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B744, en-route, Alaska USA, 1989 (WX LOC)

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Event Details
When December 1989
Event Type LOC, WX
Day/Night Day
Flight Conditions IMC
Flight Details
Aircraft BOEING 747-400
Operator KLM
Domicile Netherlands
Type of Flight Public Transport (Passenger)
Origin Amsterdam/Schiphol
Intended Destination Tokyo/Narita
Actual Destination Anchorage
Flight Phase Descent
ENR / APR
Location En-Route
Origin Amsterdam/Schiphol
Destination Tokyo/Narita
Location
Approx. near Mt. Redoubt, Alaska
Loading map...
LOC
Tag(s) Loss of Engine Power
Environmental Factors
WX
Tag(s) Volcanic Ash Effects
Outcome
Damage or injury No
Aircraft damage Nonewarning.png"None" is not in the list of possible values (Minor, Major, Hull loss) for this property.
Injuries Nonewarning.png"None" is not in the list of possible values (Few occupants, Many occupants, Most or all occupants) for this property.
Fatalities Nonewarning.png"None" is not in the list of possible values (Few occupants, Many occupants, Most or all occupants) for this property.
Causal Factor Group(s)
Group(s) Aircraft Operation
Safety Recommendation(s)
Group(s) None Made
Investigation Type
Type Independent

Volcanic Ash Encounter

Contents

Description

On 15th December 1989, a KLM Boeing 747 encountered a Volcanic Ash cloud over Alaska, USA. the ingestion of ash led to compressor stall of all engines; the engines were subsequently relighted successfully and the aircraft landed safely.

Synopsis

During Descent through FL260 the aircraft flew into a volcanic ash cloud (the result of an eruption of Mount Redoubt). Ash and smoke entered the cockpit and the crew donned Oxygen masks and applied maximum power in an attempt to climb back out of the cloud. One minute later all 4 engines lost power, there was electrical power interruption, a loss of airspeed indication (caused by blocked pitot tubes), and a fire warning alarm for the forward cargo area (caused by the smoke rather than a fire). After 8 or 9 attempts and descent to 13,300 feet, the crew were able to restart the engines and the flight made a safe landing.


The NTSB determined the probable cause as:

"Inadvertent encounter with volcanic ash cloud, which resulted in damage from foreign material (foreign object) and subsequent compressor stalling of all engines. A factor related to the accident was: the lack of available information about the ash cloud to all personnel involved."

Effect of Volcanic Ash on Jet Engines

The following is taken from the proceedings of the First International Symposium on Volcanic Ash and Aviation Safety, 1991:

"Ingestion of volcanic ash by high performance turbofan engines at operating conditions melts glass shards and some of the minerals that make up the ash. Volcanic glass compositions can show wide variations and still be melted upon ingestion into the engine because of high engine operating temperatures. Operating temperatures must be lowered below the lowest melting temperature (c. 1,000 deg C for glass) to prevent melting of ingested volcanic ash. Reduction of engine operating conditions to idle settings (c. 600°C) will prevent melting of ingested volcanic ash", an interesting summary of earlier Alaskan aircraft events and a review of the precise ingestion effects on the GE engines in the KLM 744 - "The primary cause of engine thrust loss…was the accumulation of melted and resolidified ash on the stage- 1-turbine nozzle guide vanes. These deposits reduced the effective flow of air through the engine causing compressor stall. Reduction of thrust level while in an ash cloud significantly reduces the rate of engine-performance degradation"

Related Articles

Further Reading

NTSB

  • For further information on this particular incident, see the NTSB Accident Report which contains brief details of the event.

ICAO

US Geological Survey

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