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Computational Models for Prediction of Fire Behaviour Dr. Andrej Horvat Intelligent Fluid Solutions Ltd. Ljubljana, Slovenia 17 January, 2008 Contact information IFS Andrej Horvat Intelligent Fluid Solution Ltd. 127 Crookston Road, London, SE9 1YF, United Kingdom Tel./Fax: +44 (0)1235 819 729 Mobile: +44 (0)78 33 55 63 73 E-mail: [email protected] Web: www.intelligentfluidsolutions.co.uk 2 Personal information IFS 1995, Dipl. -Ing. Mech. Eng. (Process Tech.) University of Maribor 1998, M.Sc. Nuclear Eng. University of Ljubljana 2001, Ph.D. Nuclear Eng. University of Ljubljana 2002, M.Sc. Mech. Eng. (Fluid Mechanics & Heat Transfer) University of California, Los Angeles 3 Personal information IFS More than 10 years of intensive CFD related experience: R&D of numerical methods and their implementation (convection schemes, LES methods, semi-analytical methods, Reynolds Stress models) Design analysis (large heat exchangers, small heat sinks, burners, drilling equip., flash furnaces, submersibles) Fire prediction and suppression (backdraft, flashover, marine environment, gas releases, determination of evacuation criteria) Safety calculations for nuclear and oil industry (water hammer, PSA methods, severe accidents scenarios, pollution dispersion) 4 Personal information IFS As well as CFD, experiences also in: Experimental methods QA procedures Standardisation and technical regulations Commercialisation of technical expertise and software products 5 Contents IFS Overview of fluid dynamics transport equations - transport of mass, momentum, energy and composition - influence of convection, diffusion, volumetric (buoyancy) force - transport equation for thermal radiation Averaging and simplification of transport equations - spatial averaging - time averaging - influence of averaging on zone and field models Zone models - basics of zone models (1 and 2 zone models) - advantages and disadvantages 6 Contents Field models - IFS numerical mesh and discretisation of transport equations turbulence models (k-epsilon, k-omega, Reynolds stress, LES) combustion models (mixture fraction, eddy dissipation, flamelet) thermal radiation models (discrete transfer, Monte Carlo) examples of use Conclusions - software packages Examples - diffusion flame - fire in an enclosure - fire in a tunnel 7 Some basic thoughts … IFS Today, CFD methods are well established tools that help in design, prototyping, testing and analysis The motivation for development of modelling methods (not only CFD) is to reduce cost and time of product development, and to improve efficiency and safety of existing products and installations Verification and validation of modelling approaches by comparing computed results with experimental data are necessary Nevertheless, in some cases CFD is the only viable research and design tool (e.g. hypersonic flows in rarefied atmosphere) 8 IFS Overview of fluid dynamics transport equations 9 Transport equations IFS The continuum assumption - A control volume has to contain a large number of particles (atoms or molecules): Knudsen number << 1.0 - At equal distribution of particles (atoms or molecules) flow quantities remain unchanged despite of changes in location and size of a control 10 volume Transport equations IFS Eulerian and Lagrangian description Eulerian description – transport equations for mass, momentum and energy are written for a (stationary) control volume Lagrangian description – transport equations for mass, momentum and energy are written for a moving material particle 11 IFS Transport equations Transport of mass and composition dm d dV dt dt MR dm j dt d j dV dt MR Transport of momentum Transport of energy 12 Transport equations IFS Majority of the numerical modelling in fluid mechanics is based on Eulerian formulation of transport equations Using the Eulerian formulation, each physical quantity is described as a mathematical field. Therefore, these models are also named field models Lagrangian formulation is basis for modelling of particle dynamics: bubbles, droplets (sprinklers), solid particles (dust) etc. 13 Transport equations IFS Droplets trajectories from