Title: Interaction of Turbulence, Chemistry, and Radiation in Strained Nonpremixed Flames
1Interaction of Turbulence, Chemistry, and
Radiation in Strained Nonpremixed Flames
- Chun Sang Yoo, Hong G. Im
- Department of Mechanical Engineering
- University of Michigan
- Yi Wang, Arnaud Trouvé
- Department of Fire Protection Engineering
- University of Maryland
- Sponsored by the DOE SciDAC Program
- http//purl.org/net/tstc
2Outline of Presentation
- Introduction
- Role of DNS in Combustion Science (a brief
version) - Overview Terascale High-Fidelity Simulations of
Turbulent Combustion with Detailed Chemistry
(TSTC) - Research Highlights (work led by U. Michigan)
- Computational Improved Navier-Stokes
Characteristic Boundary Conditions (NSCBC) - Science Counterflow Diffusion Flames with Soot
and Radiation Models - Ongoing/Future Work
- More TSTC Research Highlights Poster
Session - WED21 Trouvé and Wang (Maryland)
- WED22 Rutland and Wang (Wisconsin)
3DNS A Computational Microscope
- A diagnostic tool to study the fundamental
physics of turbulent reacting flows - Full access to temporally/spatially resolved
information. - Allows identification of key paths for relevant
phenomena, such as turbulence-chemistry
interaction - A benchmark tool to develop and validate physical
submodels used in macro-scale simulations of
engineering-level systems (LES with
embedded DNS)
Formation of edge flames in a turbulent
counterflow
Physical Models
Engineering-level CFD Codes
DNS
A KIVA-3V engine simulation
4Terascale High-Fidelity Simulations of Turbulent
Combustion with Detailed Chemistry (TSTC)
http//purl.org/net/tstc
Software architecture
Numerical algorithms
SciDAC CFRFS
. S3D0 F90 MPP 3D . S3D1 GrACE-based . S3D2
CCA-compliant
. IMEX ARK . IBM . AMR
Physical models
SciDAC CCA
. Thermal radiation . Soot formation . Spray
dynamics
MPP S3D
SciDAC CMCS SDM
Hong G. Im, University of Michigan Arnaud Trouvé,
University of Maryland Chris Rutland, University
of Wisconsin Jackie Chen, Sandia National Labs
Post-processors In-situ visualization Feature
tracking
5S3D MPP DNS Code
- S3D code characteristics
- Compressible reacting Navier-Stokes, total
energy, species equations - Fortran 90, MPI domain decomposition
- Highly scalable and portable on all modern
architectures - Numerical algorithms
- 8th order non-dissipative spatial finite
difference, 10th order dealiasing filter - 4th order explicit RK integrator with error
monitoring - Additive 4th order RK integrator for stiff
chemistry - Improved boundary conditions to allow transverse
velocity, flame passage through boundary, or
solid walls
- Physical models
- Lewis number, mixture averaged, or
multi-component transport - Detailed gas-phase chemical kinetics
- (Chemkin-compatible)
- All thermodynamic properties are functions of T,
p, and Yi - Radiative heat transfer (discrete ordinate /
discrete transfer method) - Soot formation
- Lagrangian spray model
- Recent Contributions from the SciDAC TSTC
Project
6Characteristic Boundary Conditions
- A pre-requisite issue for high-quality
turbulent combustion DNS - Historical Development
- General nonreflecting outflow boundary conditions
- (Engquist and Majda 1977, Hedstrom 1979)
- Pressure damping for Navier-Stokes equations
- (Rudy Strikwerda 1980, 1981)
- Inviscid characteristic theory for Euler
equations (Thompson 1987,1990) - Navier-Stokes characteristic boundary conditions
(NSCBC) - Viscous conditions (Poinsot Lele
1992) - Multi-component reacting flows (Baum et al. 1994)
- Applications to turbulent and reacting flows have
revealed problems of spurious pressure waves,
numerical instabilities. - Reaction source terms (Sutherland Kennedy 2003)
7Characteristic Waves
- Li characteristic wave with ?i
- (wave velocities, ?1 (u?c), ?2?3?4u, ?5
(uc))
Computational domain
inflow
outflow
flow
8Locally One-Dimensional Inviscid (LODI) Relations
- Neglecing transverse convection, viscous, and
reactive terms - The incoming Lis can be determined at both
inflow and outflow boundaries using LODI
relations - Hard inflow boundary conditions yield large
spurious wave reflections nonreflecting
conditions are needed
9Generalized NSCBC for Transverse, Viscous,
Reacting Flows
- LODI relations are no longer valid transverse,
viscous, reaction terms must be considered in Lis
Outflow boundary conditions (at x lx)
Conventional LODI
Improved BC
Spatial
Temporal
Low-Ma asymptotic expansion yields
10Test 1 Vortex-Convection
- Incompressible inviscid vortex
- Conditions
- Three different boundary conditions
- BC1 conventional LODI with
- BC2 keep all the transverse terms (a 0.0)
- BC3 improved BC with pressure and transverse
damping (a M 0.05)
11Vorticity and Pressure
??
