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8/17/2019 Chp 1 Hypersonics
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Hypersonic Educational Initiative
Advanced
Hypersonic Aerothermodynamics
Iain D. Boyd
Dept. Aerospace Eng.
University of Michigan
Ann Arbor, MI
Graham V. Candler
Dept. Aerospace Eng. & Mech.
University of Minnesota
Minneapolis, MN
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1. Hypersonic Gas Dynamics
1.1 Introduction
Outline (1)
1. Hypersonic Gas Dynamics (4.0 hours)1.1 Introduction and Examples
Vehicle trajectories and properties
1.2 Hypersonic gas dynamic processes
Shock waves / boundary layers wakes
1.3 Fundamental equations of gas dynamicsBoltzmann / Euler / Navier-Stokes Equations
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Outline (2)
1. Hypersonic Gas Dynamics (4.0 hours)1.4 Real gas effects:
Quantum mechanics + statistical mechanics
Perfect gasVibrational activation
Chemical reactions – nonequilibrium vs. equilibrium
Ionization, radiation
1.5 Shock wave analysis
Perfect gasIterative approach for equilibrium gas
1.6 Transport phenomena
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Outline (3)
2. Hypersonic Aerodynamics: Pressure (1.0 hour)
2.1 Exact and approximate equilibrium gas solutions:
Stagnation points
Cones and wedges2.2 Mach number independence
2.3 Newtonian and Modified Newtonian aerodynamics
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Outline (4)
3. Hypersonic Aerothermodynamics: Heat Transfer
(2.0 hours)
3.1 Introduction:
role of aerodynamic heating
hypersonic boundary layers
3.2 Boundary layer equations, similarity transformation
3.3 Flat plate / wedge / cone solutions
3.4 Stagnation point solution and scaling
3.5 Laminar and turbulent boundary layers; transition
3.6 Wall catalysis
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Outline (5)
4. Viscous Interactions (1.0 hour)
4.1 Leading edge interactions
4.2 Effect on high-altitude L/D; scaling for vehicles
4.3 Shock-BL interactions, shock-shock interactions
5. Thermal Protection Systems (1.5 hours)
5.1 Passive:
Re-radiative cooling, equilibrium wall boundary condition
Role of wall temperature, material properties5.2 Ablative
Surface ablators
Pyrolyzing ablators
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Outline (6)
6. Computational Analysis (2.0 hours)6.1 Continuum CFD methods
Requirements for aeroheating predictions
Approaches for real gas effects
Current code capabilities6.2 Non-continuum method - DSMC
7. Experimental Testing (1.0 hour)7.1 Types of facilities:
Blow-down tunnelsVitiated-air facilities
Impulse facilities
7.2 Overview of measurement techniques
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Outline (7)
8. Aerothermodynamics of Hypersonic Vehicles(1.5 hours)
Ballistic entry
Lifting capsule re-entry: Apollo
High-lift re-entry: Shuttle Aerocapture / Aerobraking
Airbreathing scramjets
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What is Hypersonic Flow?
• Hypersonic aerothermodynamic phenomena: – strong shock waves with high temperature
– not calorifically perfect (variable !)