sprinklers (left), gas temperature field during fire suppression (right) 14 IFS Transport equations Eulerian formulation of mass transport equation integral form differential (weak) form The equation also appears in the following forms change of mass in a control vol. flux difference (convection) non-conservative form ~0 in incompressible 15 fluid flow IFS Transport equations Eulerian formulation of mass fraction transport equation (general form) d j dV MR ni qi dS dt MR t j i vi j i qi change of mass of a flux component in a difference control vol. (convection) diffusive mass flow 16 Transport equations IFS Eulerian formulation of momentum equation change of momentum volumetric pressure viscous force in a control vol. force flux difference force (diffusion) (convection) 17 Transport equations IFS Eulerian formulation of energy transport equation change of internal energy flux deformation diffusive heat in a control vol. difference work flow (convection) 18 IFS Transport equations The following physical laws and terms also need to be included diffusive terms - Newton's viscosity law flux is a linear - Fourier's law of heat conduction function of a gradient - Fick's law of mass transfer - Sources and sinks due to thermal radiation, chemical reactions etc. 19 Transport equations IFS Transport of mass and composition t i vi M t j i vi j i D i j M j Transport of momentum t v j i vi v j j p 2 i Sij g j F j Sij 1 j vi i v j 2 Transport of energy t h i vi h i iT Q 20 IFS Transport equations Lagrangian formulation is simpler - equation of the particle location dx u dt - mass conservation eq. for a particle dm M dt - momentum conservation eq. for a particle du m FD FL FV dt drag lift volumetric forces 21 IFS Transport equations - thermal energy conservation eq. for a particle mc p dT QC QL QR dt convection latent heat thermal radiation Conservation equations of Lagrangian model need to be solved for each representative particle 22 IFS Transport equations Thermal radiation s I(s) I(s+ds) dA Ie Is K dI K a K s I K a I e s I s P' d' ds 4 4 change of radiation intensity absorption emission and out-scattering in-scattering 23 IFS Transport equations Thermal radiation Equations describing thermal radiation are much more complicated - spectral dependency of material properties - angular (directional) dependence of the radiation transport dI K K a K s I K a I e s ds 4 change of radiation intensity absorption emission and out-scattering I ' P ' d' s 4 in-scattering 24 IFS Averaging and simplification of transport equations 25 Averaging and simplification of transport equations IFS The presented set of transport equations is analytically unsolvable for the majority of cases Success of a numerical solving procedure is based on density of the numerical grid, and in transient cases, also on the size of the integration time-step Averaging and simplification of transport equations help (and improve) solving the system of equations: - derivation of averaged transport equations for turbulent flow simulation - derivation of integral (zone) models 26 IFS Averaging and simplification of transport equations Averaging and filtering , vi , p, h , w The largest flow structures can occupy the whole flow field, whereas the smallest vortices have the size of Kolmogorov scale 3 1 4 u 1 4 1 2 27 Averaging and simplification of transport equations IFS Kolmogorov scale is (for most cases) too small to be captured with a numerical grid Therefore, the transport equations have to be filtered (averaged) over: - spatial interval Large Eddy Simulation (LES) methods h x ,t G x h ,t d h x ,t h x ,t h' x ,t - time interval k-epsilon model, SST model, Reynolds stress models h x ,t G t h x , d h x ,t h x ,t h x ,t 28 IFS Averaging and simplification of transport equations Transport equation variables can be decomposed onto a filtered (averaged) part and a residual (fluctuation) ' p p p' vi vi vi* v~i vi* ~ i i * ~ hi h h* Filtered (averaged) transport equations ~ ~ t j i v~i j M j i j t j ( v~j ) M t v~j i v~i v~j j p 2i Sij g j Fj i ij ~ ~ ~ t h i v~i h i iT Q i i turbulent heat fluxes turbulent mass fluxes sources and sinks represent a separate problem and require additional