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Bridge over Jökulsá á Fjöllum – when is a glacial flood too large to design for?

 Bridge over Jökulsá á Fjöllum – when is a glacial flood too large to design for?
Auteur(s):
Présenté pendant IABSE Congress: Challenges in Design and Construction of an Innovative and Sustainable Built Environment, Stockholm, Sweden, 21-23 September 2016, publié dans , pp. 2668-2675
DOI: 10.2749/stockholm.2016.2667
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Volcanic eruptions can result in lava flows, ash fall or when an eruption is under the glacier, large glacial water outburst floods, or jökulhlaup, which can have catastrophic effects. Recent jökul...
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Détails bibliographiques

Auteur(s): (Icelandic Road and Coastal Administration, Reykjavik, Iceland)
Médium: papier de conférence
Langue(s): anglais
Conférence: IABSE Congress: Challenges in Design and Construction of an Innovative and Sustainable Built Environment, Stockholm, Sweden, 21-23 September 2016
Publié dans:
Page(s): 2668-2675 Nombre total de pages (du PDF): 8
Page(s): 2668-2675
Nombre total de pages (du PDF): 8
Année: 2016
DOI: 10.2749/stockholm.2016.2667
Abstrait:

Volcanic eruptions can result in lava flows, ash fall or when an eruption is under the glacier, large glacial water outburst floods, or jökulhlaup, which can have catastrophic effects. Recent jökulhlaups in Iceland have resulted in the collapse of a few bridges. The existing bridge over Jökulsá á Fjöllum on the Icelandic Ring Road (road no.1) is a suspension bridge with a main span of 107 m, built in 1947, and with a limited capacity for heavy transport. In 2014, a new bridge was being planned and almost ready for tender. However in August 2014 a volcanic eruption started 10 km north of Vatnajökull glacier. There was a considerable likelihood that the eruption would extend under the glacier. Decision was made to change from the previously designed alternative to a cable stayed bridge which provides an alternative flood path, being more robust to an extreme event and much increased flow capacity.

Mots-clé:
tremblements de terre

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