– chemical reactions
– significant surface heat flux – several different types of vehicles:
• missiles, space planes, capsules, air-breathers
• Working definition of hypersonic flow:
M = (U / a) >> 1
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Hypersonic Examples:
I. Missiles
• Mission: high-speed delivery of explosives• Aerodynamics: slender body with blunt nose
• Propulsion: rockets, ramjets
• Examples: AMRV, SCUD, Patriot, Hy-Fly
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Hypersonic Examples:
II. Space Planes
• Mission: orbital re-entry• Aerodynamics: gliders with thermal protection
• Propulsion: none (except small control thrusters)
• Examples: Space Shuttle, Buran, Hermes
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Hypersonic Examples:
III. Air-breathing Systems
• Missions: launch, cruise, orbital re-entry
• Aerodynamics: slender with integrated engines
• Propulsion: ram/scram-jets, rockets, turbojets
• Examples: X-15, NASP, X-43, X-51
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Hypersonic Examples:
IV. Planetary Entry
• Missions: EDL, aero-braking, aero-capture• Aerodynamics: very blunt, thick heat shield
• Propulsion: none (sometimes RCS)
• Examples: Apollo, MSL, CEV (Orion)
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• Flight vehicles:
– WAC Corporal missile (1949, M~8)
– Vostok I (1961, M~25)
– X-15 (1963-1967, M~7)
– Space Shuttle (1981-???, M~25)
– HyShot (2002, M~8)
– X43 (2004, M>7)
– Hy-CAUSE (2007)
• Recent programs without flight:
– NASP, Hermes, AFE, AOTV (1990)
– VentureStar-X33 (2000)
Hypersonic Vehicle
Historical Overview
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Some Current
Hypersonic Programs
Falcon (DARPA)
Orion
(NASA)
X51
(AFRL)
HyBoLT (NASA/ATK)
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Hypersonic Tales of Woe
• Hypersonics produces unexpected phenomena
• X15 test flight with dummy scramjet installed:
– unexpected shock interactions generated
– burned holes in connection pylon
• First re-entry of Space Shuttle (STS-1):
– larger than expected nose-up pitch generated
– required near-maximum deflection of body flap
• Shock-shock interactions:
– heating amplified significantly
– leading edges, cowl lips,
engine flow paths
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• Ballistic missiles:
– mission: short flight, fast impact
– rocket launch, ballistic entry – no thrust or lift during entry (T=0, L=0)
– fixed flight path at large angle (!=const)
Re-entry Trajectories
• Trajectory equations for Earth centered system:
W
D
LT, U
!
U ̇"
g=
L
W # 1#
U 2
gR
$
% &
'
( ) cos(" )
T W
"
˙Ug= DW
+ sin(# )
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• Air-breathing vehicle:
– missions: cruise, orbital return
– completely reusable
– powered take-off and entry
– constant for engine efficiency
• Space Shuttle:
– mission: orbital return
– rocket launch
– equilibrium glide entry – no thrust, L/D~1, !~0 (shallow entry)
Re-entry Trajectories
1
2" U
2
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Flight Velocity
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Stagnation Point Heating
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Stagnation Point
Temperature
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Deceleration Levels
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1.2 Hypersonic Gas Dynamics
• Goal of hypersonic gas dynamics analysis:
– predict flow field around a hypersonic vehicle
– predict properties on vehicle surface (pressure,
shear stress, heat transfer)
– hence predict aerodynamic and thermal
performance of a vehicle
• Three main gas dynamic flow phenomena:
– shock waves
– boundary layers
– wakes
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• Formed when an object is placed in supersonic flow:
– Mach number M = U / a (a~330 m/s at STP)
– supersonic: M > 1
• A shock wave is an extremely thin layer of fluid acrosswhich there are significant changes in properties:
– at STP, thickness ~ 10-7 m
– T, p, ! all increase; M, U decrease
– variable-! = compressible; high-T=real gas
• Several different types:
– normal (strongest), oblique, bow
1.2.1 Shock Waves
