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Compressible flow-Aerothermodynamics

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Hypersonic, High temperature gas flows, Aerothermodynamics By NASA
44
Hypersonic Educational Initiative Introduction to 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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Page 1: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Introduction toHypersonic Aerothermodynamics

Iain D. BoydDept. Aerospace Eng.University of Michigan

Ann Arbor, MI

Graham V. CandlerDept. Aerospace Eng. & Mech.

University of MinnesotaMinneapolis, MN

Page 2: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

1. Hypersonic Gas Dynamics

1.1 Introduction and ExamplesOutline (1)

1. Hypersonic Gas Dynamics (1.5 hours)1.1 Introduction and Examples1.2 Post-shock conditions: perfect gas vs. equilibrium gas

Iteration approach for post-shock conditionsExamples

1.3 Reacting gas effects:Finite-rate reactions – nonequilibrium vs. equilibriumIonizationRadiation

1.4 Transport phenomena

Page 3: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Outline (2)

2. Hypersonic Aerodynamics: Pressure (1.0 hours)2.1 Exact and approximate equilibrium gas solutions:

Stagnation pointsCones and wedges

2.2 Mach number independence2.3 Newtonian and Modified Newtonian aerodynamics2.4 Examples

Page 4: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Outline (3)

3. Hypersonic Aerothermodynamics: Heat Transfer (1.0 hours)3.1 Introduction:

role of aerodynamic heatinghypersonic boundary layers

3.2 Boundary layer equations, Lees-Dorodnitsyn transformation3.3 Flat plate / wedge / cone solutions3.4 Stagnation point solution3.5 Transition to turbulence3.6 Wall catalysis3.7 Examples

Page 5: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Outline (4)

4. Viscous Interactions (1.0 hours)4.1 Leading edge interactions4.2 Effect on high-altitude L/D; scaling for vehicles4.3 Shock-BL interactions, shock-shock interactions

5. Thermal Protection Systems (1.0 hours)5.1 Passive:

re-radiative cooling, equilibrium wall boundary conditionrole of wall temperature, material propertiesexamples

5.2 AblativeSurface ablatorsPyrolyzing ablators

Page 6: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Outline (5)

6. Aerothermodynamics of Hypersonic Vehicles (1.0 hours)Ballistic entryLifting capsule re-entry: ApolloHigh-lift re-entry: ShuttleAerocapture / AerobrakingAirbreathing scramjets

Page 7: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

What is Hypersonic Flow?

• Hypersonic aerothermodynamic phenomena:– strong shock waves with high temperature– not calorifically perfect (variable γ)– 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

Page 8: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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

Page 9: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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

Page 10: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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

Page 11: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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)

Page 12: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

• 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 VehicleHistorical Overview

Page 13: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Some CurrentHypersonic Programs

Falcon (DARPA)

Orion(NASA)X51

(AFRL)

HyBoLT (NASA/ATK)

Page 14: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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

Page 15: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

• 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 (γ=const)

Re-entry Trajectories

• Trajectory equations for Earth centered system:

WD

LT, U

γ

!

U ˙ "

g=L

W# 1#

U2

gR

$

% &

'

( ) cos(" )

!

T

W"

˙ U

g=

D

W+ sin(# )

Page 16: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

• 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, γ~0 (shallow entry)

Re-entry Trajectories

!

1

2"U

2

Page 17: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Flight Velocity

Page 18: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Stagnation Point Heating

Page 19: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Stagnation PointTemperature

Page 20: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Deceleration Levels

Page 21: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

1.2 Post-Shock Conditions

• Perfect-gas shock relations:

• Density ratio asymptotes to:

• Pressure and temperature are quadratic in M

– Makes sense: energy is conserved

Page 22: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Post-Shock Conditions

• Post-Shock Temperature:

Temperatures rapidlybecome huge!

Page 23: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Post-Shock Conditions

• Variation of air internal energy with T:

10% departure fromcalorically perfect gasequation of state =onset of hypersonic flow

Page 24: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Post-Shock Conditions

• More fundamentally – 1D gas dynamics:

• Plus equations of state:

• No exact solutions

Thermally perfect,calorically imperfect

General equilibriumgas mixture

Page 25: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Post-Shock Conditions

• Hypersonic limit:

• Note that post-shock enthalpy and pressure onlydepend on upstream conditions in hypersonic limit.

