Mass fux decay timescales of volcanic particles due to aeolian processes in the Argentinian Patagonia steppe

We investigate the timescales of the horizontal mass flux decay of wind remobilised volcanic particles in Argentina, associated with the tephra-fallout deposit produced by the 2011–2012 Cordón Caulle (Chile) eruption. Particle removal processes are controlled by complex interactions of meteorological conditions, surface properties and particle depletion with time. We find that ash remobilisation follows a two-phase exponential decay with specific timescales for the initial input of fresh ash (1–74 days) and the following soil stabilisation processes (3–52 months). The characteristic timescales as a function of particle size shows two minimum values, identified for sizes around 2 and 19–37 μ m, suggesting that these size-range particles are remobilised more easily, due to the interaction between saltation and suspension-induced processes. We find that in volcanic regions, characterised by a sudden release and a subsequent depletion of particles, the availability of wind-erodible particles plays a major role due to compaction and removal of fine particles. We propose, therefore, a simple and reproducible empirical model to describe the mass flux decay of remobilised ash in a supply-limited environment. This methodology represents an innovative approach to link field measurements of multi-sized and supply-limited deposits with saltation erosion theory.

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Main Authors: Dominguez, Lucia, Rossi, Eduardo, Mingari, Leonardo, Bonadonna, Costanza, Forte, Pablo Brian, Panebianco, Juan Esteban, Bran, Donaldo Eduardo
Format: info:ar-repo/semantics/artículo biblioteca
Language:eng
Published: Springer Nature 2020-09
Subjects:Cenizas, Materiales Volcánicos, Tamaño de la Partícula, Viento, Erupciones Volcánicas, Ashes, Volcanic Materials, Particle size, Wind, Volcanic Eruptions, Remobilisation, Mass Flux Decay, Cordón Caulle, Región Patagónica,
Online Access:http://hdl.handle.net/20.500.12123/14969
https://www.nature.com/articles/s41598-020-71022-w
https://doi.org/10.1038/s41598-020-71022-w
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spelling oai:localhost:20.500.12123-149692023-08-22T11:21:50Z Mass fux decay timescales of volcanic particles due to aeolian processes in the Argentinian Patagonia steppe Dominguez, Lucia Rossi, Eduardo Mingari, Leonardo Bonadonna, Costanza Forte, Pablo Brian Panebianco, Juan Esteban Bran, Donaldo Eduardo Cenizas Materiales Volcánicos Tamaño de la Partícula Viento Erupciones Volcánicas Ashes Volcanic Materials Particle size Wind Volcanic Eruptions Remobilisation Mass Flux Decay Cordón Caulle Región Patagónica We investigate the timescales of the horizontal mass flux decay of wind remobilised volcanic particles in Argentina, associated with the tephra-fallout deposit produced by the 2011–2012 Cordón Caulle (Chile) eruption. Particle removal processes are controlled by complex interactions of meteorological conditions, surface properties and particle depletion with time. We find that ash remobilisation follows a two-phase exponential decay with specific timescales for the initial input of fresh ash (1–74 days) and the following soil stabilisation processes (3–52 months). The characteristic timescales as a function of particle size shows two minimum values, identified for sizes around 2 and 19–37 μ m, suggesting that these size-range particles are remobilised more easily, due to the interaction between saltation and suspension-induced processes. We find that in volcanic regions, characterised by a sudden release and a subsequent depletion of particles, the availability of wind-erodible particles plays a major role due to compaction and removal of fine particles. We propose, therefore, a simple and reproducible empirical model to describe the mass flux decay of remobilised ash in a supply-limited environment. This methodology represents an innovative approach to link field measurements of multi-sized and supply-limited deposits with saltation erosion theory. EEA Bariloche Fil: Dominguez, Lucia. University of Geneva. Department of Earth Sciences; Suiza Fil: Rossi, Eduardo. University of Geneva. Department of Earth Sciences; Suiza Fil: Mingari, Leonardo. Barcelona Supercomputing Center; España Fil: Bonadonna, Costanza. University of Geneva. Department of Earth Sciences; Suiza Fil: Forte, Pablo Brian. Universidad de Buenos Aires. Instituto de Estudios Andinos; Argentina Fil: Forte, Pablo Brian. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Panebianco, Juan Esteban. Universidad Nacional de La Pampa. Facultad de Ciencias Exactas y Naturales. Instituto de Ciencias de la Tierra y Ambientales; Argentina Fil: Panebianco, Juan Esteban. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Bran, Donaldo Eduardo. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Bariloche; Argentina 2023-08-22T11:13:13Z 2023-08-22T11:13:13Z 2020-09 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://hdl.handle.net/20.500.12123/14969 https://www.nature.com/articles/s41598-020-71022-w 2045-2322 https://doi.org/10.1038/s41598-020-71022-w eng info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) application/pdf Springer Nature Scientific Reports 10 : 14456 (2020)