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• Thin fluid layer formed next to vehicle surface:
– created by friction between gas and wall
• Boundary layer (BL) determines surface properties:
– pressure (nearly constant across BL) – shear stress and heat transfer
– flow separation
• Different types with very different properties:
– laminar
– turbulent
– transition between the two
1.2.2 Boundary Layers
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• Region of flow in the rear of the vehicle:
– smaller influence on aerothermodynamics
• Often involves strong expansion processes:
– T, p, ! all decrease; M, U increase
• Recompression:
– leads to increased heating on a capsule backshell
– base pressure effects on missiles
– flow may become turbulent
– complex vortex dynamics
1.2.3 Wakes
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1.3.1 Boltzmann Equation
• Consider gas flow at the molecular level:
– molecule has position x, velocity C
– enormous volume of information (at STP, there
is about 1026 air molecules per cubic meter)
– adopt a statistical approach
– velocity distribution function, VDF:
f(t, x, C) dx dC
– probability of finding a particle at time t, in
physical space element dx, and in velocityspace element dC
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1d VDF’s
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• VDF is affected by:
– particle transport across dx due to C
– particle transport across dC due to a
– scattering in/out of dC due to molecular collisions
• Leads to the Boltzmann Equation:
– n=number density,a
=acceleration (force), g=relativevelocity, !=collision cross section, "=solid angle,
C’=particle velocity after collision, Z=velocity of
particle with which C-particle collides
" (nf )
" t +C #
" (nf )
" x+ a #
" (nf )
" C= n
2{ f (C') f (Z') $ f (C) f (Z)}g% d &dZ ''
1.3.1 Boltzmann Equation
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• Equilibrium solution:
– no net change in VDF, f , requires LHS = RHS = 0
– RHS = 0 satisfied by
– thus, log[f] is a linear combination of collision
invariants (mass, momentum, energy)
– leads to Maxwellian (equilibrium) VDF
f (C) f (Z) = f (C') f (Z')
1.3.1 Boltzmann Equation
log[ f (C)]+ log[ f (Z)]= log[ f (C')]+ log[ f (Z')]
f (C)d C =m
2" kt
#
$ %
&
' ( 3 / 2
exp ) m
2kT C 1 ) u1( )
2+ C 2 ) u2( )
2+ C 3 ) u3( )
2( )*
+ , -
. / d C
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• Very difficult to obtain solutions:
– seven-dimensional space
– non-linear collision integral on RHS
– expensive computations required
• Solution only required for strongly nonequilibrium flow:
– Knudsen number: Kn = # / L
– at Kn < 0.01, f is close to Maxwellian
– for L=1 m, Kn~0.01 at h=90 km in atmosphere
– for small Kn, Boltzmann equation can be used to
derive sets of macroscopic transport equations
1.3.1 Boltzmann Equation
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• Take moments of Boltzmann Eq (Maxwell):
– Q=Q(C) is a particle property, e.g. momentum mC
– $[Q]=rate of change of Q due to collisions
–
• Assumptions for f , Q lead to sets of partial differential
equations describing macroscopic flow
1.3.2 Method of Moments
" n Q
" t +
" n CQ
" x= # Q[ ]
Q = Qf (C )dC "
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• Assumptions:
– local thermodynamic equilibrium
– VDF’s are Maxwellian everywhere
– use Q=m, mC, 0.5mC2 for which $[Q]=0
– leads to 5 PDE’s: the Euler equations
– no viscosity, no thermal conductivity
1.3.2 Euler Equations
"#
" t +
"# u
" x= 0
"# u
" t +
"# CC
" x= 0 = #
" u
" t + # u $ %u+% p
" 0.5
# C
2
" t + "
0.5# C
C
2
" x= 0 = 3
2
" p" t
+ 32$ % pu+ p$ % u
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• Chapman-Enskog distribution:
– VDF is small perturbation from equilibrium
– where %(C)=1+F(Kn)=1+F(heat flux, shear stress)
• Navier-Stokes equations from transfer equation:
– same five relations as Euler Equations
– also: Q=mCiC j, mCiC jCk (15 further relations)
– replace heat flux tensor by heat flux vector
– derive and substitute linear transport relations
1.3.3 Navier-Stokes Eqns.
f (C)d C = "(C) f M (C)d C
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• Again, a set of five PDE’s:
