Relating Dike Geometry and Injection Rate in Analogue Flux-Driven Experiments

Dikes feed most eruptions, so understanding their mechanism of propagation is fundamental for volcanic hazard assessment. The variation in geometry of a propagating dike as a function of the injection rate remains poorly studied. Here we use experiments injecting water into gelatin to investigate th...

Full description

Bibliographic Details
Main Authors: Federico Galetto, Alessandro Bonaccorso, Valerio Acocella
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-05-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.665865/full
id doaj-3f5567dc97444cdf99e798b1a225cc8f
record_format Article
spelling doaj-3f5567dc97444cdf99e798b1a225cc8f2021-05-13T05:03:14ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-05-01910.3389/feart.2021.665865665865Relating Dike Geometry and Injection Rate in Analogue Flux-Driven ExperimentsFederico Galetto0Federico Galetto1Alessandro Bonaccorso2Valerio Acocella3Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Catania, ItalyDepartment of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY, United StatesIstituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Catania, ItalyUniversità Degli Studi di Roma Tre, Dipartimento di Scienze, Roma, ItalyDikes feed most eruptions, so understanding their mechanism of propagation is fundamental for volcanic hazard assessment. The variation in geometry of a propagating dike as a function of the injection rate remains poorly studied. Here we use experiments injecting water into gelatin to investigate the variation of the thickness, width and length of a flux-driven dike connected to its source as a function of the injection time and intruded volume. Results show that the thickness of vertically propagating dikes is proportional to the injection rate and remains constant as long as the latter is constant. Neither buoyancy nor injected volume influence the thickness. The along-strike width of the dike is, however, proportional to the injected volume. These results, consistent with the inferred behavior of several dikes observed during emplacement, open new opportunities to better understand how dikes propagate and also to forecast how emplacing dikes may propagate once their geometric features are detected in real-time through monitoring data.https://www.frontiersin.org/articles/10.3389/feart.2021.665865/fullflux-driven dikesdike propagationinjection ratedike geometryanalogue experiments
collection DOAJ
language English
format Article
sources DOAJ
author Federico Galetto
Federico Galetto
Alessandro Bonaccorso
Valerio Acocella
spellingShingle Federico Galetto
Federico Galetto
Alessandro Bonaccorso
Valerio Acocella
Relating Dike Geometry and Injection Rate in Analogue Flux-Driven Experiments
Frontiers in Earth Science
flux-driven dikes
dike propagation
injection rate
dike geometry
analogue experiments
author_facet Federico Galetto
Federico Galetto
Alessandro Bonaccorso
Valerio Acocella
author_sort Federico Galetto
title Relating Dike Geometry and Injection Rate in Analogue Flux-Driven Experiments
title_short Relating Dike Geometry and Injection Rate in Analogue Flux-Driven Experiments
title_full Relating Dike Geometry and Injection Rate in Analogue Flux-Driven Experiments
title_fullStr Relating Dike Geometry and Injection Rate in Analogue Flux-Driven Experiments
title_full_unstemmed Relating Dike Geometry and Injection Rate in Analogue Flux-Driven Experiments
title_sort relating dike geometry and injection rate in analogue flux-driven experiments
publisher Frontiers Media S.A.
series Frontiers in Earth Science
issn 2296-6463
publishDate 2021-05-01
description Dikes feed most eruptions, so understanding their mechanism of propagation is fundamental for volcanic hazard assessment. The variation in geometry of a propagating dike as a function of the injection rate remains poorly studied. Here we use experiments injecting water into gelatin to investigate the variation of the thickness, width and length of a flux-driven dike connected to its source as a function of the injection time and intruded volume. Results show that the thickness of vertically propagating dikes is proportional to the injection rate and remains constant as long as the latter is constant. Neither buoyancy nor injected volume influence the thickness. The along-strike width of the dike is, however, proportional to the injected volume. These results, consistent with the inferred behavior of several dikes observed during emplacement, open new opportunities to better understand how dikes propagate and also to forecast how emplacing dikes may propagate once their geometric features are detected in real-time through monitoring data.
topic flux-driven dikes
dike propagation
injection rate
dike geometry
analogue experiments
url https://www.frontiersin.org/articles/10.3389/feart.2021.665865/full
work_keys_str_mv AT federicogaletto relatingdikegeometryandinjectionrateinanaloguefluxdrivenexperiments
AT federicogaletto relatingdikegeometryandinjectionrateinanaloguefluxdrivenexperiments
AT alessandrobonaccorso relatingdikegeometryandinjectionrateinanaloguefluxdrivenexperiments
AT valerioacocella relatingdikegeometryandinjectionrateinanaloguefluxdrivenexperiments
_version_ 1721442753057914880