Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/23197
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dc.contributor.authorMahmud, M.N.-
dc.date.accessioned2019-11-27T09:04:39Z-
dc.date.available2019-11-27T09:04:39Z-
dc.date.issued2018-
dc.identifier.citationMahmud, M. N. (2018). Stability enhancement of high Prandtl number chaotic convection in an anisotropic porous layer with feedback control. Journal of Physics: Conference Series, 1011(1).en_US
dc.identifier.issn1742-6596-
dc.identifier.urihttps://doi.org/10.1088/1742-6596/1011/1/012081-
dc.identifier.urihttps://iopscience.iop.org/article/10.1088/1742-6596/1011/1/012081-
dc.identifier.urihttps://www.scopus.com/record/display.uri?eid=2-s2.0-85047725080&doi=10.1088%2f1742-6596%2f1011%2f1%2f012081&origin=inward&txGid=49dd2f4750a4f17ce10def678c851e94-
dc.identifier.urihttp://ir.unikl.edu.my/jspui/handle/123456789/23197-
dc.descriptionThis is an open access article distributed under the terms of the Creative Commons CC-BY license. This article index by Scopusen_US
dc.description.abstractThe chaotic dynamical behaviour of thermal convection in an anisotropic porous layer subject to gravity, heated from below and cooled from above, is studied based on theory of dynamical system in the presence of feedback control. The extended Darcy model, which includes the time derivative has been employed in the momentum equation to derive a low dimensional Lorenz-like equation by using Galerkin-truncated approximation. The classical fourth-order Runge-Kutta method is used to obtain the numerical solution in order to exemplify the dynamics of the nonlinear autonomous system. The results show that stability enhancement of chaotic convection is feasible via feedback control.en_US
dc.language.isoenen_US
dc.publisherIOP Publishing Ltden_US
dc.titleStability enhancement of high Prandtl number chaotic convection in an anisotropic porous layer with feedback controlen_US
dc.typeArticleen_US
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