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Abo Homos-Nubaria Pipeline QRA

Weather Data

The Weather Data relevant to this study consists of a list of weather conditions in the form of different combinations of wind-speed, temperature, humidity and atmospheric stability. The weather conditions are an important input into the dispersion calculations and results for a single set of conditions could give a misleading picture of the hazard potential.

Mete oceanographic data gathered for Greater Cairo over a period of 5 years. This data included wind speed and direction; air temperature and pressure, as well as current speed, direction and wave height.

The general climatic conditions at North Cairo are summarised below:

Air Temperature oC:

 

o

Minimum recorded

- 1.1

o

Maximum recorded

52.2

o

Yearly average

28

Relative humidity %:

o Average daily minimum82

o

Average daily minimum54

o

Annual average

78

The recorded annual wind speeds at Cairo are shown in Table 10.1.

Month Jan.

Wind

4.7

speed

 

Table 10.1 Wind speeds at Cairo (Knots)

Feb.

Mar.

Apr.

May

June

July

Aug.

Sep.

Oct.

 

 

 

 

 

 

 

 

 

5.6

6.3

6.2

5.6

5.2

4.4

3.4

3.6

4.0

 

 

 

 

 

 

 

 

 

Nov.

Dec

3.84.4

In wind Rose figures the radius = 10%

Average wind speed

=

2.44 m/sec.

Wind Direction:

Three permanent high-pressure belts control the wind circulation over Egypt: the Azores, the Indian subtropical and the South Atlantic subtropical. In addition, there is a permanent low-pressure belt ‘the doldrums’ which crosses Africa near the equator. Seasonal high and low pressure systems also alternate over the continental mass, the red sea, the Mediterranean and the Arabian Peninsula.

Table 10.2 Wind Rose for North Cairo

20

Abo Homos-Nubaria Pipeline QRA

 

 

 

 

 

 

 

 

 

345/

015/

045/

075/

105/

135/

165/

195/

225/

255/

285/

315/

 

014

044

074

104

134

164

194

224

254

284

314

344

Jan

5.4

8.5

7.4

3.0

1.3

2.7

13.5

14.8

12.6

8.5

6.3

5.8

Feb

9.9

14.4

8.7

3.6

1.2

1.3

8.0

12.0

10.1

7.1

6.1

8.9

Mar

15.8

16.3

9.3

3.6

1.4

1.6

5.0

7.5

6.4

7.9

8.2

10.1

Apr

15.8

21.4

13.3

4.3

0.7

0.6

1.7

3.0

5.0

7.0

8.6

12.5

May

21.3

24.9

13.3

3.0

0.6

0.3

0.7

1.3

2.0

4.3

7.7

14.4

June

24.4

22.2

8.3

1.3

0.1

0.1

0.2

0.7

1.2

2.9

9.3

20.1

July

26.3

16.4

4.8

0.8

0.2

0.0

0.1

0.2

1.2

3.1

7.7

23.4

Aug

29.1

16.2

3.8

0.8

0.4

0.0

0.0

0.2

0.9

2.6

6.8

21.6

Sep

22.8

23.9

8.1

1.4

0.2

0.2

0.7

1.2

0.8

1.3

6.3

15.4

Oct

19.4

23.2

11.4

2.9

0.4

0.4

1.5

1.8

3.0

3.7

7.6

10.5

Nov

16.6

17.2

6.6

1.9

0.5

0.8

3.3

5.7

6.6

6.3

7.2

9.7

Dec

10.6

10.8

6.8

2.4

0.8

1.9

8.8

12.0

8.3

8.2

5.9

8.8

The prevailing winds are quite parallel to or heading towards the Northwest, mostly from west to north all year, except December and January, when they are from SE. When atmospheric low pressure is passing quite frequently and fast, the wind direction will change ‘anti-clockwise’, normally during a short period of one to two days. After a low pressure has passed, the wind returns to the prevailing direction (W-NW). The mean wind speed at Cairo is 2.44 m/sec.

Data on the direction of wind at North Cairo was obtained from the Egyptian Meteorological Office. Table 10.2 shows the analysis of the 12-months wind distribution data over a period of 10 years. FIGURE 10.1 gives the average wind directions at Cairo throughout the year.

