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Aerothermodynamics of high speed flowsAERO 0033–1
Lecture 2: Flow with discontinuities, normal shocks
Thierry Magin, Greg Dimitriadis, and Johan [email protected]
Aeronautics and Aerospace Departmentvon Karman Institute for Fluid Dynamics
Aerospace and Mechanical Engineering DepartmentFaculty of Applied Sciences, University of Liege
Room B52 +1/443Wednesday 9am – 12:00pm
February – May 2017
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 1 / 34
Outline
1 Introduction: high-temperature gas dynamics
2 Flows with discontinuitiesExamplesRankine-Hugoniot jump relations
3 Normal shocks
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 2 / 34
von Karman Institute for Fluid Dynamics
“With the advent of jet propulsion, it became necessary to broaden the field of
aerodynamics to include problems which before were treated mostly by physical
chemists. . .”
Theodore Karman, 1958
“Aerothermochemistry” was coined by von Karman in the 1950s to denote this
multidisciplinary field of study shown to be pertinent to the then emerging aerospace era
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 3 / 34
AERO 0033–1 (30h Th +30h Pr – 5 ECTS)
) Course contents – This course introduces the students to theaerothermodynamic analysis of high speed flows. Two main subjectsare addressed:
Transonic and supersonic aerodynamicsHigh-temperature gas dynamics (today’s introduction)
The lecture notes are available online in the form of presentations
Supplementary textbooksJ. D. Anderson, Modern Compressible Flow: With HistoricalPerspective, McGraw-Hill, 2002P. A. Thompson, Compressible-fluid Dynamics, Advanced engineeringseries, 1988A. H. Shapiro, The dynamics and thermodynamics of fluid flow, TheRonald Press Company, New York, 1953
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 4 / 34
Some additional references
J. D. Anderson, Hypersonic and high-temperature gas dynamics,American Institute of Aeronautics and Astronautics, 2006
M. Mitchner, C. H. Kruger, Partially ionized gases, Wiley, 1973
G. Vincenti, C. H. Kruger, Introduction to physical gas dynamics,Wiley, 1965
L. C. Woods, The thermodynamics of fluid systems, OxfordUniversity Press, 1975
D. A. McQuarrie and J. D Simon, Physical chemistry, a molecularapproach, University Science Books, 1997
G. A. Bird, Molecular Gas Dynamics and the Direct Simulation ofGas Flows, Oxford University Press, 1994
T. E. Magin, Physical Gas Dynamics, von Karman Institute for FluidDynamics, 2012
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 5 / 34
Introduction: high-temperature gas dynamics
Outline
1 Introduction: high-temperature gas dynamics
2 Flows with discontinuities
3 Normal shocks
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 5 / 34
Introduction: high-temperature gas dynamics
Design of spacecraft heat shields requires the developmentof integrated codes for flow/radiation/material coupling
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 6 / 34
Introduction: high-temperature gas dynamics
Motivation: new challenges for aerospace science
Design of spacecraft heat shieldsModeling of the convective and radiative heat fluxes for:
Robotic missions aiming at bringing back samples to EarthManned exploration program to the Moon and Mars
Intermediate eXperimental Vehicle of ESA Ballute aerocapture concept of NASA
Hypersonic cruise vehicles and ballutesModeling of flows from continuum to rarefied conditions for the nextgeneration of air breathing hypersonic vehicles and Entry Descent andLanding (EDL) technologies such as ballutes
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 7 / 34
Introduction: high-temperature gas dynamics
Motivation: new challenges for aerospace science
Electric propulsion (EP)Today, 20% of active satellites operate with EP systems
STO-VKI Lecture Series Electric Propulsion Systems: from recent research developments to industrial
space applications
