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VAJONT DAM VAJONT DAM FAILURE FAILURE MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS

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Page 1: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

VAJONT DAM FAILUREVAJONT DAM FAILURE

MARIA CHINIVIKI IOANNOUTHEMISTOKLIS TERATSIAS

Page 2: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

INTRODUCTIONINTRODUCTIONo Vajont valley: part of the NE

Italian Alps region

o The dam is located between the

mountains Toc and Salta

o Narrow, deep side slopes and

glacial morphology

o Height: 262 m above the valley

floor

o Width: 190 m at the top and

27 m at the bottom

o Construction: 1956-1960

o Volume: 150 million m³ of

water

Page 3: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

GEOLOGYGEOLOGY

o Vajont Valley dominating rocks :

• Limestones

• Dolomites

o Two locations under consideration

o Location with more rigid limestones and bigger dam capacity

More or less fractured

Page 4: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

GEOLOGYGEOLOGY

Colle Isolato (1959):

Provides evidence for the existence of the prehistoric landslide

o Overlying alluvial deposits from old river

o Different from in-situ rock mass

Page 5: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

CHRONICLE - RECORDSCHRONICLE - RECORDSo June 1960: a report pointed out that

potential reservoir filling would

cause sliding

o July 1960: a report indicated that

sliding could occur only in the surface

o December 1959: seismic velocity

of rock 5,000-6,000 m/s

o Reduced to 1,000-2,000 m/s in one year

Page 6: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

CHRONICLE - RECORDSCHRONICLE - RECORDSo 4th November 1960: a mass of debris

estimated to 700,000 m3 slipped

o May 1960 - August 1963: seismographs

placed on the dam

o May 1963: Velocity of slip 1 mm/day

o August 1963: Velocity of slip

5 mm/day

Page 7: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

DAY OF CATASTROPHEDAY OF CATASTROPHE

o By September the velocity of movements = 20mm/day

=> Operations to lower reservoir level began

=> Velocity continued to increase rapidly

9th of October 1963, at 22.39:

Sudden slide of the main rock mass

Page 8: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

DAY OF CATASTROPHEDAY OF CATASTROPHEo Landslide detached from the southern slope of Mt. Toc

o Volume of the landslide = 270 million m3

o Collapsed in 45s

o 25 million m3 of water was displaced

o Wave crested 140 m above the dam’s crest and that still had a height of 70 m downstream

Page 9: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

DAY OF CATASTROPHEDAY OF CATASTROPHEo Energy of spilled water = 1.5 x Hiroshima’s atomic bomb

o The wave hit the town of Longarone and other villages killing more than 2000 people

o The dam remained almost intact even if the load at the abutment was 8 times greater than design load

Page 10: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

CAUSES OF FAILURECAUSES OF FAILURE

Generally agreed that failure

happened along bands of clay

(5-15 cm thick) inside the

limestone mass:

Clay layers

Page 11: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

CAUSES OF FAILURECAUSES OF FAILURELandslide initiation factors:

I.Prehistoric landslide located in the northern part of the slope :

=> Reactivated by the water level rise

II.Clay layers below slide

=> Mobilized by the increase of water pore pressures

High velocity of displacement:

I.Existence of the old landslide indicates a low friction angle of rock mass => low resistance in movement

II.Frictional heat created a cushion during sliding and converted slow rate sliding into rapid failure

Page 12: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

OMISSIONSOMISSIONSI. Presence of cataclastites in mylonitic zone: fault plane

II. Seismic activity: no connection with the formation of Vajont gorge

III. Wrong interpretation: increasing water level not favourable

IV. Omission: to analyse the slope or take a sample for laboratory tests

V. The superficial slides: verified but they were deeper than expected

VI. Rock degradation: indication that the rock was not as strong as before

Page 13: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

OMISSIONSOMISSIONS

Carlo Semenza was aware of the problems:

“...things are probably bigger than us and there are no adequate practical measures...”

“...I am in front of a thing which due to its dimensions seems toescape from our hands...”

Page 14: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

POST-FAILURE CONSIDERATIONSPOST-FAILURE CONSIDERATIONS

o Modification in the design standards of ongoing projects

o Geodetic station => sustain water level in safe limits

o Microseismic monitoring => localize and forewarn for an oncoming

slope failure

o Acoustic emissions => forecast future movements

o Engineers and geologists observe and inspect the slopes of

projected basins

Page 15: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

CONCLUDING REMARKSCONCLUDING REMARKS

o Construction giant dams need to take all

factors under consideration

o Continue checking, supervising and

maintaining the construction, after its

completion

There are always unpredictable and ‘‘time independent hazards’’

Page 16: MARIA CHINI VIKI IOANNOU THEMISTOKLIS TERATSIAS. o Vajont valley: part of the NE Italian Alps region o The dam is located between the mountains Toc and

THANK YOU FOR YOUR THANK YOU FOR YOUR ATTENTION!ATTENTION!