21

Abo Homos-Nubaria Pipeline QRA

Jan

Feb

March

April

May

June

July

August

Sept

Oct

Nov

Dec

FIGURE 10.1 Average wind directions at Cairo

The overall analysis of the wind data at Cairo is given in what is known as the wind rose. FIGURE 10.2 shows Cairo wind rose, based on data collected during 19922000. Note that winds blow towards the centre of the rose.

18% 20%

15%

7%

 

5%

 

6%

2.4

4%

 

5%

 

3%

N

 

5% 4%

8%

 

> 22.5 m/sec

20 - 22.5

17.5 - 20

15 - 17.5

12.5 - 15

10 - 12.5

7.5 -10

5- 7.5

2.5 - 5

0- 2.5

FIGURE 10.2 the Wind Rose at Cairo

22

Abo Homos-Nubaria Pipeline QRA

Stability Categories:

The two most significant variables, which would affect the dispersion calculations, are: Wind-speed and atmospheric stability. The stability class is a measure of the atmospheric turbulence caused by thermal gradients. Pasquill Stability identifies six main categories, which are shown in the Table 10.3.

Table 10.3 Pasquill Stability Categories

 

 

 

A

B

C

D

E

F

Very Unstable

Unstable

Moderately Unstable

Neutral

Moderately Stable

Stable

Neutral conditions correspond to a vertical temperature gradient of about 1(oC) per 100m.

Cairo weather data for the Geographical area is somewhat limited and do not show seasonal variations over a long time.

Therefore, the calculations included in this study have considered alternative stabilities for the average wind speed of 2.4 m/sec.

This was done with reasonable accuracy, since the stability is related to the wind speed, and the range of stabilities that is observed for a given wind speed is generally small, as shown in the Table 10.4.

As the range is large for a given wind speed, the calculations have initially considered four different combinations of wind speeds and stability classes to include the worst possible conditions.

The calculations have also considered atmospheric temperature (30oC), relative humidity 70% and surface roughness parameter of 0.1.

Table 10.4 The Relationship between Wind speed and Stability

Wind speed

 

 

Day-time

 

 

 

Night-time

 

 

 

Solar Radiation

 

 

 

Cloud Cover

 

(m/s)

strong

 

medium

 

slight

 

thin

medium

 

overcast

 

 

 

 

 

 

 

<3/8

>3/8

 

>4/5

<2

A

 

A-B

 

B

-

-

 

D

2-3

A-B

 

B

 

C

 

E

F

 

D

3-5

B

 

B-C

 

C

 

D

E

 

D

5-6

C

 

C-D

 

D

 

D

D

 

D

>6

C

 

D

 

D

 

D

D

 

D

At night, the ground is often cooler than the air if the sky is clear, and this gives rise to the most stable conditions and potentially the greatest effect distances.

FIGURE 10.3 shows the criteria used for the selection of weather parameters used for the consequences modelling for this study.

23

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Is the ground covered

 

 

Check category

 

m/s

 

 

 

 

 

 

 

0- 6

 

F

 

 

in frost or snow?

 

 

against wind speed

 

 

 

 

 

> 7

 

 

 

 

 

 

 

 

 

 

 

 

 

E

 

 

 

 

 

 

 

 

 

 

 

 

 

 

No

 

 

 

 

 

 

 

 

 

 

 

 

Is it night-time?

Yes

 

Is sky overcast?

 

Yes

 

D

m/s

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

F

No

 

 

 

 

No

 

 

 

 

 

< 2

 

 

 

 

 

 

 

 

 

 

 

 

 

Sky more than half covered Y

Check category

2

E

Inland

Coastal

 

> 3

 

 

 

 

 

 

 

 

against wind speed

D

sites

sites

 

 

 

No

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Sky clear?

 

 

 

Check category

m/s

F

 

 

 

 

 

 

 

against wind speed

< 2

 

 

 

 

 

 

 

 

 

 

 

Wind mainly from

Yes

D

 

 

 

 

 

2-4

E

 

from the sea?

 

 

 

 

 

 

 

> 5

 

 

 

 

 

 

 

 

 

 

D

 

 

 

 

 

 

 

 

 

 

 

 

 

No

 

 

 

 

 

 

 

 

 

 

 

Time within 1 hr

Yes

D

 

 

 

 

 

 

 

 

 

before sunset?

