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            <name>Title</name>
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                <text>Faculty Publications</text>
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    <name>Article</name>
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          <name>Creator</name>
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            <elementText elementTextId="221898">
              <text>Kruthik, P.S.; Idris, Ruwaidiah; Siddheshwar, P.G.</text>
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          <name>Title</name>
          <description>A name given to the resource</description>
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            <elementText elementTextId="221899">
              <text>STUDY OF THE LINEAR AND NONLINEAR REGIMES OF NATURAL CONVECTION WITH WEAK OR DOMINATING INTERNAL HEAT GENERATION FOR RIGID-FREE BOUNDARIES</text>
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          <name>Date</name>
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            <elementText elementTextId="221900">
              <text>01-01-2025</text>
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          <name>Source</name>
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            <elementText elementTextId="221901">
              <text>Journal of Porous Media;Volume;28;Issue;9;pp.21-39</text>
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          <name>Identifier</name>
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              <text>&lt;a href="https://doi.org/10.1615/JPorMedia.2025056500" target="_blank" rel="noreferrer noopener"&gt;https://doi.org/10.1615/JPorMedia.2025056500&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;&lt;a href="https://www.scopus.com/pages/publications/105004989484?origin=resultslist" target="_blank" rel="noreferrer noopener"&gt;https://www.scopus.com/pages/publications/105004989484?origin=resultslist&lt;/a&gt;</text>
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              <text>Kruthik P.S., Special Interest Group for Modelling and Data Analytics (SIGMDA), Faculty of Computer Science and Mathematics, Universiti Malaysia Terengganu, Kuala Nerus, Terengganu, 21030, Malaysia; Idris R., Special Interest Group for Modelling and Data Analytics (SIGMDA), Faculty of Computer Science and Mathematics, Universiti Malaysia Terengganu, Kuala Nerus, Terengganu, 21030, Malaysia; Siddheshwar P.G., Centre for Mathematical Needs, Department of Mathematics, CHRIST University, Bengaluru, 560029, India</text>
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              <text>The paper presents the linear and non-linear regimes of natural convection in the presence of uniform internal heat generation for rigid-free boundaries. A linear stability analysis followed by nonlinear stability analysis is carried out for using a novel procedure. The eigenvalue of the two problems are different. The first one has Rayleigh number based on internal heat generation as the eigenvalue while the second, which is of the classical Bard type, has a buoyancyRayleigh number. The critical Rayleigh number in both problems is initially determined using the single-term Galerkin method, followed by a refinement of the value by the Maclaurin series method. The findings indicate that the system becomes stable with increasing values of the porous parameter and the Brinkman number. The percentage relative error in the eigenvalue obtained by the single-term Galerkin method relative to that obtained by the Maclaurin series method is presented. In the second natural convection problem, we have two Rayleigh numbers, viz., the weak internal Rayleigh number, RI, and the external Rayleigh number, Ra. The effect of RI on Rac is to reduce it in the case of a heat source and increase it in the case a of heat sink. Additionally, conditions facilitating the transition from Brinkman Bard convection to DarcyBard convection are presented. The GinzburgLandau equation is obtained for both the problems and the scaled Lorenz model is derived in the case of second problem. The solution from the GinzburgLandau equation is used to plot for the amplitude and results are illustrated.  2025 by Begell House,.</text>
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          <name>Subject</name>
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              <text>BrinkmanBard convection; DarcyBard convection; internal heat generation; linear stability analysis; Maclaurin series; natural convection; nonlinear stability analysis; RayleighBard convection; single-term Galerkin method</text>
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          <name>Publisher</name>
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              <text>Begell House Inc.</text>
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              <text>ISSN: 1091028X; CODEN: JPMEF</text>
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              <text>English</text>
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              <text>Article</text>
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              <text>Restricted Access; Hardcopy may be available in the library</text>
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          <name>Format</name>
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              <text>online</text>
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