1.3.3 Navier-Stokes Eqns.
"
" t U+
"
" xF +
"
" yG +
"
" zH = 0
U =
"
" u
" v
" w
" E
#
$
% % %
&
% % %
'
(
% % %
)
% % %
F =
" u
" u2+ p# $
xx
" uv # $ xy" uw # $ xz
" E + p# $ xx( )u # $ xyv # $ xzw + q x
%
&
' ' '
(
' ' '
)
*
' ' '
+
' ' '
G =
" v
" uv # $ yx
" v2+ p# $ yy
" vw # $ yz
" E + p# $ yy( )v # $ yxv # $ yzw + q y
%
&
'
' '
(
' ' '
)
*
'
' '
+
' ' '
H =
" w
" uw # $ zx" vw # $
zy
" w2+ p # $ zz
" E + p# $ zz( )w # $ zxu # $ zyv + q z
%
&
'
' '
(
' ' '
)
*
'
' '
+
' ' '
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• Stress tensor modeled using Stokes’ hypothesisfor Newtonian fluid:
–
µ = viscosity coefficient
• Heat flux vector modeled using Fourier’s Law:
– ! = coefficient of thermal conductivity
1.3.3 Navier-Stokes Eqns.
" xx
= 2µ # u
# x $ 1
3% &u
'
( ) *
+ , " xy
= " yx
= µ # u
# y+
# v
# x
$
% &
'
( )
q x = "# $ T
$ x
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1.4 Real Gas Effects
• In low-speed flows, air is a perfect gas:
– simplified thermodynamics, no chemistry
• In most hypersonic flows, air is a real gas:
– mainly due to high temperatures – complex thermodynamics, chemical reactions
• Requires us to consider:
– quantum+statistical mechanics
– vibrational activation, chemistry – equilibrium and finite rate processes
– ionization and radiation
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1.4.1 Quantum Mechanics
• An atom / molecule has several energy modes:
– translation (due to 3D motion)
– rotation (gyration of atoms in a molecule)
– vibration (oscillation of atoms in a molecule)
– electronic (arrangement of electrons in orbits)
• Quantum mechanics provides energy states:
– solution of Schrodinger equation
– separate analysis for each energy mode – each atom / molecule may only occupy certain
quantized energy states in each energy mode
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1.4.1 Quantum Mechanics
• Translational energy:
– h=Planck’s constant, L=dimension, m=mass
– n1, n2, n3 are translational quantum numbers
– !"t ~10-38 J so continuum can be assumed
• Rotational energy (rigid rotor):
– k=Boltzmann const, #r =char. temp. for rotation – J=rotational quantum number
– for air, !"r ~10-23 J so continuum OK
" t =
h2
8mL2 n
1
2+ n
2
2+ n
3
2( )
" r= k #
r $ J ( J +1)
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1.4.2 Statistical Mechanics
• Each atom / molecule has an enormous number of
possible energy levels:
– degenerate energy states for each energy level
• Large number of atoms/molecules in a gas: – huge volume of information
• Statistical mechanics:
– distributions of particles across energy states
– macroscopic thermodynamics viaintegration/summation of atomic/molecular
behavior
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1.4.2 Statistical Mechanics
• Boltzmann energy distribution:
– gi=degeneracy of energy level i
– summation in denominator is partition function, Q
• Overall partition function:
(diatomic)
f (" i) =gi exp #" i /kT ( )gi exp #" i /kT ( )$
Qt =V 2" mkT
h2
#
$ %
&
' (
3 / 2
Qr=
T
" r
Qv =
1
1" exp "# v /T ( )
Qe = g0 + g1exp "# 1 /T ( ) $ g0
Q = Qt "Q
r "Q
v "Q
e
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1.4.2 Statistical Mechanics
• Internal energy (thermodynamics):
• Specific heats:
cv=
" e
" T
#
$ %
&
' ( v
=
3 R
2+ R + R
) v /2T
sinh() v /2T )
*
+ ,
-
. /
2
et =
3 RT
2
er= RT
ev=
R" v
exp " v /T ( )#1
ee " 0
e = et + e
r + e
v+ e
e
c p = cv + R
" =c
p
cv
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1.4.2 Statistical Mechanics
• Specific heats (non-reacting):
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1.4.3 Perfect Gas
• Assumption often invoked in hypersonics:
– no vibrational activation, no chemistry
– cp, cv, $ are all constants
• For air:
p=
" RT
e=
c vT
h=
c pT
c p=
7 R
2
" =7
5
cv=
5 R
2
c p=
" R