models - turbulent stresses - Reynolds stresses - subgrid stresses 29 Averaging and simplification of transport equations Turbulent stresses IFS ji v j vi v~j v~i v*j vi* Transport equation t ji k v~k ji k p' v*j ik p' vi* jk vi* v*j v*k v*jTik ' vi*T jk ' p' ( j vi* i v*j ) ik k v~j jk k v~i F j vi F j v~i Fi v j Fi v~j Tik ' v T jk ' v * k j * k i v*j k p ik Tik vi* k p jk T jk higher order product turbulence generation turbulence dissipation - the equation is not solvable due to the higher order product - all turbulence models include at least some of the terms of this equation (at least the generation and the dissipation term) 30 Averaging and simplification of transport equations IFS Turbulent heat and mass fluxes ~ j v j h v~j h Transport equation t j k v~k j k p' h* jk v*k v*j h* v*j qk ' h*Tkj ' ~ ~ ~ vk vj k h vk h k v~j F j h F j h Q h Q h qk k v*j Tkj k h* v*j h* higher order product generation dissipation h* k p jk Tkj v*j k qk - the equation is not solvable due to the higher order product - most of the turbulence models do not take into account the equation 31 IFS Averaging and simplification of transport equations Turbulent heat fluxes due to thermal radiation - little is known and published on the subject - majority of models do not include this contribution - radiation heat flow due to turbulence Qs ~ T ' 4 32 Averaging and simplification of transport equations IFS Buoyancy induced flow over a heat source (Gr=10e10); inert model of a fire 33 Averaging and simplification of transport equations IFS (a) LES model; instantaneous temperature field 34 Averaging and simplification of transport equations (a) a) IFS b) Temperature field comparison: a) steady-state RANS model, b) averaged LES model results 35 Averaging and simplification of transport equations (a) IFS a) b) Comparison of instantaneous mass fraction in a gravity current : a) transient RANS model, b) LES model 36 Averaging and simplification of transport equations IFS Additional simplifications - flow can be modelled as a steady-state case the solution is a result of force, energy and mass flow balance taking into consideration sources and sinks - fire can be modelled as a simple heat source inert models; do not need to solve transport equations for composition - thermal radiation heat transfer is modelled as a simple sink of thermal energy FDS takes 35% of thermal energy - control volumes can be so large that continuity of flow properties is not preserved zone models 37 IFS Zone models 38 Zone models IFS Basics - theoretical base of zone model is conservation of mass and energy in a space separated onto zones - thermodynamic conditions in a zone are constant; in fields models the conditions are constant in a control volume - zone models take into account released heat due to combustion of flammable materials, buoyant flows as a consequence of fire, mass flow, smoke dynamics and gas temperature - zone models are based on certain empirical assumptions - in general, they can be divided onto one- and two-zone models 39 IFS Zone models One-zone and two-zone models - one-zone models can be used only for assessment of a fully developed fire after flashover - in such conditions, a valid approximation is that the gas temperature, density, internal energy and pressure are (more or less) constant across the room Qw (konv+rad) Qout (konv+rad) Qin (konv) pg , Tg , mg , vg mout mf , H f min 40 IFS Zone models One-zone and two-zone models - two-zone models can be used for evaluation of a localised fire before flashover - a room is separated onto different zone, most often onto an upper and lower zone, a fire and buoyant flow of gases above the fire - conditions are uniform and constant in each zone Qw (konv+rad) mU,out mL,out mf , Hf Qin (konv) zgornja cona QU,out (konv+rad) pU,g , TU,g , mU,g , vU,g spodnja cona pL,g , TL,g , mL,g , vL,g mL,in QL,out (konv+rad) 41 Zone models IFS Advantages and disadvantages of zone models - in zone models, ordinary differential equations describe the conditions more easily solvable equations - because of small number of zones, the models are fast - simple setup of different arrangement of spaces as well as of size and