A General Theory for Coupled Chemo-Electro-Thermo-Mechanical
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Fundamental Governing Equations of Motion in Consistent Continuum Mechanics
Fundamental governing equations of motion in consistent continuum mechanics Ali R. Hadjesfandiari, Gary F. Dargush Department of Mechanical and Aerospace Engineering University at Buffalo, The State University of New York, Buffalo, NY 14260 USA [email protected], [email protected] October 1, 2018 Abstract We investigate the consistency of the fundamental governing equations of motion in continuum mechanics. In the first step, we examine the governing equations for a system of particles, which can be considered as the discrete analog of the continuum. Based on Newton’s third law of action and reaction, there are two vectorial governing equations of motion for a system of particles, the force and moment equations. As is well known, these equations provide the governing equations of motion for infinitesimal elements of matter at each point, consisting of three force equations for translation, and three moment equations for rotation. We also examine the character of other first and second moment equations, which result in non-physical governing equations violating Newton’s third law of action and reaction. Finally, we derive the consistent governing equations of motion in continuum mechanics within the framework of couple stress theory. For completeness, the original couple stress theory and its evolution toward consistent couple stress theory are presented in true tensorial forms. Keywords: Governing equations of motion, Higher moment equations, Couple stress theory, Third order tensors, Newton’s third law of action and reaction 1 1. Introduction The governing equations of motion in continuum mechanics are based on the governing equations for systems of particles, in which the effect of internal forces are cancelled based on Newton’s third law of action and reaction. -
Hypersonic-Flow Governing Equations with Electromagnetic Fields
Hypersonic-FlowGoverningEquationswith ElectromagneticFields D. Giordano 1 European Space Research & Technology Center P.O. Box 299, 2200 AG Noordwijk, The Netherlands Abstract The paper deals with the formulation of a consistent set of governing equations apt to de- scribe the physical phenomenology comprising the hypersonic flow field of an ionized gas mixture and the electromagnetic field. The governing equations of the flow field and those of the electromagnetic field are revisited in sequence and differences or similarities with past treatments are pointed out and discussed. The equations governing the flow field hinge on the customary balance of masses, momenta and energies. The equations governing the electromagnetic field are introduced both directly in terms of the Maxwell equations and by recourse to the scalar and vector potentials. The theory of linear irreversible thermody- namics based on the entropy-balance equation is also revisited for the purpose of obtaining, consistently with the presence of the electromagnetic field, the phenomenological relations required to bring the governing equations into a mathematically closed form. Old problems, such as the influence of the medium compressibility on chemical-relaxation rates or the im- portance of cross effects among generalized fluxes and forces, are re-discussed; additional problems, such as the necessity to consider the tensorial nature of the transport properties because of the presence of the magnetic field, are pointed out. A non-conventional choice of first-tensorial-order generalized forces and corresponding fluxes is proposed which ap- pears to offer more simplicity and better convenience from a conceptual point of view when compared to alternative definitions customarily used in the literature. -
Numerical Models of Groundwater Flow and Transport
4 USE OF NUMERICAL MODELS TO SIMULATE GROUNDWATER FLOW AND TRANSPORT L.F. KONIKOW1 US Geological Survey, Reston, Virginia, USA 4.1 INTRODUCTION In the past, the main driving force for hydrogeologic studies has been the need to assess the water-supply potential of aquifers. During the past 20 years, however, the emphasis has shifted from water-supply problems to water-quality problems. This has driven a need to predict the movement of contaminants through the subsurface environment. One consequence of the change in emphasis has been a shift in perceived priorities for scientific research and data collection. Formerly, the focus was on developing methods to assess and measure the water-yielding properties of high-permeability aquifers. The focus is now largely on transport and dispersion processes, retardation and degradation of chemical contaminants, the effects of heterogeneity on flow paths and travel times, and the ability of low-permeability materials to contain contaminated groundwater. The past 20 years or so have also seen some major technological breakthroughs in groundwater hydrology. One technological growth area has been in the development and use of deterministic, distributed-parameter, computer simulation models for analysing flow and solute transport in groundwater systems. These developments have somewhat paralleled the development and widespread availability of faster, larger memory, more capable, yet less expensive computer systems. Another major technological growth area has been in the application of isotopic analyses to groundwater hydrology, wherein isotopic measurements are being used to help interpret and define groundwater flow paths, ages, recharge areas, leakage, and interactions with surface water (Coplen 1993). Because isotopes move through groundwater systems under the same driving forces and by the same processes as do dissolved chemicals, it is natural that the groundwater flow and solute-transport models applied to groundwater contamination problems be linked to and integrated with isotopic measurements and interpretations. -