EP system for ESA’s gravity mission GOCE ⇠20,000 space debris > 10cm
Space debrisSpace debris, a threat for satellite and space systems and for mankindwhen undestroyed debris impact the Earth
STO-VKI Lecture Series Space Debris, In Orbit Demonstration, Debris Mitigation
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 8 / 34
Introduction: high-temperature gas dynamics
Motivation: engineering design in hypersonics
Blast capsule flow simulation
COOLFluiD platform and Mutation library
Relevant quantities for engineers:Heat flux &Shear stress to the vehicle surface
) Complex multiphysics problemChemical nonequilibrium (gas)
Dissociation, ionization, . . .Internal energy excitation
Thermal nonequilibriumTranslational and internal energyrelaxation
Gas / surface interactionRadiationTurbulence (laminar-turbulenttransition)Rarefied gas e↵ects
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 9 / 34
Introduction: high-temperature gas dynamics
Example of aerospace mission killerInaccurate heat-flux predictions can be fatal for the crew / success ofa robotic missione.g. Lessons learned from Galileo’s entry into the Jovian atmosphere:
Stagnation point material recession ofheatshield was less than predicted
Ablation at frustrum and shoulder wasmuch higher than predicted
e.g. New carbon / resin composites require improved models
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 10 / 34
Introduction: high-temperature gas dynamics
Gas-surface interaction: complex multiphysics problem
chemical(species((diffusion(
surface(recession(
virgin(material(
pyrolysis((zone(
porous(char(
hot(radia7ng(gas(
boundary(layer(
convec7ve((heat(flux(
radia7on(flux((
shock(heated(gas((T(~(10,000K)(
heat(transfer(
mechanical(erosion(
pyrolysis(gases(
reac7on(products(
OH( OH(
Radiative and convectiveheating
) Pyrolysis of phenolic resinC6H5 �OH (>200�C)
) Ablation of the charChemical mechanisms
oxidation (CO, CO2)nitridation (CN)
Phase changesmeltingsublimation (C, C2, C3)
Mechanical removalspallation, shear stress,melt removal
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 11 / 34
Introduction: high-temperature gas dynamics
Three pillars for predictive engineering simulations
Computation cannot be truly predictive without the coupling tophysico-chemical models and experiments. . .
This coupling is precisely the verification and validation process!
Verification: Is the computational method implemented correctly?Validation : Are we solving the right equations?Uncertainty Quantification: Error bars in scientific predictions. . .
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 12 / 34
Introduction: high-temperature gas dynamics
Heat-flux measurement in plasma jet obtained in VKIPlasmatron facility
Water-cooled calorimeter in a plasma jet stream, VKI Plasmatron,air, 8g/s mass flow, 3500 Pa pressure, 0.370 MHz frequency,
120 kW generator power, 0.16 cm torch diameter
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 13 / 34
Introduction: high-temperature gas dynamics
Simulation of high-enthalpy flow in VKI Plasmatron facility
Inductively Coupled Plasma (ICP) wind-tunnelInjected gas
AirMass flow rate = 8 g/s, straight injectionTemperature = 300 K
Outlet pressure = 10 000 PaTorch characteristics (Plasmatron)
f = 0.37 MHzPower injected into the plasma = 60 kWConfiguration assumed to be axisymmetric
Dimensions [m]
0.16
0.15
0.486
0.05 0.05 0.05 0.05 0.050.127
0.21
8
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 14 / 34
Introduction: high-temperature gas dynamics
Physico-chemical models for ICP wind-tunnel
Steady Navier-Stokes equations (including time-average Lorentzforces and Joule heating source terms)Helmholtz di↵usion equation for magnetic field (Maxwell equations)Example of high-temperature property: dynamic viscosity of air as afunction of temperature (at 1 atm pressure)) Viscosity cannot be directly measured at temperatures above 5000 K) Closure at microscopic level by means of the kinetic theory of gases