location of openings - these models can be used only in the frame of theoretical assumptions that they are based on - they cannot be used to obtain a detailed picture of flow and thermal conditions - these models are limited to the geometrical arrangements that they can describe 42 IFS Field models 43 Field models IFS Numerical grid and discretisation of transport equations - analytical solutions of transport equations are known only for few very simple cases - for most real world cases, one needs to use numerical methods and algorithms, which transform partial differential equations to a series of algebraic equations - each discrete point in time and space corresponds to an equation, which connects a grid point with its neighbours - The process is called discretisation. The following methods are used: finite difference method, finite volume method, finite element method and boundary element method (and different hybrid methods) 44 IFS Field models Numerical grid and discretisation of transport equations - simple example of discretisation ui 1 ui x 0 x x u lim ui 1 2ui ui 1 x 0 x 2 x x u lim - many different discretisation schemes exist; they can be divided onto conservative and non-conservative schemes (linked to the discrete form of the convection term) ui 1ui 1 ui ui x 0 x x u u lim u x u lim ui 1 2 x 0 ui 1 ui x 45 Field models IFS Numerical grid and discretisation of transport equations - non-conservative schemes represent a linear form and therefore they are more stable and numerically better manageable - non-conservative schemes do not conserve transported quantities, which can lead to time-shift of a numerical solution time-shift due to a non-conservative scheme 46 IFS Field models Numerical grid and discretisation of transport equations - quality of numerical discretisation is defined with discrepancy between a numerical approximation and an analytical solution - error is closely link to the order of discretisation x 2 u x x u x x xu x x xu x ....... 2 u x x u x x xu x x xu x . ...... x 2 1st order truncation (~x) 47 Field models IFS Numerical grid and discretisation of transport equations - higher order methods lead to lower truncation errors, but more neighbouring nodes are needed to define a derivative for a discretised transport equation - two types of numerical error: dissipation and dispersion 48 Field models IFS Numerical grid and discretisation of transport equations - during the discretisation process most of the attention goes to the convection terms - the 1st order methods have dissipative truncation error, whereas the 2nd order methods introduce numerical dispersion - today's hybrid methods are a combination of 1st and 2nd order accurate schemes. These methods switch automatically from a 2nd order to a 1st order scheme near discontinuities to damp oscillations (TVD schemes) - there are also higher order schemes (ENO, WENO etc.) but their use is limited on structured numerical meshes 49 IFS Field models Numerical grid and discretisation of transport equations - connection matrix and location of neighbouring grid nodes defines two types of numerical grid: structured and unstructured numerical grid i-1, j+1 i, j+1 i+1, j+1 k+2 k+1 k+6 i-1, j i, j i+1, j k+9 k k+3 i-1, j-1 i, j-1 i+1, j-1 k+7 k+5 k+4 structured grid unstructured grid 50 Field models IFS Numerical grid and discretisation of transport equations - unstructured grids raise a possibility of arbitrary orientation and form of control volumes and therefore offer larger geometrical flexibility - all modern simulation packages (CFX, Fluent, Star-CD) are based on the unstructured grid arrangement 51 Field models IFS Numerical grid and discretisation of transport equations - flame above a burner - automatic refinement of unstructured numerical grid - start with 44,800 control volumes; 3 stages of refinement which leads to 150,000 cont. volumes - refinement criteria velocity and temperature gradients 52 IFS Turbulence models 53 Turbulence models IFS laminar flow transitional flow turbulent flow van Dyke, 1965 54 Turbulence models IFS Turbulence models introduce additional (physically related) diffusion to a numerical simulation This enables : - RANS