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

No

 

 

 

 

 

 

 

Yes

F

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Time within 1 hr

Yes

Sky clear and

 

 

 

 

 

 

 

after sunrise?

 

wind calm/light?

 

No

D

 

 

 

 

 

 

 

 

 

 

 

 

 

 

No

 

 

 

 

 

 

 

 

 

 

 

 

Is sky overcast?

Yes

 

 

 

 

Check category

m/s

C

 

 

 

 

 

 

against wind speed

0- 4

 

 

 

No

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

> 5

D

 

 

 

 

 

 

 

 

 

 

 

 

 

Summer only

Select weather type from

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Hot

 

Warm

Cool

 

 

 

 

 

 

Check category

 

 

Check category

 

 

Check category

 

against wind speed

 

against wind speed

 

against wind speed

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

m/s

A

 

 

m/s

 

 

A

 

 

m/s

 

 

C

 

< 3

 

 

 

 

< 1

 

 

 

 

0- 4

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

3- 4

 

 

B

 

1- 3

 

 

B

 

 

> 5

 

 

D

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

5- 8

C

 

4- 7

 

 

C

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

> 8

 

 

 

 

 

> 7

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

D

 

 

 

 

 

 

D

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

24

Abo Homos-Nubaria Pipeline QRA

FIGURE 10.3 Determinations of Modified Pasquill Stability Categories

Category D (neutral) is the most probable at inland sites, and appears to occur for up to 80% of the time at Cairo. To overcome the uncertainty of the accuracy of Cairo weather data results, the following cases were selected in this analysis to study the effects of normal and extreme weather conditions at Cairo.

Table 10.5 Sets of weather conditions initially selected for this study:

 

Set 1

 

Set 2

Wind speed

 

Stability

Wind speed

 

Stability

2 m/s

 

F

10 m/s

 

D

The wind speed range between 1 to 5 m/s was considered to be reasonable representation of typical conditions at Cairo. This would overcome some of the uncertainty of the meteorological data provided by the meteorological office. Wind speeds in excess of 8 m/s are likely to disperse the cloud over long distances to well below LFL.

The weather set 2 was eventually selected to represent the most likely conditions; however the worst case conditions shall be defined by a sensitivity analysis study.

25

Abo Homos-Nubaria Pipeline QRA

Release Scenarios

Events associated with release, dispersion and ignition of flammable releases considered in this study can be summarized in the following figure.

 

 

 

Release

 

 

 

 

 

Yes

Ignites?

No

Dispersing cloud

 

 

 

 

 

Yes

Ignites?

No

 

 

 

 

More obstacles

 

 

 

 

 

Greater confinement

 

 

 

 

 

Flame acceleration

 

 

Jet fire

 

Pool fire

Cloud fire

Fast flame

Internal

Safe

 

explosion

dispersion

 

 

 

 

 

 

Impinge?

 

 

 

 

 

 

Yes

 

 

 

 

Structural

BLEVE

 

 

 

 

Failure

 

 

 

 

 

 

 

 

 

 

 

Figure 11.1 Hazardous events

These events can be more detailed as follows:

Jet fires

A jet fire will result from an ignited pressurized hydrocarbon gas release. The

 

consequence of jet fires is directional depending on the on release orientation.

 

Jet fires typically have flame temperature of about 2,200 oF and can produce

 

high intensity thermal radiation. The high temperature poses a hazard from

 

direct effects of heat on humans and also from possibility of escalation. If a jet

 

flame impinges upon a target such as a vessel, pipe or structural member, it

 

can cause failure of the item to fail within several minutes.

Jet (spray) fire will also result from ignited continuous releases of pressurized flammable liquid. The momentum of the release carries the material forwards in

26

Abo Homos-Nubaria Pipeline QRA

 

a plume entraining air to give a flammable mixture as gas is released from the

 

plume.

Flash fires

If flammable gas accumulates in an unconfined area and is ignited, then the

 

result will be a flash fire within the flammable limits of the vapour cloud.

Explosions

Ignition of accumulated gas in semi-confined areas may also be accompanied

 

by an explosion; the overpressure generated will depend on the degree of

 

congestion and confinement of the process area, and the gas cloud size.

Pool fires

If a liquid release is ignited after it has time to form a pool, a pool fire results.