0 2500 5000 7500 10000 12500 15000Temperature [ K ]
0.0
0.5×10-4
1.0×10-4
1.5×10-4
2.0×10-4
2.5×10-4
η [
kg
m-1
K-1
]
Chapman-EnskogGupta-Yos’s mixture ruleWilke’s mixture rule
11-species air mixture at 1 atm pressure
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 15 / 34
Introduction: high-temperature gas dynamics
Computed electromagnetic field
100
50
500
750 10001250
1500
150012501000
750500
250
250
100
12501500
1000750 25
0
15001250
750 1000
500
2000
2000
Induced electric field [V/m]
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 16 / 34
Introduction: high-temperature gas dynamics
Computed temperature and flow fields
Temperature field [K]
Streamlines
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 17 / 34
Flows with discontinuities
Outline
1 Introduction: high-temperature gas dynamics
2 Flows with discontinuitiesExamplesRankine-Hugoniot jump relations
3 Normal shocks
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 17 / 34
Flows with discontinuities Examples
Longshot Gun Tunnel at VKI
Schlieren visualisation of detached shocks in the Longshotfacility of the von Karman Institute for Fluid Dynamics
Nagamatsu probeStatic pressure
Reference probeStagnation point pressure andheat flux
FADS modelNose tip radius: 53 mmInstrumented with 5fast-response Kulite XCQ-093pressure sensors and 5 coaxialtype-E thermocouplesMeasurement locations: 1 atnosetip and 4 o↵-stagnationpoints at 45� equally spacedaround the probe
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 18 / 34
Flows with discontinuities Examples
Electric Arc Shock Tube (EAST) facility at NASA ARC
Electric Arc Shock Tube facilityNASA Ames Research Center
Snapshot of radiating flow measured bymeans of a spectrometer
Wavelength resolved on x-axisSpatially resolved on y-axisRadiative intensity indicated by color
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 19 / 34
Flows with discontinuities Examples
Shock tube operation
Wave propagation
Bursting of the diaphragm att = 0
Flow at rest and gases atambient temperatureDriver gas (region 4): highpressure p4Driven gas (region 1): lowpressure p1 ⌧ p4
Wave propagation at t = t⇤ > 0Expansion wave: region 3 ! 4Contact discontinuity wave:region 3 ! 2Shock wave: region 2 ! 1
Atmospheric entry shock layersimulated in region 2 behindshock wave
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 20 / 34
Flows with discontinuities Rankine-Hugoniot jump relations
Discontinuities in shock-tube flows
The interface between the regions 2 and 1 is called normal shockwaveIn the laboratory reference frame, the flow in region 1 is at rest(u1 = 0)As the normal shockwave propagates to the right with a velocity �, itincreases the pressure p2 of the gas behind it and induces a massmotion with velocity u2
In the shockwave reference frame (v = |u� �|), the normal shock waveappears stationary in space
The interface between the driver gas (region 3) and driven gase(region 2) is called contact surface
It propagates to the right with a velocity equal to the velocity of thegas in regions 2 and 3 (u2 = u3)The pressure is also preserved through a contact discontinuity (p2 = p3)
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 21 / 34
Flows with discontinuities Rankine-Hugoniot jump relations
Shock wave at microscopic level
The density rises continuously in shockwavesThe shock thickness if of the order of the mean-free-path (averagedistance between two successive collisions of a molecule)The flow is rarefied ) failure of the fluid dynamical description
Normalized density distribution across shock wave in Argon at M=9
Alsmeyer experiment
Navier-Stokes eqs.simulation
Computational FluidDynamics (CFD)
Boltzmann eq.simulation
Direct SimulationMonte-Carlo (DSMC)
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 22 / 34
Flows with discontinuities Rankine-Hugoniot jump relations
Euler eqs. as limit of the Navier-Stokes eqs.