models to use a larger time step (Δt >> Kolmogorov time scale) or even steady-state simulation - LES models to use less dense (smaller) numerical grid (Δx > Kolmogorov length scale) The selection of the turbulence model influences the distribution of the simulated flow fundamentally and hence that of the flow variables (velocity, temperature, heat flow, composition etc) 55 Turbulence models IFS In general 2 kinds of averaging (filtering) exist, which leads to 2 families of turbulence models: - filtering over a spatial interval Large Eddy Simulation (LES) models - filtering over a time interval Reynolds Averaged Navier-Stokes (RANS) models: k-epsilon model, SST model, Reynolds Stress models etc For RANS models, size of the averaging time interval is not known or given (statistical average of experimental data) For LES models, size of the filter or the spatial averaging interval is a basic input parameter (in most case it is equal to grid spacing) 56 IFS Turbulence models Reynolds Averaged Navier-Stokes (RANS) models For two-equation models (e.g. k-epsilon, k-omega or SST), 2 additional transport equations need to be solved: - for kinetic energy of turbulent fluctuations k 1 2 ii - for dissipation of turbulent fluctuations ( j vi* j vi* ) or - for frequency of turbulent fluctuations ~ k 57 IFS Turbulence models Reynolds Averaged Navier-Stokes (RANS) models k-epsilon model t k j v~j k P G j ( t ) j k k t 2 ~ t j v j C1 P C3 max(G ,0) j ( ) j C2 k k convection production (source) term production (source) term diffusion destruction (sink) term 2 P 2 t Sij j v~i l v~l k 3 t l v~l 3 G t g j j Prt 58 IFS Turbulence models Reynolds Averaged Navier-Stokes (RANS) models - model parameters are usually defined from experimental data e.g. dissipation of grid generated turbulence or flow in a channel C C C C Pr 1 0.09 1.44 2 1.92 3 1.0 k 1.0 1.3 t 0.9 - from the calculated values of k in , eddy viscosity is defined as 2 t C ρ k - from eddy viscosity, Reynolds stresses, turbulent heat and mass fluxes are obtained 1 2 ij ll ji 2 t Sij t ( l v~l ) ji 3 3 j t ~ jh Prt j t ~ j Sct 59 Turbulence models IFS Reynolds Averaged Navier-Stokes (RANS) models - transport equation for k is derived directly from the transport equations for Reynolds stresses ij - transport equation for is empirical - these equations have a common form: source and sink term, convection and diffusion term - the rest of the terms are model specific and they can be numerically and computationally very demanding - definition and implementation of boundary conditions is different even for the same turbulence model between different software vendors 60 IFS Turbulence models Reynolds Averaged Navier-Stokes (RANS) models For Reynolds Stress (RS) model, 7 additional transport equations need to be solved: - for 6 components of Reynolds stress tensor xx , xy , xz , yy , yz , zz - for dissipation of turbulent fluctuations ( j vi* j vi* ) or - for frequency of turbulent fluctuations ~ k 61 Turbulence models IFS Reynolds Averaged Navier-Stokes (RANS) models Reynolds stress model 2 2 k2 ~ t ij l vl ij Pij ij l ( Cs ) l ij ij 3 3 t 2 ~ t l vl C1 P l ( ) l C 2 k k convection generation (source) term generation diffusion term (source) term pressure-velocity fluctuation term destruction (sink) term Pij ik k u~ j jk k u~i 62 Turbulence models IFS Reynolds Averaged Navier-Stokes (RANS) models - Reynolds stress models calculate turbulent stresses directly introduction of eddy viscosity is not needed - includes the pressure-velocity fluctuation term 2 1 ij C1 ij kij C2 Pij Pll ij k 3 3 - describes anisotropic turbulent behaviour - computationally more demanding than the two-equation models - due to higher order terms (linear and non-linear), RS models are numerically more complex (convergence) 63 Turbulence models IFS Large Eddy Simulation (LES) models - Large Eddy Simulation (LES) models are based on spatial filtering (averaging) - many different forms of the filter exist, but most common is "top hat" filter (simple geometrical averaging) - the size of the filter is based on grid node spacing Basic assumption of LES methodology: Size of the used filter is so small that the averaged flow structures do no influence large structures, which contain most of the energy. These small structures are being deformed, disintegrated onto even smaller structures until they do not dissipate due to viscosity (kinetic energy thermal energy). 