Two-Fluid Formulation of the Cloud-Top Mixing Layer for Direct Numerical
Theor. Comput. Fluid Dyn. (2010) 24:511–536 DOI 10.1007/s00162-010-0182-x ORIGINAL ARTICLE Juan Pedro Mellado · Bjorn Stevens · Heiko Schmidt · Norbert Peters Two-fluid formulation of the cloud-top mixing layer for direct numerical simulation Received: 2 April 2009 / Accepted: 19 November 2009 / Published online: 2 February 2010 © The Author(s) 2010. This article is published with open access at Springerlink.com Abstract A mixture fraction formulation to perform direct numerical simulations of a disperse and dilute two-phase system consisting of water liquid and vapor in air in local thermodynamic equilibrium using a two- fluid model is derived and discussed. The goal is to understand the assumptions intrinsic to this simplified but commonly employed approach for the study of two-layer buoyancy reversing systems like the cloud-top mix- ing layer. Emphasis is placed on molecular transport phenomena. In particular, a formulation is proposed that recovers the actual nondiffusive liquid-phase continuum as a limiting case of differential diffusion. High-order numerical schemes suitable for direct numerical simulations in the compressible and Boussinesq limits are described, and simulations are presented to validate the incompressible approach. As expected, the Boussinesq approximation provides an accurate and efficient description of the flow on the scales (of the order of meters) that are considered. Keywords Stratocumulus clouds · Multiphase · Free convection · Free turbulent flows 1 Introduction Phase transition at the cloud boundaries often compounds the difficulty in understanding turbulent entrain- ment [15,21]. There are many different aspects of the problem, which can be considered. One of them, the role of buoyancy reversal due to the evaporative cooling that is promoted by the evaporation of the droplets under certain mixing conditions, has been long debated using theory, field and laboratory measurements, and numerical simulations [7,14,25,28,29,36,46,51,54,61]. -
Theoretical and Numerical Aspects of Modelling Geological Carbon Storage with Application to Muographic Monitoring
Theoretical and Numerical Aspects of Modelling Geological Carbon Storage with Application to Muographic Monitoring Darren L. Lincoln This thesis is submitted for partial consideration towards the degree of Doctor of Philosophy at the The Department of Civil and Structural Engineering at the University of Sheffield December 2015 No flow system is an island. A. Bejan Abstract The storage of waste carbon dioxide (CO2) from fossil fuel combustion in deep geological forma- tions is a strategy component for mitigating harmfully increasing atmospheric concentrations to within safe limits. This is to help prolong the security of fossil fuel based energy systems while cleaner and more sustainable technologies are developed. The work of this thesis is carried out as part of a multi-disciplinary project advancing knowledge on the modelling and monitoring of geological carbon storage/sequestration (GCS). The underlying principles for mathematically describing the multi-physics of multiphase multi- component behaviour in porous media are reviewed with particular interest on their application to modelling GCS. A fully coupled non-isothermal multiphase Biot-type double-porosity formu- lation is derived, where emphasis during derivation is on capturing the coupled hydro-thermo- mechanical (HTM) processes for the purposes of study. The formulated system of governing field equations is discretised in space by considering the standard Galerkin finite element procedure and its spatial refinement in the context of capturing coupled HTM processes within a GCS system. This presents a coupled set of nonlinear first-order ordinary differential equations in time. The system is discretised temporally and solved using an embedded finite difference method which is schemed with control theoretical techniques and an accelerated fixed-point-type procedure. -
The Heat Transfer Module User's Guide
Heat Transfer Module User’s Guide Heat Transfer Module User’s Guide © 1998–2018 COMSOL Protected by patents listed on www.comsol.com/patents, and U.S. Patents 7,519,518; 7,596,474; 7,623,991; 8,457,932; 8,954,302; 9,098,106; 9,146,652; 9,323,503; 9,372,673; and 9,454,625. Patents pending. This Documentation and the Programs described herein are furnished under the COMSOL Software License Agreement (www.comsol.com/comsol-license-agreement) and may be used or copied only under the terms of the license agreement. COMSOL, the COMSOL logo, COMSOL Multiphysics, COMSOL Desktop, COMSOL Server, and LiveLink are either registered trademarks or trademarks of COMSOL AB. All other trademarks are the property of their respective owners, and COMSOL AB and its subsidiaries and products are not affiliated with, endorsed by, sponsored by, or supported by those trademark owners. For a list of such trademark owners, see www.comsol.com/trademarks. Version: COMSOL 5.4 Contact Information Visit the Contact COMSOL page at www.comsol.com/contact to submit general inquiries, contact Technical Support, or search for an address and phone number. You can also visit the Worldwide Sales Offices page at www.comsol.com/contact/offices for address and contact information. If you need to contact Support, an online request form is located at the COMSOL Access page at www.comsol.com/support/case. Other useful links include: • Support Center: www.comsol.com/support • Product Download: www.comsol.com/product-download • Product Updates: www.comsol.com/support/updates • COMSOL Blog: www.comsol.com/blogs • Discussion Forum: www.comsol.com/community • Events: www.comsol.com/events • COMSOL Video Gallery: www.comsol.com/video • Support Knowledge Base: www.comsol.com/support/knowledgebase Part number: CM020801 Contents Chapter 1: Introduction About the Heat Transfer Module 20 Why Heat Transfer is Important to Modeling .