" #1
cv=
R
" #1
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• At high temperatures (T>1,000K) air molecules
become vibrationally activated:
– equilibrium (infinite rate) results provided by
quantum mechanics + statistical mechanics
– finite rate activation modeled using
– where e*v=equilibrium value at temperature T
– %v=vibrational relaxation time (Millikan & White)
dev
dt =
ev
*(T ) " e
v
# v
1.4.4 Vibrational Activation
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• Analysis of Earth hypersonic vehicles at U
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Rate Processes
• For illustration, consider:
– 2-species: N2, N
• Each reaction proceeds at a finite rate:
• Forward rate coefficients measured experimentally, k f (T)
• Backward rate coefficients from equilibrium constant:
partition functions Q from quantum+statistical mechanics
N 2+ M " N + N + M
N 2 + N 2"k b1
k f 1
N + N + N 2
N 2 + N "k b 2
k f 2
N + N + N
K e =k f
k b=
"Qproducts
"Qreactants
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Rates of Change
• Net rate of change in concentration of a species:
– contributions from forward and backward directions
• Chemical equilibrium: – final state reached instantaneously
– production of each species balanced by its destruction
– analytical solution for our system:
– &=mass fraction, m=atom mass, '=density, V=volume,
#d=dissociation temperature
d [ N 2]
dt = "k f 1[ N 2][ N 2]" k f 2[ N 2][ N ]+ k b1[ N ][ N ][ N 2]+ k b2[ N ][ N ][ N ]
"
2
1#" = m$ V
Q N 2
Q N 2exp(#% d /T )
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Infinite Rate of Reactions
• Chemical equilibrium:
– O2 dissociates before N2 (has lower #d)
– fewer atoms at high pressure (more recombination)
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Finite Rate of Reactions
• Chemical nonequilibrium: – equilibrium end state reached only after finite time
– in a flow field, this translates as finite distance
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Nonequilibrium
• Impact of chemical nonequilibrium:
– chemical composition mainly affects energy of flow
• endothermic reactions consume energy
• catalysis: fraction of atoms reaching the vehicle
surface may recombine releasing heat – scaling:
• nonequilibrium flow occurs at lower density
and/or smaller body length scales
large Kn " # $ L%
1
& $ L
small Re " #
$U $ L
µ $
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Ionization
• Very high temperature reacting air (U>8km/s): – N2, O2, NO, N, O, N2+, O2+, NO+, N+, O+, e-
• Reactions:
– dissociation-recombination:
– exchange:
– associative Ionization:
– direct Ionization:
N 2 + M " N + N + M
N 2+O" NO+ N
N + N " N 2
+
+ e#
N + e"# N
+
+ e"+ e
"
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Ionization
• Equilibrium solution (Saha) for [N, N+, e-] system:
– (=ion mole fraction,
– C=constant, – p=pressure,
– #i=ionization
temperature
" 2
1#" 2= C
T 5 / 2
pexp(#$ i /T )
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Radiation
• Another important process at high temperature: – activation-deactivation:
– spontaneous emission:
– analysis is complex, no closed form expressions – research area, e.g. NEQAIR (NASA-ARC)
• Radiative heating important at U>12km/s:
– e.g. stagnation point heating correlation (Martin)
– also proportional to shock layer thickness
– Stardust: radiation provides 10% of total heating
N *" N + h#
N + e"# N
*+ e
"
q̇rad " R N U 8.5
# 1.6
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1.5 Post-Shock Conditions
• Perfect-gas shock relations:
• Density ratio asymptotes to:
• Pressure and temperature are quadratic in M
– Makes sense: energy is conserved
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Post-Shock Conditions
• Post-Shock Temperature:
Temperatures rapidly
become huge!