Fluid dynamical description based on conservative equations for mass,momentum and total energy (in absence of external forces)
@t⇢+ @x
·(⇢u) = 0
@t(⇢u) + @x
·(⇢u⌦u + pI) + "@x
·⌧ = 0
@t(⇢E ) + @x
·(⇢uH) + "@x
·q + "@x
·(⌧·u) = 0
The Navier-Stokes equations are expressed by means of a closure. Forinstance, the viscous stress tensor is given by ⌧ = �2⌘S, with thevelocity gradient tensor S = 1
2
⇥@
x
u + (@x
u)T⇤� 1
3@x
·u IThe Navier-Stokes equations are written in a compact form as
@tU + @x
· F + "@x
· F d = 0
with U = (⇢, ⇢u, ⇢E )T and F = (⇢u, ⇢u⌦u + pI, ⇢uH)T
The Euler equations are obtained as the limit of the Navier-Stokesequations when the dissipative terms vanishes (" ! 0)
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 23 / 34
Flows with discontinuities Rankine-Hugoniot jump relations
Rankine-Hugoniot jump relations
N-S and Euler solutions match in inviscid regions upstream (1) anddownstream (2) of a discontinuity where gradients vanishes (F d = 0)
Let us consider a point P on a discontinuity surface moving at speed�, with the normal n to the surfaceLet us assume the existence of a travelling wave solution U = U(y) tothe Navier-Stokes equations in the vicinity of P , with
Normalized density distribution across shock wave
Coordinate: y = x · n � �ntNormal component: �n = � · n
Travelling wave eq.��n
dUdy + d
dy (F ·n)+" ddy (F
d ·n) = 0
After integrationR y2y1(·) dy from
region 1 to region 2, the Rankine -Hugoniot jump relations for inviscidflows are derived
�n(U2 � U1) = (F · n)2 � (F · n)1Magin (AERO 0033–1) Aerothermodynamics 2016-2017 24 / 34
Normal shocks
Outline
1 Introduction: high-temperature gas dynamics
2 Flows with discontinuities
3 Normal shocks
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 24 / 34
Normal shocks
Normal shock relations (inviscid flows)Rankine-Hugoniot relations for steady normal shocks� = 0, u = u ex , n = ex )
⇢2u2 = ⇢1u1
⇢2u22 + p2 = ⇢1u
21 + p1
⇢2u2H2 = ⇢1u1H1
These equations are valid for calorically perfect gases and mixtures ofgases in thermo-chemical equilibrium
For calorically perfect gases, further simplifications applyCalorically perfect gas law: p = ⇢RT with R = R
M and R = NAkB = 8.31 [J / (Kmole)]Specific energy: e = cvT , h = cpT , with cp � cv = R
Specific heat ratio: � =cpcv
Molecular gases: cv = 52R, � = 7
5 = 1.4
Atomic gases: cv = 32R, � = 5
3 = 1.66Entropy: s = cv ln
p⇢� = cp lnT � R ln p+ cp lnR
Speed of sound: a2 = (@p/@⇢)s = �p/⇢ = �RTMagin (AERO 0033–1) Aerothermodynamics 2016-2017 25 / 34
Normal shocks
Normal shock relations for calorically perfect gases
The total enthalpy conservation can be expressed as
H2 = H1 ) �
� � 1
p2⇢2
+u222
=�
� � 1
p1⇢1
+u212
The non-linear algebraic system of 3 eqs. in 3 unknowns ⇢2, u2, andp2 has a a closed solution expressed as a function of the dimensionlessparameters: Mach number M1 = u1/a1 and �, with a1 =
p�RT1
For M1 > 1(derivation given further in this section)
⇢2⇢1
= u1u2
=(�+1)M2
12+(��1)M2
1> 1
p2p1
= 1 + 2��+1 (M
21 � 1) > 1
T2T1
= ( p2p1)/( ⇢2⇢1
) =h1 + 2�
�+1 (M21 � 1)
i 2+(��1)M2
1(�+1)M2
1
�> 1
M22 =
1+ ��12 M2
1
�M21�
��12
< 1
