Role of mechanical erosion in controlling the effusion rate of basaltic eruptions

Abstract In many basaltic eruptions, observations show that the effusion rate of magma has a typical dependence on time: the effusion rate curves show first a period of increasing and later a decreasing phase by a maximum value. We present a model to explain this behavior by the emptying of a magma...

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Main Authors: Antonello Piombo, Andrea Tallarico, Michele Dragoni
Format: Article
Language:English
Published: Wiley 2016-09-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1002/2016GL069737
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author Antonello Piombo
Andrea Tallarico
Michele Dragoni
author_facet Antonello Piombo
Andrea Tallarico
Michele Dragoni
author_sort Antonello Piombo
collection DOAJ
description Abstract In many basaltic eruptions, observations show that the effusion rate of magma has a typical dependence on time: the effusion rate curves show first a period of increasing and later a decreasing phase by a maximum value. We present a model to explain this behavior by the emptying of a magma reservoir through a vertical cylindrical conduit with elliptical cross section, coupled with the its widening due to mechanical erosion, produced by the magma flow. The model can reproduce the observed dependence on time of effusion rate in basaltic eruptions. Eruption duration and the maximum value of effusion rate depend on the size of magma chamber, on lava viscosity and strongly on erosion rate per unit traction.
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spelling doaj-art-ff5257bdcb5149b8bef99c74a26c0c7c2025-08-20T03:10:24ZengWileyGeophysical Research Letters0094-82761944-80072016-09-0143178970897710.1002/2016GL069737Role of mechanical erosion in controlling the effusion rate of basaltic eruptionsAntonello Piombo0Andrea Tallarico1Michele Dragoni2Dipartimento di Fisica e Astronomia Alma Mater Studiorum–Università di Bologna Bologna ItalyDipartimento di Scienze della Terra e Geoambientali Università degli Studi di Bari “Aldo Moro” Bari ItalyDipartimento di Fisica e Astronomia Alma Mater Studiorum–Università di Bologna Bologna ItalyAbstract In many basaltic eruptions, observations show that the effusion rate of magma has a typical dependence on time: the effusion rate curves show first a period of increasing and later a decreasing phase by a maximum value. We present a model to explain this behavior by the emptying of a magma reservoir through a vertical cylindrical conduit with elliptical cross section, coupled with the its widening due to mechanical erosion, produced by the magma flow. The model can reproduce the observed dependence on time of effusion rate in basaltic eruptions. Eruption duration and the maximum value of effusion rate depend on the size of magma chamber, on lava viscosity and strongly on erosion rate per unit traction.https://doi.org/10.1002/2016GL069737volcanologylava flow ratebasaltic eruption
spellingShingle Antonello Piombo
Andrea Tallarico
Michele Dragoni
Role of mechanical erosion in controlling the effusion rate of basaltic eruptions
Geophysical Research Letters
volcanology
lava flow rate
basaltic eruption
title Role of mechanical erosion in controlling the effusion rate of basaltic eruptions
title_full Role of mechanical erosion in controlling the effusion rate of basaltic eruptions
title_fullStr Role of mechanical erosion in controlling the effusion rate of basaltic eruptions
title_full_unstemmed Role of mechanical erosion in controlling the effusion rate of basaltic eruptions
title_short Role of mechanical erosion in controlling the effusion rate of basaltic eruptions
title_sort role of mechanical erosion in controlling the effusion rate of basaltic eruptions
topic volcanology
lava flow rate
basaltic eruption
url https://doi.org/10.1002/2016GL069737
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AT andreatallarico roleofmechanicalerosionincontrollingtheeffusionrateofbasalticeruptions
AT micheledragoni roleofmechanicalerosionincontrollingtheeffusionrateofbasalticeruptions