Can solve for thethermodynamic state

Page 26: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Post-Shock Conditions

• Iterative solution to shock relations:

• Guess a value of ε = εi and iterate:

Use tables, NASA CEA, etc.

Page 27: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Equilibrium Air

Temperature (K) Z = Compressibility

Page 28: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Post-Shock Conditions

• Example: M = 12 at 30 km altitude:

Imperfect Perfect

Page 29: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Post-Shock Conditions

• Perfect-gas vs. equilibrium post-shock conditions:

Difference is due toenergy storage ininternal energymodes + chemistry

Page 30: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Post-Shock Conditions

• Post-shock pressure has weak dependence on non-ideal gas effects (just through (1- ε))

• Post-shock temperature and density have strong Machnumber (free-stream speed) dependence– Density ratio > (γ + 1)/(γ - 1) = 6– Temperature decreases significantly

• Concept of γ no longer has much meaning; if:

• Matlab code: ftp://ftp.aem.umn.edu/users/candler/HEI/mollier.m

Page 31: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

1.3 Reacting Gas Effects

• Analysis of Earth hypersonic vehicles at U<8km/s:– 5-species air model sufficient: N2, O2, NO, N, O

• Reactions:– Dissociation-recombination:

– Zeldovich exchange:!

N2

+ M" N + N + M

!

N2

+O" NO+ N

!

NO+O"O2

+ N!

O2

+ M"O+O+ M

!

NO+ M" N +O+ M

Page 32: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Finite Rate of Reactions

• For illustration, consider:– 2-species: N2, N

• Each reaction proceeds at a finite rate:

• Forward rate coefficients measured experimentally, kf (T)

• Backward rate coefficients from equilibrium constant:

partition functions Q from quantum+statistical mechanics

!

N2

+ M" N + N + M

!

N2

+ N2"kb1

k f 1

N + N + N2

!

N2

+ N"kb 2

k f 2

N + N + N

!

Ke =k f

kb="Qproducts

"Qreactants

Page 33: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Finite Rate of Reactions

• 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:

– α=mass fraction, m=atom mass, ρ=density, V=volume,θd=dissociation temperature

!

d[N2]

dt= "k f 1[N2

][N2]" k f 2[N2

][N]+ kb1[N][N][N2]+ kb2[N][N][N]

!

" 2

1#"=m

$V

QN

2

QN2

exp(#%d /T)

Page 34: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Finite Rate of Reactions

• Chemical equilibrium:– O2 dissociates before N2 (has lower θd)– fewer atoms at high pressure (more recombination)

Page 35: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Finite Rate of Reactions• Chemical nonequilibrium:

– equilibrium end state reached only after finite time– in a flow field, this translates as finite distance

Page 36: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Nonequilibrium

• Impact of chemical nonequilibrium:– chemical composition mainly affects energy of flow

• exothermic reactions consume energy• catalysis: fraction of atoms reaching the vehicle

surface may recombine releasing heat– scaling:

• nonequilibrium flow occurs at lower densityand/or smaller body length scales

!

large Kn "#$L%

1

&$L

!

small Re "#$U$L

µ$

Page 37: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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:

!

N2

+ M" N + N + M

!

N2

+O" NO+ N

!

N + N" N2

++ e

#

!

N + e"# N

++ e

"+ e

"

Page 38: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Ionization

• Equilibrium solution (Saha) for [N, N+, e-] system:

– φ=ion mole fraction,– C=constant,– p=pressure,– θi=ionization temperature

!

" 2

1#" 2= C

T5 / 2

pexp(#$i /T)

Page 39: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Ionization• Significance:

– plasma causes communications blackout– highly catalytic ions are source of heating

Page 40: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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

"

!

˙ q rad "RNU8.5#1.6

Page 41: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

1.4 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):κ = thermal conductivity coefficient

!

JA = "#DAB

dCA

dy

!

" = µdu

dy

!

q = "#dT

dy

Page 42: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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)

Page 43: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

Viscosity

• Affects momentum and energy equations

• Influences surface shear stress

• Coefficient evaluation:– for simple gas

– various mixing rules

– are viscosity collision integrals!

µi=5

16

"mikT

"#ii

(2,2)

!

µ = µ("ij

(1,1),"ij

(2,2))

!

"ij

(2,2)

Page 44: Compressible flow-Aerothermodynamics

Hypersonic Educational Initiative

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

Mi

Cv

+9

4Ru

%

& '

(

) *

!

" ="(#ij

(1,1),#ij

(2,2))

!

"ij

(2,2)


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