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Fire Storms and Large Scale Modelling Derek Bradley University of Leeds UKELG 50TH ANNIVERSARY DISCUSSION MEETING “Explosion Safety – Assessment and Challenges” 9th to 11th July 2013 Cardiff University

Fire Storms and Large Scale Modelling

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Fire Storms and Large Scale Modelling. Derek Bradley University of Leeds UKELG 50TH ANNIVERSARY DISCUSSION MEETING “Explosion Safety – Assessment and Challenges” 9th to 11th July 2013 Cardiff University. Fire Storms ?. The Buoyant Plume. Conditions for a Fire Storm. - PowerPoint PPT Presentation

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Page 1: Fire Storms and Large Scale Modelling

Fire Storms and Large Scale Modelling

Derek BradleyUniversity of Leeds

UKELG 50TH ANNIVERSARY DISCUSSION MEETING

“Explosion Safety – Assessment and Challenges”

9th to 11th July 2013Cardiff University

Page 2: Fire Storms and Large Scale Modelling

Fire Storms ?

Page 3: Fire Storms and Large Scale Modelling

•  

Page 4: Fire Storms and Large Scale Modelling

The Buoyant Plume

Page 5: Fire Storms and Large Scale Modelling

Conditions for a Fire Storm

• High column of burned gas

• Large spillage and favourable topology

• Turbulence generation at base

• Rich aerosol mixture topped by lighter fractions

• Large turbulent length scales

• (Turbulence, buoyancy and aerosols give positive feed-back)

Page 6: Fire Storms and Large Scale Modelling

Atmospheric Turbulenceu m/s u′ m/s l m

zo = .05 m zo = 1 m zo = .05 m zo = 1 m

3 (light breeze)

0.57 1.30 59.8 26.1

15 (near gale)

2.83 6.51 59.8 26.1

31 (violent storm)

5.85 13.46 59.8 26.1

Page 7: Fire Storms and Large Scale Modelling

Turbulent Explosion

Page 8: Fire Storms and Large Scale Modelling

Turbulent Burning Correlation

U = ut /u' K =0.25(u'/uℓ)2Rl-0.5

Page 9: Fire Storms and Large Scale Modelling

Cellular Laminar Explosion

Page 10: Fire Storms and Large Scale Modelling

Laminar Instability Inner and Outer Cut-offs

Flame area ratio

= (ns/nl)D-2

Fractal Dimension,D = 7/3

Page 11: Fire Storms and Large Scale Modelling

Spillage Magnitudes

Spillage at Explosion

(tonnes)

Spillage Area (m2)

Mean height at lean flammability limit (m)

Donnellson

(1978)

300 304,000 24

Ufa

(1989)

4,500 2,500,000 140

Page 12: Fire Storms and Large Scale Modelling

Atmospheric Turbulenceu m/s u′ m/s l m

zo = .05 m zo = 1 m zo = .05 m zo = 1 m

3 (light breeze)

0.57 1.30 59.8

K=0.0004

26.1

K=0.0019

15 (near gale)

2.83 6.51 59.8

K=0.0041

26.1

K=0.022

31 (violent storm)

5.85 13.46 59.8

K=0.012

26.1

K=0.064

Page 13: Fire Storms and Large Scale Modelling

Turbulent Burning Correlation

U = ut/u' K =0.25(u'/uℓ)2Rl-0.5

Page 14: Fire Storms and Large Scale Modelling

0.01 0.1 10

2

4

6

8 Masr

-23 -19 3

Flame stretchdominant regime

Flame Instabilitiesdominant regime

U

K

Regime of Peak Turbulence-Instability Interaction

Page 15: Fire Storms and Large Scale Modelling

Influence of ls/lG on U

0

1

2

3

4

5

6

7

0 0.02 0.04 0.06 0.08

K

U

0

10

20

30

40

50

60

ls /lG

U

l s /lG 2128 Kll ss G

Masr = -23 Masr = 3

Page 16: Fire Storms and Large Scale Modelling

Estimated Donnellson Burning Velocity

Page 17: Fire Storms and Large Scale Modelling

Ufa

X

Page 18: Fire Storms and Large Scale Modelling

Ufa Topography

Page 19: Fire Storms and Large Scale Modelling

Ufa Ignition Source

Page 20: Fire Storms and Large Scale Modelling

The Buoyant Plume

Page 21: Fire Storms and Large Scale Modelling

Ufa Topography

Page 22: Fire Storms and Large Scale Modelling

Ufa and Donnellson Burning Velocities Compared

Page 23: Fire Storms and Large Scale Modelling

23

Congestion:Flame and Shock Wave in a Duct

aA

Flame Shock wave

Page 24: Fire Storms and Large Scale Modelling

The Maximum Turbulent Burning Velocity

Page 25: Fire Storms and Large Scale Modelling

Maximum Turbulent Burning Velocity

Page 26: Fire Storms and Large Scale Modelling

Influence of Venting Ratio, A/a

0

5

10

15

20

25

0 0.5 1 1.5 2

u t /a 1

P2/

P1

1

2

3

4

5

6

T2/T

1

A/a = 3

A/a = 1.44

g = 1.4

Page 27: Fire Storms and Large Scale Modelling

0

10

20

30

40

50

0 5 10 15 20 25

x

B

DEVELOPING DETONATION

P

e

x u

x l

N2

K2

S E

65.2

33.7

48.4

0

10

20

30

40

50

0 5 10 15 20 25

x

B

DEVELOPING DETONATION

P

e

x u

x l

N2

K2

S E

65.2

33.7

48.4

Strong, Stable, Detonations require Low (ξε), or (τi /τe)

Page 28: Fire Storms and Large Scale Modelling

Problems of Large Scale Modelling

• Uncertain discharge composition, mixing, and circumstances of ignition.

• Uncertain physico-chemical data (Ma, extinction stretch rates, burning velocities, (τi /τe).

• Complexity of congestions,venting, shock wave reflection and refraction.

• Uncertainties in rate of change of heat release rate.

Page 29: Fire Storms and Large Scale Modelling

References

• G.M. Makhviladze, S.E. Yakush, (2002) “Large Scale Unconfined Fires and Explosions,” Proceedings of the Combustion Institute 29: 195-210.

• D. Bradley, M. Lawes, K. Liu, M.S. Mansour, (2013) “Measurements and Correlations of Turbulent Burning Velocities over Wide Ranges of Fuels and Elevated Pressures,” Proceedings of the Combustion Institute 34: 1519-1526.

• D. Bradley, M. Lawes, Kexin Liu, (2008) “Turbulent flame speeds in ducts and the deflagration/detonation transition,” Combust. Flame 154 96-108.

• D. Bradley, (2012) “Autoignitions and detonations in engines and ducts,” Philosophical Transactions of the Royal Society a-Mathematical Physical and Engineering Sciences, 370, no. 1960: 689–714.