 

Because they are less well aerated, pool fires tend to have lower flame

 

temperatures and produce lower levels of thermal radiation than jet fires. They

 

also produce more smoke. Although a pool fire can still lead to structure failure

 

of items within the flame, this would take longer than in a jet fire.

 

An additional hazard of pool fires is their ability to flow. A burning liquid pool can

 

spread along horizontal surface or run down a vertical surface to give a running

 

fire.

BLEVE

BLEVE stands for Boiling Liquid Expanding Vapour Explosion.

(Fire Ball)

 

 

A fire ball can occur if a vessel containing fuel ruptures in the presence of an

 

ignition source (usually a jet or pool fire). A fraction of the liquefied fuel

 

subsequently released will evaporate immediately and take part in a huge

 

fireball, which has the shape of a hemispherical burning cloud or ball of fire.

 

High degree of turbulent mixing and rapid air entrainment allows large quantities

 

of fuel to be consumed in a short period of time.

Structural

Loss of structure integrity due to overheating of structure members. The

failure

structure shall collapse under much lower load than the designed due to

 

increased temperature.

Safe

Dilution of the released gases beyond the lower flammability limits (LFL) leading

dispersion

to safe dispersion situation.

27

Abo Homos-Nubaria Pipeline QRA

Impairment Criteria

This section defines the human injury and asset impairment criteria in caring out the consequence analysis of the identified hazardous events scenarios on the proposed facilities.

Table 12.1 represents standard human impact criteria as applied in consequence modelling.

Table 12.1: Criteria for Assessment of Fire Effects on Humans

Event Effect

Distance to

Effect

Jet fire / Pool fire

4.7kW/m2

Will cause pain in 15-20 seconds and injury after 30

 

 

seconds exposure.

 

12.5 kW/m2

Significant chance of fatality for extended exposure

 

 

and high chance of injury.

 

37.5 kW/m2

Significant chance of fatality for people exposed

 

 

instantaneously.

Flash fire

LFL

Fatal for people in the flammable cloud path

Explosion

0.05 Bar

Will cause injuries from flying debris

overpressure

0.2 Bar

20% chance of fatality to a person in a protected

 

 

enclosure

 

0.3 Bar

Threshold for eardrum damage,

 

 

50% chance of fatality for a person within enclosure,

 

 

15% chance of fatality for a person in the open.

 

0.50 Bar

Will cause 100 % fatality for a person within enclosure

 

 

or in the open.

The criteria applied for assessment of the effects of fire on assets are summarised in Table 12.2.

Table 12.2: Criteria for Assessment of Fire Effects on Assets

Impairment Mechanism

Level

Effect

Thermal Radiation

4.7kW/m2

Impairment of evacuation/embarkation areas

 

6.3 kW/m2

Impairment of escape routes

Thermal Radiation or Flame

500 deg.C

Structural Failure.

Impingement on Load Bearing

 

 

Structural Steel

 

 

Both jet fires and explosions can lead to structure failure of items, though this will take several times longer for jet fires than for explosions. Table 13.3 presents indicative failure times under hydrocarbon fire impact conditions, where times to failure refer to burn through or loss of load bearing capacity.

Table 12.3: Structure Failure times in Fires (Indicative)

 

Component

 

Time to Failure (Min)

 

Jet Fire

 

Pool Fire

 

 

 

Unprotected structural steel beam

 

10

 

10

Unprotected steel plate

 

5

 

10

A-60 firewall

 

15

 

60

H-120 firewall

 

60

 

120

 

28

 

 

 

Abo Homos-Nubaria Pipeline QRA

Table 12.4 reports published information on the explosion overpressure effects.

Table 12.4: Explosion Overpressure Effects

Explosion

Damage

Overpressure - Bar(g)

0.0250% windows shattering

0.07Collapse of tank roof

0.07-0.14

Connection failure of corrugated panelling

0.08-0.1

Minor damage to steel framework

0.15-0.2

Wall of concrete blocks shattered

0.2

Collapse of steel framework

0.3

"Reparable damage" cladding blown off. Offshore bridjes and lifeboats

 

impaired

0.34Steel walls blown off. Process plant within offshore module rupture, in neighbouring modules damaged. 50% chance for ESD valve closure failing

1.0

Columns and buoyant deck of semi-sub ruptured

2.0

Riser wall rupture

29