institution INTA AR
collection DSpace
country Argentina
countrycode AR
component Bibliográfico
access En linea
databasecode dig-inta-ar
tag biblioteca
region America del Sur
libraryname Biblioteca Central del INTA Argentina
language eng
topic Cenizas
Materiales Volcánicos
Tamaño de la Partícula
Viento
Erupciones Volcánicas
Ashes
Volcanic Materials
Particle size
Wind
Volcanic Eruptions
Remobilisation
Mass Flux Decay
Cordón Caulle
Región Patagónica
Cenizas
Materiales Volcánicos
Tamaño de la Partícula
Viento
Erupciones Volcánicas
Ashes
Volcanic Materials
Particle size
Wind
Volcanic Eruptions
Remobilisation
Mass Flux Decay
Cordón Caulle
Región Patagónica
spellingShingle Cenizas
Materiales Volcánicos
Tamaño de la Partícula
Viento
Erupciones Volcánicas
Ashes
Volcanic Materials
Particle size
Wind
Volcanic Eruptions
Remobilisation
Mass Flux Decay
Cordón Caulle
Región Patagónica
Cenizas
Materiales Volcánicos
Tamaño de la Partícula
Viento
Erupciones Volcánicas
Ashes
Volcanic Materials
Particle size
Wind
Volcanic Eruptions
Remobilisation
Mass Flux Decay
Cordón Caulle
Región Patagónica
Dominguez, Lucia
Rossi, Eduardo
Mingari, Leonardo
Bonadonna, Costanza
Forte, Pablo Brian
Panebianco, Juan Esteban
Bran, Donaldo Eduardo
Mass fux decay timescales of volcanic particles due to aeolian processes in the Argentinian Patagonia steppe
description We investigate the timescales of the horizontal mass flux decay of wind remobilised volcanic particles in Argentina, associated with the tephra-fallout deposit produced by the 2011–2012 Cordón Caulle (Chile) eruption. Particle removal processes are controlled by complex interactions of meteorological conditions, surface properties and particle depletion with time. We find that ash remobilisation follows a two-phase exponential decay with specific timescales for the initial input of fresh ash (1–74 days) and the following soil stabilisation processes (3–52 months). The characteristic timescales as a function of particle size shows two minimum values, identified for sizes around 2 and 19–37 μ m, suggesting that these size-range particles are remobilised more easily, due to the interaction between saltation and suspension-induced processes. We find that in volcanic regions, characterised by a sudden release and a subsequent depletion of particles, the availability of wind-erodible particles plays a major role due to compaction and removal of fine particles. We propose, therefore, a simple and reproducible empirical model to describe the mass flux decay of remobilised ash in a supply-limited environment. This methodology represents an innovative approach to link field measurements of multi-sized and supply-limited deposits with saltation erosion theory.
format info:ar-repo/semantics/artículo
topic_facet Cenizas
Materiales Volcánicos
Tamaño de la Partícula
Viento
Erupciones Volcánicas
Ashes
Volcanic Materials
Particle size
Wind
Volcanic Eruptions
Remobilisation
Mass Flux Decay
Cordón Caulle
Región Patagónica
author Dominguez, Lucia
Rossi, Eduardo
Mingari, Leonardo
Bonadonna, Costanza
Forte, Pablo Brian
Panebianco, Juan Esteban
Bran, Donaldo Eduardo
author_facet Dominguez, Lucia
Rossi, Eduardo
Mingari, Leonardo
Bonadonna, Costanza
Forte, Pablo Brian
Panebianco, Juan Esteban
Bran, Donaldo Eduardo
author_sort Dominguez, Lucia
title Mass fux decay timescales of volcanic particles due to aeolian processes in the Argentinian Patagonia steppe
title_short Mass fux decay timescales of volcanic particles due to aeolian processes in the Argentinian Patagonia steppe
title_full Mass fux decay timescales of volcanic particles due to aeolian processes in the Argentinian Patagonia steppe
title_fullStr Mass fux decay timescales of volcanic particles due to aeolian processes in the Argentinian Patagonia steppe
title_full_unstemmed Mass fux decay timescales of volcanic particles due to aeolian processes in the Argentinian Patagonia steppe
title_sort mass fux decay timescales of volcanic particles due to aeolian processes in the argentinian patagonia steppe
publisher Springer Nature
publishDate 2020-09
url http://hdl.handle.net/20.500.12123/14969
https://www.nature.com/articles/s41598-020-71022-w
https://doi.org/10.1038/s41598-020-71022-w
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