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 26 / 34
Normal shocks
Entropy across normal shocks
The entropy variation through a normal shock is
s2 � s1 = cp lnT2
T1� R ln
p2p1
= cv lnp2/p1
(⇢2/⇢1)�
This function is positive for M1 � 1 ) the 2nd law of thermodynamicsimposes that, for a calorically perfect gas, a shock wave may onlyhappen if M1 � 1
What is the origine of the entropy increase through a shock wave?Answer: the changes across the shockwave occur through a shortdistance of the order of the mean-free-path. Through the shockstructure, the gradients are very large. In turns, heat fluxes and viscousstresses are dissipative phenomena that generate entropy
Weak shock: M21 = 1 + " with 0 < " ⌧ 1
p2p1
= 1 + 2��+1 " and ( ⇢2⇢1
)�� = (1 + ")��⇣1 + ��1
�+1 "⌘�
p2p1( ⇢2⇢1
)�� ⇠ 1 + 23�(��1)(�+1)2
"3 +O("4)
) s2�s1cv
⇠ 23�(��1)(�+1)2
"3 +O("4): isentropic approximation valid for weak shocks
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 27 / 34
Normal shocks
Total and critical quantities
Consider a fluid element in an arbitrary flow travelling at velocity uwith static pressure p and temperature T
Total pressure p0 and total temperature T0
They are defined as quantities obtained by isentropically decelerating the
flow to rest
⇢H = cpT0 = cpT + u2/2s = cp lnT0 � R ln p0 = cp lnT � R ln p
Critical conditions
Let us imagine that a fluid element is adiabatically decelerated (if M > 1)or accelerated (if M < 0) until its velocity equals the speed of sound:u⇤ = a⇤ =
p�RT⇤. The velocity reached at critical condition is sonic
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 28 / 34
Normal shocks
Total and critical quantities
In steady inviscid flows, we will show in lecture 2 that the totalenthalpy is constant along a trajectory (pathline)
Therefore, in steady inviscid flows, one has,
H = cpT0 = cpT⇤ +
�RT⇤
2= 1
��1a⇤2 +
a⇤2
2= 1
2
� + 1
� � 1a⇤2
) The total temperature, critical temperature, and critical speed of soundare constant properties of a streamline
Through a normal shock) The total temperature is conserved T0,2 = T0,1
) The critical temperature and critical speed of sound are conserved:
T ⇤2 = T ⇤
1 and a⇤2 = a⇤1) The total pressure is a decreasing function: p0,2
p0,1= exp(� s2�s1
R )
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 29 / 34
Normal shocks
Total quantities (local quantities with definition still valid for viscous flows)
The total temperature is obtained from
T0
T= 1 + 1
2
u2
cpT= 1 + �R
2cp
u2
a2
= 1 + ��12 M2
The isentropic relations p0p =
⇣⇢0⇢
⌘�=
⇣T0T
⌘ ���1
yields the expressions
for the total pressure and total density
p0p
=⇣1 + ��1
2 M2⌘ �
��1
⇢0⇢
=⇣1 + ��1
2 M2⌘ 1
��1
For M ⌧ 1, using the Taylor expansion (1 + x)↵ = 1 + ↵x +O(x2),the Bernoulli relation for incompressible flows is retrieved
p0p
= 1 + �2M
2 +O(M4) ) p0 ⇠ p + 12⇢u
2
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 30 / 34
Normal shocks
Pitot probe measurement in the Plasmatron facilityHenri Pitot (1695-1771), French hydraulic engineer, is the inventor ofthe Pitot tubePitot probes are widely used in fluid dynamics (airspeed of aircraftand air and gas velocities in industrial applications)