64 IFS Turbulence models Large Eddy Simulation (LES) models - required size of flow structures for LES modelling 1 k l lEI ~ 6 32 - these structures are in the turbulence inertial subrange and they are isotropic - on this level, turbulence production is of the same size as turbulence dissipation ik k v~i Fi vi Fi v~i 65 IFS Turbulence models Large Eddy Simulation (LES) models - eddy (turbulent) viscosity is defined as t ~ l 4 / 31 / 3 where l ~ Cs grid spacing - using the definition of turbulent (subgrid) stresses 2 2 ji k ji 2 t Sij t ( l v~l ) ji 3 3 and turbulent fluxes j t ~ jh Prt the expression for turbulent viscosity can be written as t Cs 2S ji Sij G 2 1/ 2 where the contribution due to buoyancy is ~ gi i h G~ ~ Prt h 66 Turbulence models IFS Large Eddy Simulation (LES) models - presented Smagorinsky model is the simplest from LES models - it requires knowledge of empirical parameter Cs, which is not constant for all flow conditions - newer, dynamic LES models calculates Cs locally - the procedure demands introduction of the secondary filter - LES models demand much denser (larger) numerical grid - they are used for transient simulations - to obtain average flow characteristics, we need to perform statistical averaging over the simulated time interval 67 IFS Turbulence models Comparison of turbulence models 10 10 k-e (Gr = 10 ) k-e N&B (Gr = 10 10 ) 10 RNG k-e (Gr = 10 ) 10 S S T (Gr = 10 ) 10 S S G (Gr = 10 ) 10 LES (Gr = 10 ) Rous e e t al. (1952) S habbir and Ge orge (1994) 8 7 6 5 4 k-e (Gr = 10 ) k-e N&B (Gr = 10 10 ) 10 RNG k-e (Gr = 10 ) 10 S S T (Gr = 10 ) 10 S S G (Gr = 10 ) 10 LES (Gr = 10 ) Rous e e t al. (1952) S habbir and Ge orge (1994) 10 -1 b c (R 5 /F 02 )1/3 w c (R/F0 )1/3 3 2 1 10 -2 25 50 z/R a) 75 100 25 50 75 100 z/R b) Buoyant flow over a heat source: a) velocity, b) temperature* 68 IFS Combustion models 69 IFS Combustion models Chen et al., 1988 Grinstein, Kailasanath, 1992 70 Combustion models IFS Combustion can be modelled with heat sources - information on chemical composition is lost - thermal loading is usually under-estimated Combustion modelling contains - solving transport equations for composition - chemical balance equation - reaction rate model Modelling approach dictates the number of additional transport equations required 71 IFS Combustion models Modelling of composition requires solving n-1 transport equations for mixture components – mass or molar (volume) fractions ~ ~ t j i v~i j i t Sc Sct ~ i j M j Chemical balance equation can be written as ' A A ' B B 'C C ..... " A A " B B "C C ..... or N N ' I " I I A ,B ,C.... I I A ,B ,C.... I 72 IFS Combustion models Reaction source term is defined as M j W j " j ' j R or for multiple reactions M j W j "k , j ' k , j Rk k where R or Rk is a reaction rate Reaction rate is determined using different models - Constant burning (reaction) velocity - Eddy break-up model and Eddy dissipation model - Finite rate chemistry model - Flamelet model - Burning velocity model 73 IFS Combustion models Constant burning velocity sL sF c sL h speed of flame front propagation is larger due to expansion - values are experimentally determined for ideal conditions - limits due reaction kinetics and fluid mechanics are not taken into account - source/sink in mass fraction transport equation - source/sink in energy transport equation M j ~ f sL l Q ~ M j hc - expressions for sL usually include additional models 74 IFS Combustion models Eddy break-up model and Eddy dissipation model - is a well established model - based on the assumption that the reaction is much faster than the transport processes in flow - reaction rate depends on mixing rate of reactants in turbulent flow s ~ k L - Eddy break-up model reaction rate R ~ ' 2f k - Eddy dissipation model reaction rate ~ ~ ~ p o R C A min f , ,CB k s 1 s 75 Combustion models IFS Eddy break-up model and Eddy dissipation model - typical values of model coefficients CA = 