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Post-Shock Conditions
• Variation of air internal energy with T:
10% departure from
calorically perfect gas
equation of state =
onset of hypersonic flow
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Post-Shock Conditions
• More fundamentally – 1D gas dynamics:
• Plus equations of state:
• No exact solutions
Thermally perfect,
calorically imperfect
General equilibrium
gas mixture
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Post-Shock Conditions
• Hypersonic limit:
• Note that post-shock enthalpy and pressure only
depend on upstream conditions in hypersonic limit.
Can solve for the
thermodynamic state
!
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Post-Shock Conditions
• Iterative solution to shock relations:
• Guess a value of ! = !i and iterate:
Use tables, NASA CEA, etc.
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Equilibrium Air
Temperature (K) Z = Compressibility
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Post-Shock Conditions
• Example: M = 12 at 30 km altitude:
Imperfect Perfect
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Post-Shock Conditions
• Perfect-gas vs. equilibrium post-shock conditions:
Difference is due to
energy storage ininternal energy
modes + chemistry
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Post-Shock Conditions
• Post-shock pressure has weak dependence on non-ideal gas effects (just through (1- !))
• Post-shock temperature and density have strong Mach
number (free-stream speed) dependence
– Density ratio > (" + 1)/(" - 1) = 6 – Temperature decreases significantly
• Concept of " no longer has much meaning; if:
• Matlab code:
ftp://ftp.aem.umn.edu/users/candler/HEI/mollier.m
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1.6 Transport Phenomena
• Generated by gradients in flow properties:
– diffusion (Fick’s Law):
DAB
=diffusion coefficient
– viscosity (Newtonian fluid):
µ = viscosity coefficient
– thermal conduction (Fourier’s Law):
! = thermal conductivity coefficient
J A = "# D ABdC A
dy
" = µ du
dy
q = "# dT
dy
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Diffusion
• Affects continuity and energy equations
• Influences transport of species to surface
• Coefficient evaluation:
– for simple gas (self diffusion)
– for gas mixture
– are diffusion collision integrals
– averaged binary coefficient D1m often used
Dii =3
8"
# mikT
# $ii
(1,1)
Dij "kT
p
(mi + m j )kT
mim j
1
# $ij (1,1)
"ij (1,1)
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Diffusion
Depends on temperature, pressure, species
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Viscosity
• Affects momentum and energy equations
• Influences surface shear stress
• Coefficient evaluation:
– for simple gas
– various mixing rules
– are viscosity collision integrals
µ i =5
16
" mikT
" #ii
(2,2)
µ = µ ("ij (1,1)
,"ij (2,2)
)
"ij (2,2)
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Viscosity
• Sutherland law kg/m/s
– depends on pressure at high T due to chemistry
µ air =1.458"10#6 T
1.5
T +110.4
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Thermal Conductivity
• Affects energy equations
• Influences surface convective heat flux
• Coefficient evaluation:
– for simple gas (Eucken)
– various mixing rules
– are again viscosity collision integrals – curve fits for collision integrals from the literature
" i
=
5
16
# mikT
# $ii(2,2)1
M i
cv
+
9
4 R
u
%
& '
(
) *
" =" (#ij (1,1)
,#ij (2,2)
)
"ij (2,2)
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Thermal Conductivity
• Sutherland law W/m/K
– complex behavior due to chemistry
" air =1.993#10$3 T
1.5
T +112
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Prandtl Number
• Often used to evaluate thermal conductivity:
• Eucken’s relation:
– monatomic gas: Pr=0.67
– diatomic gas ("=1.4): Pr=0.737
Pr =c
pµ
"
Pr =4"
9" # 5
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Prandtl Number
• Real gas:
– again, complex behavior due to chemistry