The stagnation pressure is measured at the probe nose pPitotFor low Mach number flows, pPitot = p0 ⇠ p + 1
2⇢u2
In low Reynolds number flows (e.g . subsonic plasma flows): pPitotdeparts from p0 due to viscous e↵ects [Barker, 1922]
10144
10145
10147
10146
1014410147
10146 10145
10146
10147
10148
Pressure field around a Pitot probe in a plasma jet at Mach = 0.1(�p = 1 Pa)
p=10,145 Pa, ⇢ = 6.6 kg/m3, u=137.2 m/s ) p0=10,207 PaThe Reynolds number based on the probe radius (3 mm) is Re = 19 and pPitot=10,225 Pa
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 31 / 34
Normal shocks
Prandtl’s relation for normal shocks
Prandtl’s relation, a⇤2 = u1u2, is derived as followsTotal enthalpy conservation: �
��1p2⇢2
+u222 = �
��1p1⇢1
+u212 = 1
2�+1��1a
⇤2
Alternative form: p2⇢2
=� � 1
2�
✓� + 1
� � 1a⇤2 � u22
◆
p1⇢1
=� � 1
2�
✓� + 1
� � 1a⇤2 � u21
◆
Introducing the previous relations in the ratio of momentum to massshock relations
⇢2u22 + p2⇢2u2
=⇢1u21 + p1
⇢1u1) u2 +
p2⇢2u2
= u1 +p1
⇢1u1
yields Prandtl’s relation after some algebra
The critical Mach number M⇤ = u/a⇤, can be obtained from
1
� � 1a2 +
u2
2= 1
2
� + 1
� � 1a⇤2 ) 1
� � 1
1
M2+
1
2= 1
2
� + 1
� � 1
1
M⇤2
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 32 / 34
Normal shocks
Application of Prandtl relation and critical Mach number
The critical Mach number behaves as the local Mach number butremains finite at high speeds
M⇤2 =(� + 1)M2
2 + (� � 1)M2)
M⇤ < 1 if M < 1M⇤ = 1 if M = 1M⇤ > 1 if M > 1
M⇤ ! �+1��1 if M ! 1
Alternative form of Prandtl relation for normal shocks: M⇤1M
⇤2 = 1
For a normal shock M1 > 1 ) M⇤1 > 1 ) M⇤
2 < 1 ) M2 < 1
The normal shock relations are then easily derived as follows⇢2⇢1
= u1u2
=u21
u1u2=
u21a⇤2
= M⇤21 =
(�+1)M21
2+(��1)M21
M⇤22 = 1
M⇤21
) (�+1)M22
2+(��1)M22=
2+(��1)M21
(�+1)M21
) M22 =
1+ ��12 M2
1
�M21�
��12
p2 � p1 = ⇢1u21 � ⇢2u22 = ⇢1u1(u1 � u2) = ⇢1u21(1� u2u1)
) p2�p1p1
= �M21 (1� u2
u1) = �M2
1
✓1� (�+1)M2
12+(��1)M2
1
◆= 2�
�+1 (M21 � 1)
T2T1
= ( p2p1)/( ⇢2⇢1
) =h1 + 2�
�+1 (M21 � 1)
i 2+(��1)M2
1(�+1)M2
1
�
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 33 / 34
Normal shocks
Exercise
Consider a shock-tube facility closed at both ends with a diaphragmseparating a region of high-pressure gas on the left (region 4) from aregion of low-pressure gas on the right (region 1). When the diaphragm isbroken at t = 0 s (for instance by mechanical means), a shock wavepropagates into section 1 and an expansion wave propagate into section 4.As the normal shock-wave propagate to the right with a constant velocity�, it increases the pressure of the gas behind it (region 2), and induces amass motion with velocity u2.
1 Derive the Rankine-Hugoniot jump relations between the regions 1 and 2 with the gasvelocities u1 and u2 in the laboratory frame.
2 Using the change of variables v = u � � for the velocity in the shock- wave frame, showthat the normal shock relations are satisfied in this reference frame.
⇢2v2 = ⇢1v1
⇢2v22 + p2 = ⇢1v
21 + p1
h2 +12 v
22 = h1 +
12 v
21
Magin (AERO 0033–1) Aerothermodynamics 2016-2017 34 / 34