4 in CB = 0.5 - the model can be used for simple reactions (one- and two-step combustion) - in general, it cannot be used for prediction of products of complex chemical processes (NO, CO, SOx, etc) - the use can be extended by adding different reaction rate limiters → extinction due to turbulence, low temperature, chemical time scale etc. 76 Combustion models IFS Backdraft simulation 77 Combustion models IFS Finite rate chemistry model - it is applicable when a chemical reaction rate is slow or comparable with turbulent mixing - reaction kinetics must be known ~ E ~ ' I R AT exp ~a I RT I A ,B ,C ... - for each additional component, the component molar concentration I needs to be multiplied with the product - for each additional reaction the same expression is added 78 Combustion models IFS Finite rate chemistry model - the model is numerically demanding due to exponential terms - often the model is used in combination with the Eddy dissipation model 79 Combustion models IFS Flamelet model - describes interaction of reaction kinetics with turbulent structures for a fast reaction (high Damköhler number) - basic assumption is that combustion is taking place in thin sheets - flamelets - turbulent flame is an ensemble of laminar flamelets - the model gives a detailed picture of chemical composition - resolution of small length and time scales of the flow is not needed - the model is also known as "Mixed-is-burnt" - large difference between various implementations of the model 80 IFS Combustion models Flamelet model - the model is only applicable for two-feed systems (fuel and oxidiser) - it is based on definition of a mixture fraction Z kg/s fuel A 1-Z kg/s oxidiser B mešalni proces Z A 1 Z B M or 1 kg/s mixture M Z M B A B Z is 1 in a fuel stream, 0 in an oxidiser stream 81 IFS Combustion models Flamelet model - conserved property often used in the mixture fraction definition f o i - for a simple chemical reaction 1kg fuel i kg oxidiser 1 i kg products the stoihiometric ratio is f ST 1 (1 i) 82 Combustion models IFS Flamelet model - Shvab-Zel'dovich variable f o o i i B Z f A io B - the conditions in vicinity of flamelets are described with the respect to Z; Z=Zst is a surface with the stoihiometric conditions - transport equations are rewritten with Z dependencies; conditions are one-dimensional ξ(Z) , T(Z) etc. - for limited cases, the simplified equations can be solve analytically 83 IFS Combustion models Flamelet model - numerical implementations of the model differ significantly - for turbulent flow, we need to solve an additional transport equation for mixture fraction Z ~ ~ t Z i v~i Z i t Sc Sct ~ i Z - and a transport equation for variation of mixture fraction Z" ~'' 2 ~ ~'' 2 t Z i ui Z i D t Sct ~ ~'' 2 t '' 2 ~2 i Z 2 i Z C Z Sc k t 84 IFS Combustion models Flamelet model - composition is calculated from preloaded libraries 1 ~ Z PDF Z dZ j j 0 1 ~ Z , PDF Z PDF dZ d j j 0 0 these PDFs are tabulated for different fuel, oxidiser, pressure and temperature - is the scalar dissipation rate - it increases with stresses (stretching of a flame front) and decreases with diffusion. - at critical value of flame extinguishes 85 Combustion models IFS Flamelet model Ferreira, Schlatter, 1995 86 Combustion models IFS Burning velocity model - it is used for pre-mixed or partially pre-mixed combustion - contains: a) model of the reaction progress: Burning Velocity Model (BVM) or Turbulent Flame Closure (TFC) b) model for composition of the reacting mixture: Flamelet model - definition of the reaction progress variable c, where c = 0 corresponds to the fresh mixture, and c = 1 to combustion products ~ 1 c~ ~ ~~ j j ,svezi c j ,zgoreli 87 IFS Combustion models Burning velocity model Preheating T, j Reaction layer O() Oxidation layer Temperature Oxidiser Products Fuel x Flame location lF 0.1 ... 