquamarine gemstone (beryllium aluminium silicate) with chemical formula Be<sub>3</sub>Al<sub>2</sub>Si<sub>6</sub>O<sub>18</sub> which crystallizes in the hexagonal system with P6/mcc (192) space group its effect of external pressure on mechanical properties has been studied using the First principle. Using Materials Studio simulation, the forcite module was used to calculate mechanical properties at convergence tolerance energy of 2e−005 kcal/mol, the force of 0.001 kcal/mol/A, and tress of 0.001 GPa while applying the external pressure within the range of 0 - 200 GPa on the optimized structure at electrostatic and Van der Waals terms Ewald. The results show that the independent elastic constants are mechanically stable at 0 GPa to 40 GPa, above 120 Gpa, and unstable at 60 - 120 Gpa. While the average bulk modulus, shear modulus, Young’s modulus, and Poisson’s ratio are 2319.9447, 652.3058, 1789.2236, and 0.26 respectively. The compressibility of the material was found to be 0.059921/TPa, this indicates that aquamarine gemstones are stable against strain and strongly against shear stress but opposing shear deformation. These values are within other crystalline materials found in the literature <xref ref-type="bibr" rid="scirp.135514-28">
     [28]
    </xref>-<xref ref-type="bibr" rid="scirp.135514-30">
     [30]
    </xref>. Furthermore, this provides technological backing for the comprehensive valuation of mechanical properties, quality, and stability of gemstones available in Tanzania.</p>
  </sec><sec id="s5">
   <title>Acknowledgements</title>
   <p>The Tanzania Atomic Energy Commission as a government institution has funded the research described in this publication. The sponsors’ views are not reflected in the opinions, results, conclusions, or suggestions made in this work; rather, they are the authors’ alone.</p>
  </sec>
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