LODI
BC2 (a 0.0)
Improved BC (a 0.05)
P
12Velocities
u
LODI
BC2 (a 0.0)
Improved BC (a 0.05)
v
13Temporal Pressure Variation
- Examine how the solution approaches the steady
state - The L2-norm
Temporal variations of the L2-norms of pressure
difference
14Test 2 Ignition H2-O2 Mixture
- Stoichiometric H2-O2 mixture diluted with 50 N2
by volume - 2mm ? 2mm (200 ? 200 grid points)
- Initial temperature and pressure, 300K and 1atm
- Initial Gaussian temperature peak
- Three test cases
- Case A conventional LODI
- Case B include source terms in incoming Lis
(Sutherland Kennedy 2003) - Case C improved BC with a 0.125 (scaling
analysis)
15Temperature and HO2
T
Case A (LODI)
Case B (Sutherland Kennedy)
Case C (Improved BC)
YHO2
16Test 3 Poiseuille Flow (Isothermal Wall)
- Viscous terms must be considered
- Test cases
- Case A conventional LODI B.C. with ?1,exact
- Case B including only pressure damping term (a
0.0) - Case C improved B.C. with a 0.1
- The pressure level of Case A is increased because
?1,exact does not cancel out all the viscous and
heat flux effect - The velocity at the outflow boundary in Case B is
not accurate transverse damping term is needed
Temporal variation of pressure
17Test 4 Turbulent Reacting Counterflow
- Transverse terms cannot be ignored
- a 0.01
- Use the steady laminar H2?air nonpremixed
counterflow flame as the initial condition - Turbulence inflow condition
- Velocity fluctuations are superimposed on the
mean inlet velocities. - Homogenous turbulence
(a) temperature
(b) vorticity
18Strained Nonpremixed Flames with Soot and
Radiation
- Motivation
- Predictive tools for pollutant formation (soot,
NOx) - Thermal radiation plays an important role, but
has not been incorporated in high-fidelity
simulations - Need better understanding of interaction between
flow, chemistry, and heat transfer - Objectives
- To develop high-fidelity DNS capabilities with
advanced physical submodels for soot and
radiation - Validate and assess the impact of the advanced
physical models in a canonical configuration
(flame-vortex) - Perform laboratory-scale simulations to answer
science questions on turbulence-chemistry-radiatio
n interaction (future work)
19Radiation Models in S3D
- Based on gray gas assumption
- Radiative heat flux
- Optically thin model (OTM)
- Discrete ordinate method (DOM)
- RTE solved in n discrete directions (ordinates)
- Sn approx. ? number of equations n(n2)/2 (2-D)
- S2 4 eqs., and S4 12 eqs.
- Discrete transfer method (DTM)
- RTE solved for n rays (ray-tracing)
20Performance of DOM/DTM
- DOM is found to be overall superior for the
desired accuracy.
Relative error
21Soot Model (Two Equation Model)
- A semi-empirical two-equation model based on a
flamelet approach (Young and Moss, 1995) - Soot number density
- Soot volume fraction
22Computational Configuration
- Calculation procedure
- Generate 1-D diffusion flame profile (Oppdif)
- Establish steady diffusion flame in counterflow
- Superimpose initial vortex pairs
- Velocity profile for a vortex
23Parameters
- Three different vortex strength cases
- Weak vortex flame and soot are not extinguished
- Medium vortex extinguishes soot only
- Strong vortex extinguishes both flame and soot
24Weak vs. Strong Vortex Cases
Temperature
Nsoot
fv
Vorticity
Case A
Case B
Case C
25Integrated Nsoot and fv (Case B)
Volume-integrated Nsoot and flame volume
Volume-integrated fv in different temperature
regions
- Soot number density depends strongly on the
high-temperature flame volume - Soot volume fraction increases by surface growth
at low temperature, fuel-rich regions
26Effects of the Vortex Strength
Comparison of integrated fv for Cases A-C
Comparison of integrated Nsoot for Cases A-C
- As vortex strength increases, more soot particles
are convected into fuel rich zone - Case A fv is more directly affected by the soot
nucleation. - Case C fv does not change much even the the soot
nucleation (Nsoot) is turned off.
27Comparison of Radiation Models
- Radiative heat loss
- During transient period, OTM overpredicts the
radiative heat loss by up to a factor of two
compared to DOM - Fidelity of radiation model is important in DNS
Total radiative heat loss with OTM and DOM for
Case B
28Ongoing/Future Work
- Terascale Computing 3D Turbulent Nonpremixed
Counterflow - Flames with Radiation, Soot, and Water Spray
- Integration of all the developed physical
submodels - Test bench for numerical algorithms boundary
conditions, acoustic speed reduction (ASR) - Science issue partial/total extinction and
pollutant formation due to water spray
interaction - Further To-Do List
- Computational Development
- Immersed boundary method
- Adaptive mesh refinement
- Chemistry reduction strategies
- Physical Models
- Detailed soot model
- Radiation model (spectral)
- Catalytic surface reaction
DOE INCITE Project 3D DNS of turbulent
nonpremixed jet flame, J. H. Chen et al. Sandia
National Labs
- Enabling Technologies
- Data-mining and visualization
- Object-oriented code architecture for efficient
management
29Acknowledgments
- SciDAC TSTC Program
- Hong G. Im (Michigan)
- Chunsang Yoo, Ramanan Sankaran (SNL)
- Christopher J. Rutland (Wisconsin)
- Yunliang Wang
- Arnaud Trouvé (Maryland)
- Yi Wang
- Jacqueline H. Chen (Sandia National Laboratories)
- Scott Mason, Chris Kennedy, James Sutherland,
Evatt Hawkes - Pittsburgh Supercomputing Center
- Ravishankar Subramanya, Raghurama Reddy
- DOE Computing Resources
- National Energy Research Scientific Computing
Center - Oak Ridge National Laboratory
- Pacific Northwest National Laboratory
- University of Oregon (the Tau Project)
- Sameer Shende, Allen Malony