0.5 mm l 0.01 mm 88 IFS Combustion models Burning velocity model - additional transport equation for the reaction progress variable ~ ~ ~ t c i vi c i D t Sct ~ i c M source term - source/sink due to combustion is defined as M freshST c~ modelling of the turbulent burning velocity - better results by solving the transport equation for weighted reaction progress variable ~ ~ ~ F Z 1 c 89 Combustion models IFS Burning velocity model - it is suitable for a single step reaction - applicable for fast chemistry conditions (Da >> 1) - a thin reaction zone assumption - fresh gases and products need to be separated 90 IFS Thermal radiation models 91 IFS Thermal radiation It is a very important heat transfer mechanism during fire In fire simulations, thermal radiation should not be neglected The simplest approach is to reduce the heat release rate of a fire (35% reduction in FDS) Modelling of thermal radiation - solving transport equation for radiation intensity dI K K a K s I K a I e s ds 4 change of intensity absorption emission and scattering I ' P ' d' s 4 in-scattering 92 IFS Thermal radiation Radiation intensity is used for definition of a source/sink in the energy transport equation and radiation wall heat fluxes Energy spectrum of blackbody radiation 22 n 2 h E T I T 2 [Wm -2 Hz -1 ] c exph k BT 1 - frequency c - speed of light n - refraction index h - Planck's constant kB - Boltzmann's constant integration over the whole spectrum E T n T E T d [Wm -2 ] 2 4 0 93 IFS Thermal radiation Models - Rosseland (primitive model, for optical thick systems, additional diffusion term in the energy transport equation) q qd qr kd kr iT 16n 2T 3 kr 3 - P1 (strongly simplified radiation transport equation - solution of an additional Laplace equation is required) G I d 4 - Discrete Transfer (modern deterministic model, assumes isotropic scattering, reasonably homogeneous properties) - Monte Carlo (modern statistical model, computationally demanding) 94 IFS Thermal radiation Discrete Transfer - modern deterministic model - assumes isotropic scattering, homogeneous gas properties - each wall cell works as a radiating surface that emits rays through the surrounding space (separated onto multiple solid angles) - radiation intensity is integrated along each ray between the walls of the simulation domain I (r , s) I 0 e - K a K s s I e 1 e K a s K s I qrad , j I r , s cos j cos d 4 - source/sink in the energy transport equation Q rad i qirad 95 Thermal radiation IFS Monte Carlo - it assumes that the radiation intensity is proportional to (differential angular) flux of photons - radiation field can be modelled as a "photon gas" - absorption constant Ka is the probability per unit length of photon absorption at a given frequency - average radiation intensity I is proportional to the photon travelling distance in a unit volume and time - radiation heat flux qrad is proportional to the number of photon incidents on the surface in a unit time - accuracy of the numerical simulation depends on the number of used "photons" 96 Thermal radiation IFS These radiation methods can be used: - for averaged radiation spectrum - grey gas - for gas mixture, which can be separated onto multiple grey gases (such grey gas is just a modelling concept) - for individual frequency bands; physical parameters are very different for each band 97 Thermal radiation IFS Flashover simulation 98 IFS Conclusions 99 Conclusions IFS The seminar gave a short (but demanding) overview of fluid mechanics and heat transfer theory that is relevant for fire simulations All current commercial CFD software packages (ANSYSCFX, ANSYS-Fluent, Star-CD, Flow3D, CFDRC, AVL Fire) contain most of the shown models and methods: - they are based on the finite volume or the finite element method and they use transport equations in their conservative form - numerical grid is unstructured for greater geometrical flexibility - open-source computational packages exist and are freely accessible (FDS, OpenFoam, SmartFire, Sophie) 100 Conclusions IFS I would like to remind you to the project "Methodology for selection and use of fire models in preparation of fire safety studies, and for intervention groups", sponsored by Ministry of Defence, R. of Slovenia, which contains an overview of functionalities that are offered in commercial software products 101 Acknowledgement IFS I would like to thank to our hosts and especially to Aleš Jug I would like to thank to ANSYS Europe Ltd. (UK) who permitted access to some of the graphical material 102